Abstract

We present HST spectroscopy for 45 cataclysmic variables (CVs), observed with HST/COS and HST/STIS. For 36 CVs, the white dwarf is recognisable through its broad Ly α absorption profile and we measure the white dwarf effective temperatures (Teff) by fitting the HST data assuming log  g = 8.35, which corresponds to the average mass for CV white dwarfs (≃0.8 M). Our results nearly double the number of CV white dwarfs with an accurate temperature measurement. We find that CVs above the period gap have, on average, higher temperatures (〈Teff〉 ≃ 23 000 K) and exhibit much more scatter compared to those below the gap (〈Teff〉 ≃ 15 000 K). While this behaviour broadly agrees with theoretical predictions, some discrepancies are present: (i) all our new measurements above the gap are characterized by lower temperatures (Teff ≃ 16 000–26 000 K) than predicted by the present-day CV population models (Teff ≃ 38 000–43 000 K); (ii) our results below the gap are not clustered in the predicted narrow track and exhibit in particular a relatively large spread near the period minimum, which may point to some shortcomings in the CV evolutionary models. Finally, in the standard model of CV evolution, reaching the minimum period, CVs are expected to evolve back towards longer periods with mean accretion rates |$\dot{M}\lesssim 2 \times 10^{-11}\,\mathrm{M}_{\odot }\,\mathrm{yr}^{-1}$|⁠, corresponding to Teff ≲ 11 500 K. We do not unambiguously identify any such system in our survey, suggesting that this major component of the predicted CV population still remains elusive to observations.

1 INTRODUCTION

Cataclysmic variables (CVs) are close interacting binaries containing a white dwarf accreting from a Roche lobe filling low-mass companion star (Warner 1995). In the absence of a strong magnetic field (B ≲ 10 MG), the flow of material lost by the secondary gives rise to an accretion disc around the white dwarf primary.

In the standard model of CV evolution, the stability of the accretion process on long time-scales (of the order of 109 Gyr; Kolb & Stehle 1996) requires a mass ratio q = M2/M1 ≲ 5/6 (Frank, King & Raine 2002, M1 and M2 denote the white dwarf and secondary mass) and a mechanism of angular momentum loss (AML) that continuously shrinks the system and keeps the secondary in touch with its Roche lobe. In the frequently referenced Interrupted Magnetic Braking Scenario, at least two different AML mechanisms drive CV evolution (Paczynski & Sienkiewicz 1983; Rappaport, Verbunt & Joss 1983; Spruit & Ritter 1983). For orbital periods Porb ≳ 3 h, the angular momentum is predominantly removed by magnetic braking (MB) that arises from a stellar wind associated with the magnetic activity of the secondary, with typical mass-transfer rates of |$\dot{M}\,\sim \,10^{-9} \text{--} 10^{-8} \,\mathrm{M}_{\odot } \, \mathrm{yr}^{-1}$| (Spruit & Ritter 1983). For Porb ≲ 3 h, the dominant AML mechanism is gravitational wave radiation (GR), with typical |$\dot{M} \sim 5 \times 10^{-11} \,\mathrm{M}_{\odot } \, \mathrm{yr}^{-1}$| (Patterson 1984).

Another fundamental ingredient for CV evolution is the internal structure of the secondary and its response to mass-loss (Knigge 2006; Knigge, Baraffe & Patterson 2011). At Porb ≃ 3 h, the donor star has become fully convective. MB via a stellar wind is thought to be greatly reduced and the system evolves as a detached binary through the period range 2 h ≲ Porb ≲ 3 h (the period gap). Following the diminution of MB (Rappaport et al. 1983), the system evolves through GR only, which reduces the orbital separation bringing the secondary again into contact with its Roche lobe at Porb ≃ 2 h.

In the final phase of CV evolution (Porb ≃ 80 min), the donor starts behaving like a degenerate object, ceasing to contract in response to continue mass-loss, and the system evolves back towards longer periods (the so-called period bouncers), with mean accretion rates |$\dot{M} \lesssim 2 \times 10^{-11}\,\mathrm{M}_{\odot }\,\mathrm{yr}^{-1}$|⁠.

Since different period ranges are characterized by different mass-transfer rates, Porb (one of the most easily measured system parameter in CVs) provides a first rough estimate of the accretion rate and the evolutionary stage of the system. A more precise measurement of the mean accretion rate can be derived from the white dwarf effective temperature (Teff): its value is set by compressional heating of the accreted material (Sion 1995), providing a constraint on the secular mean of the mass-transfer rate |$\langle \dot{M} \rangle$|⁠, averaged over the thermal time-scale of the white dwarf envelope, (103–105 yr) and is one of the best-available tests for the present models of CV evolution (Townsley & Bildsten 2003).

While there are now over 1100 CVs with an orbital period determination (Ritter & Kolb 2003), comparatively little is known about their accreting white dwarfs: reliable1Teff measurements are available for only 43 CV white dwarfs (Townsley & Gänsicke 2009), only 32 have an accurate mass determination (Zorotovic, Schreiber & Gänsicke 2011) and only 11 have both. To improve our knowledge of CV evolution, it is essential to increase the number of objects with an accurate Teff and mass measurement.

Since CV white dwarfs are relatively hot objects (Teff ≳ 10 000 K), their spectral energy distribution peaks in the ultraviolet. At these wavelengths, the contamination from the accretion flow and the secondary star is often small or negligible compared to their contribution at optical wavelengths, and therefore space-based ultraviolet observations are necessary for a white dwarf Teff determination (Szkody et al. 2002a; Gänsicke et al. 2006; Sion et al. 2008, and many others). For this purpose, we carried out a large Hubble Space Telescope (HST) programme in which we obtained high-resolution ultraviolet spectroscopy of 40 CVs with the Cosmic Origin Spectrograph (COS). We complemented our sample with eight systems (three of which are in common with the COS sample) observed during two programmes carried out with the Space Telescope Imaging Spectrograph (STIS).

The targets were selected to sample the entire orbital period range of the Galactic CV population (Fig. 1); four objects with previous Teff measurements were included for comparison with our results (CU Vel, DV UMa, GW Lib and SDSS J103533.02+055158). In particular, we selected two eclipsing systems (DV UMa and SDSS J103533.02+055158) to compare our spectroscopic analysis with results obtained from modelling the eclipse light curve (e.g. Feline et al. 2004; Littlefair et al. 20062008), which is the most commonly used method for determining white dwarf Teff from ground-based observations.

The orbital period distribution of 1144 semidetached binaries containing a white dwarf and a Roche lobe filling low-mass secondary (Ritter & Kolb 2003, 7th edition, release 7.21, 2014 March). The systems visible at short orbital periods (Porb ≲ 75 min) are the AM CVn stars and CVs hosting an evolved donor. The green band highlights the period gap (2.15 h ≲ Porb ≲ 3.18 h; Knigge 2006), the blue box indicates the period spike (80 min ≲ Porb ≲ 86 min; Gänsicke et al. 2009), the red line shows the period minimum (Pmin = 76.2 min; Knigge 2006), while the vertical lines along the top mark the orbital periods of the objects in our survey.
Figure 1.

The orbital period distribution of 1144 semidetached binaries containing a white dwarf and a Roche lobe filling low-mass secondary (Ritter & Kolb 2003, 7th edition, release 7.21, 2014 March). The systems visible at short orbital periods (Porb ≲ 75 min) are the AM CVn stars and CVs hosting an evolved donor. The green band highlights the period gap (2.15 h ≲ Porb ≲ 3.18 h; Knigge 2006), the blue box indicates the period spike (80 min ≲ Porb ≲ 86 min; Gänsicke et al. 2009), the red line shows the period minimum (Pmin = 76.2 min; Knigge 2006), while the vertical lines along the top mark the orbital periods of the objects in our survey.

Here we present the HST observations and the results of our spectral analysis, which almost doubles the number of objects with reliable Teff measurements, providing |$\langle \dot{M} \rangle$| and testing the present-day CV population evolution models.

2 OBSERVATIONS

2.1 COS observations

The COS data were collected in 122 HST orbits from 2012 October to 2014 March (programme ID 12870; Table 1). Each CV was observed using the Primary Science Aperture for two to five consecutive spacecraft orbits. The data from all the orbits were summed to produce an average ultraviolet spectrum for each object. We used the G140L grating, which has a nominal resolution of R ≃ 3000, at the central wavelength of 1105 Å  and the far-ultraviolet (FUV) channel, covering the wavelength range 1105–2253 Å. The detector sensitivity quickly decreases in the red portion of the spectrum, reducing the useful range to ≃1150–1730 Å.

Table 1.

Log of the HST/COS observations. The systems are ordered by orbital period. The V-band magnitudes listed here are the quiescent values reported from the literature and do not represent the brightness during the COS observations (see Figs 3 and 4).

SystemPorbTypeVE(B − V)ObservationNumberTotalState
(min)(mag)(mag)dateofexposure
orbitstime (s)
V485 Cen59.03SU UMa17.70.071a2013 Mar 1649907q
GW Lib76.78WZ Sge16.50.03b2013 May 3037417q
SDSS J143544.02+233638.778.00WZ Sge?18.20.029a2013 Mar 0937123q
OT J213806.6+26195778.10WZ Sge16.10.063a2013 Jul 2524760q
SDSS J013701.06−091234.879.71SU UMa18.70.024c2013 Sep 13410 505q
SDSS J123813.73−033932.980.52WZ Sge17.80.006c2013 Mar 0137183q
PU CMa81.63SU UMa16.20.09a2013 Mar 2224757eq
V1108 Her81.87WZ Sge17.70.025c2013 Jun 0637327q
ASAS J002511+1217.282.00WZ Sge17.50.025c2012 Nov 1537183q
SDSS J103533.02+055158.482.22WZ Sge?18.80.009c2013 Mar 08512 282q
CC Scl84.10DN/IP17.00.013a2013 Jun 2924668q
SDSS J075507.70+143547.684.76WZ Sge?18.20.028a2012 Dec 1437183q
1RXS J105010.8−14043188.56WZ Sge17.00.018c2013 May 1037363q
MR UMa91.17SU UMa16.70.02a2013 Apr 0424401q
QZ Lib92.36WZ Sge17.50.054c2013 Apr 2637512q
SDSS J153817.35+512338.093.11CV18.60.012a2013 May 1624704q
1RXS J023238.8−37181295.04WZ Sge18.80.027a2012 Nov 01512 556q
SDSS J093249.57+472523.095.48DN?17.90.014a2013 Jan 1124326eq
BB Ari101.20SU UMa17.90.105a2013 Sep 2724817q
DT Oct104.54SU UMa16.50.145a2013 May 2024875eq
IY UMa106.43SU UMa18.40.012c2013 Mar 3024195q
SDSS J100515.38+191107.9107.60SU UMa18.20.025a2013 Jan 3137093q
RZ Leo110.17WZ Sge19.20.029c2013 Apr 11410 505q
CU Vel113.04SU UMa17.0<0.02d2013 Jan 1824634q
AX For113.04SU UMa18.50.027c2013 Jul 1137483q
SDSS J164248.52+134751.4113.60DN18.60.063a2012 Oct 1237240eq
QZ Ser119.75SU UMa17.90.038c2013 Jun 21410 505q
IR Com125.34DN18.00.016c2013 Feb 0836866q
SDSS J001153.08−064739.2144.40U Gem17.80.029a2012 Nov 09512 601q
OR And195.70VY Scl18.20.158a2013 Jul 1037361hs
BB Dor221.90VY Scl18.00.03a2013 Feb 1337272is
SDSS J040714.78−064425.1245.04U Gem17.80.08a2013 Jan 2424315q
CW Mon254.30U Gem16.80.044c2012 Nov 3024774eq
V405 Peg255.81CV18.20.064c2012 Dec 0737303eq
HS 2214+2845258.02U Gem16.80.078a2013 Jun 1824680q
BD Pav258.19U Gem15.40.0b2013 Jun 1437375q?
SDSS J100658.41+233724.4267.71U Gem18.30.018c2014 Mar 20512 494q
HM Leo268.99U Gem17.50.021c2013 Feb 2249979eq
SDSS J154453.60+255348.8361.84U Gem?16.90.032c2013 Apr 22?
HS 0218+3229428.02U Gem15.50.05c2012 Dec 2237159q
HS 1055+0939541.88U Gem15.50.025a2013 Apr 1524688eq
SystemPorbTypeVE(B − V)ObservationNumberTotalState
(min)(mag)(mag)dateofexposure
orbitstime (s)
V485 Cen59.03SU UMa17.70.071a2013 Mar 1649907q
GW Lib76.78WZ Sge16.50.03b2013 May 3037417q
SDSS J143544.02+233638.778.00WZ Sge?18.20.029a2013 Mar 0937123q
OT J213806.6+26195778.10WZ Sge16.10.063a2013 Jul 2524760q
SDSS J013701.06−091234.879.71SU UMa18.70.024c2013 Sep 13410 505q
SDSS J123813.73−033932.980.52WZ Sge17.80.006c2013 Mar 0137183q
PU CMa81.63SU UMa16.20.09a2013 Mar 2224757eq
V1108 Her81.87WZ Sge17.70.025c2013 Jun 0637327q
ASAS J002511+1217.282.00WZ Sge17.50.025c2012 Nov 1537183q
SDSS J103533.02+055158.482.22WZ Sge?18.80.009c2013 Mar 08512 282q
CC Scl84.10DN/IP17.00.013a2013 Jun 2924668q
SDSS J075507.70+143547.684.76WZ Sge?18.20.028a2012 Dec 1437183q
1RXS J105010.8−14043188.56WZ Sge17.00.018c2013 May 1037363q
MR UMa91.17SU UMa16.70.02a2013 Apr 0424401q
QZ Lib92.36WZ Sge17.50.054c2013 Apr 2637512q
SDSS J153817.35+512338.093.11CV18.60.012a2013 May 1624704q
1RXS J023238.8−37181295.04WZ Sge18.80.027a2012 Nov 01512 556q
SDSS J093249.57+472523.095.48DN?17.90.014a2013 Jan 1124326eq
BB Ari101.20SU UMa17.90.105a2013 Sep 2724817q
DT Oct104.54SU UMa16.50.145a2013 May 2024875eq
IY UMa106.43SU UMa18.40.012c2013 Mar 3024195q
SDSS J100515.38+191107.9107.60SU UMa18.20.025a2013 Jan 3137093q
RZ Leo110.17WZ Sge19.20.029c2013 Apr 11410 505q
CU Vel113.04SU UMa17.0<0.02d2013 Jan 1824634q
AX For113.04SU UMa18.50.027c2013 Jul 1137483q
SDSS J164248.52+134751.4113.60DN18.60.063a2012 Oct 1237240eq
QZ Ser119.75SU UMa17.90.038c2013 Jun 21410 505q
IR Com125.34DN18.00.016c2013 Feb 0836866q
SDSS J001153.08−064739.2144.40U Gem17.80.029a2012 Nov 09512 601q
OR And195.70VY Scl18.20.158a2013 Jul 1037361hs
BB Dor221.90VY Scl18.00.03a2013 Feb 1337272is
SDSS J040714.78−064425.1245.04U Gem17.80.08a2013 Jan 2424315q
CW Mon254.30U Gem16.80.044c2012 Nov 3024774eq
V405 Peg255.81CV18.20.064c2012 Dec 0737303eq
HS 2214+2845258.02U Gem16.80.078a2013 Jun 1824680q
BD Pav258.19U Gem15.40.0b2013 Jun 1437375q?
SDSS J100658.41+233724.4267.71U Gem18.30.018c2014 Mar 20512 494q
HM Leo268.99U Gem17.50.021c2013 Feb 2249979eq
SDSS J154453.60+255348.8361.84U Gem?16.90.032c2013 Apr 22?
HS 0218+3229428.02U Gem15.50.05c2012 Dec 2237159q
HS 1055+0939541.88U Gem15.50.025a2013 Apr 1524688eq

Notes. The E(B − V) data have been retrieved from: athe NASA/IPAC Extragalactic Database (NED); bGW Lib: Bullock et al. (2011), BD Pav: Sion et al. (2008); cthe three-dimensional map of interstellar dust reddening based on Pan-STARRS 1 and 2MASS photometry (Green et al. 2015); dthis work. The NED data are the Galactic colour excess and represent an upper limit for the actual reddening while the Pan-STARRS data are the actual reddening for the systems with a known distance. The last column reports the state of the system during the HST observations: eq – early quiescence, i.e. observed close to an outburst; q – quiescence; hs – high state; is – intermediate state.

Table 1.

Log of the HST/COS observations. The systems are ordered by orbital period. The V-band magnitudes listed here are the quiescent values reported from the literature and do not represent the brightness during the COS observations (see Figs 3 and 4).

SystemPorbTypeVE(B − V)ObservationNumberTotalState
(min)(mag)(mag)dateofexposure
orbitstime (s)
V485 Cen59.03SU UMa17.70.071a2013 Mar 1649907q
GW Lib76.78WZ Sge16.50.03b2013 May 3037417q
SDSS J143544.02+233638.778.00WZ Sge?18.20.029a2013 Mar 0937123q
OT J213806.6+26195778.10WZ Sge16.10.063a2013 Jul 2524760q
SDSS J013701.06−091234.879.71SU UMa18.70.024c2013 Sep 13410 505q
SDSS J123813.73−033932.980.52WZ Sge17.80.006c2013 Mar 0137183q
PU CMa81.63SU UMa16.20.09a2013 Mar 2224757eq
V1108 Her81.87WZ Sge17.70.025c2013 Jun 0637327q
ASAS J002511+1217.282.00WZ Sge17.50.025c2012 Nov 1537183q
SDSS J103533.02+055158.482.22WZ Sge?18.80.009c2013 Mar 08512 282q
CC Scl84.10DN/IP17.00.013a2013 Jun 2924668q
SDSS J075507.70+143547.684.76WZ Sge?18.20.028a2012 Dec 1437183q
1RXS J105010.8−14043188.56WZ Sge17.00.018c2013 May 1037363q
MR UMa91.17SU UMa16.70.02a2013 Apr 0424401q
QZ Lib92.36WZ Sge17.50.054c2013 Apr 2637512q
SDSS J153817.35+512338.093.11CV18.60.012a2013 May 1624704q
1RXS J023238.8−37181295.04WZ Sge18.80.027a2012 Nov 01512 556q
SDSS J093249.57+472523.095.48DN?17.90.014a2013 Jan 1124326eq
BB Ari101.20SU UMa17.90.105a2013 Sep 2724817q
DT Oct104.54SU UMa16.50.145a2013 May 2024875eq
IY UMa106.43SU UMa18.40.012c2013 Mar 3024195q
SDSS J100515.38+191107.9107.60SU UMa18.20.025a2013 Jan 3137093q
RZ Leo110.17WZ Sge19.20.029c2013 Apr 11410 505q
CU Vel113.04SU UMa17.0<0.02d2013 Jan 1824634q
AX For113.04SU UMa18.50.027c2013 Jul 1137483q
SDSS J164248.52+134751.4113.60DN18.60.063a2012 Oct 1237240eq
QZ Ser119.75SU UMa17.90.038c2013 Jun 21410 505q
IR Com125.34DN18.00.016c2013 Feb 0836866q
SDSS J001153.08−064739.2144.40U Gem17.80.029a2012 Nov 09512 601q
OR And195.70VY Scl18.20.158a2013 Jul 1037361hs
BB Dor221.90VY Scl18.00.03a2013 Feb 1337272is
SDSS J040714.78−064425.1245.04U Gem17.80.08a2013 Jan 2424315q
CW Mon254.30U Gem16.80.044c2012 Nov 3024774eq
V405 Peg255.81CV18.20.064c2012 Dec 0737303eq
HS 2214+2845258.02U Gem16.80.078a2013 Jun 1824680q
BD Pav258.19U Gem15.40.0b2013 Jun 1437375q?
SDSS J100658.41+233724.4267.71U Gem18.30.018c2014 Mar 20512 494q
HM Leo268.99U Gem17.50.021c2013 Feb 2249979eq
SDSS J154453.60+255348.8361.84U Gem?16.90.032c2013 Apr 22?
HS 0218+3229428.02U Gem15.50.05c2012 Dec 2237159q
HS 1055+0939541.88U Gem15.50.025a2013 Apr 1524688eq
SystemPorbTypeVE(B − V)ObservationNumberTotalState
(min)(mag)(mag)dateofexposure
orbitstime (s)
V485 Cen59.03SU UMa17.70.071a2013 Mar 1649907q
GW Lib76.78WZ Sge16.50.03b2013 May 3037417q
SDSS J143544.02+233638.778.00WZ Sge?18.20.029a2013 Mar 0937123q
OT J213806.6+26195778.10WZ Sge16.10.063a2013 Jul 2524760q
SDSS J013701.06−091234.879.71SU UMa18.70.024c2013 Sep 13410 505q
SDSS J123813.73−033932.980.52WZ Sge17.80.006c2013 Mar 0137183q
PU CMa81.63SU UMa16.20.09a2013 Mar 2224757eq
V1108 Her81.87WZ Sge17.70.025c2013 Jun 0637327q
ASAS J002511+1217.282.00WZ Sge17.50.025c2012 Nov 1537183q
SDSS J103533.02+055158.482.22WZ Sge?18.80.009c2013 Mar 08512 282q
CC Scl84.10DN/IP17.00.013a2013 Jun 2924668q
SDSS J075507.70+143547.684.76WZ Sge?18.20.028a2012 Dec 1437183q
1RXS J105010.8−14043188.56WZ Sge17.00.018c2013 May 1037363q
MR UMa91.17SU UMa16.70.02a2013 Apr 0424401q
QZ Lib92.36WZ Sge17.50.054c2013 Apr 2637512q
SDSS J153817.35+512338.093.11CV18.60.012a2013 May 1624704q
1RXS J023238.8−37181295.04WZ Sge18.80.027a2012 Nov 01512 556q
SDSS J093249.57+472523.095.48DN?17.90.014a2013 Jan 1124326eq
BB Ari101.20SU UMa17.90.105a2013 Sep 2724817q
DT Oct104.54SU UMa16.50.145a2013 May 2024875eq
IY UMa106.43SU UMa18.40.012c2013 Mar 3024195q
SDSS J100515.38+191107.9107.60SU UMa18.20.025a2013 Jan 3137093q
RZ Leo110.17WZ Sge19.20.029c2013 Apr 11410 505q
CU Vel113.04SU UMa17.0<0.02d2013 Jan 1824634q
AX For113.04SU UMa18.50.027c2013 Jul 1137483q
SDSS J164248.52+134751.4113.60DN18.60.063a2012 Oct 1237240eq
QZ Ser119.75SU UMa17.90.038c2013 Jun 21410 505q
IR Com125.34DN18.00.016c2013 Feb 0836866q
SDSS J001153.08−064739.2144.40U Gem17.80.029a2012 Nov 09512 601q
OR And195.70VY Scl18.20.158a2013 Jul 1037361hs
BB Dor221.90VY Scl18.00.03a2013 Feb 1337272is
SDSS J040714.78−064425.1245.04U Gem17.80.08a2013 Jan 2424315q
CW Mon254.30U Gem16.80.044c2012 Nov 3024774eq
V405 Peg255.81CV18.20.064c2012 Dec 0737303eq
HS 2214+2845258.02U Gem16.80.078a2013 Jun 1824680q
BD Pav258.19U Gem15.40.0b2013 Jun 1437375q?
SDSS J100658.41+233724.4267.71U Gem18.30.018c2014 Mar 20512 494q
HM Leo268.99U Gem17.50.021c2013 Feb 2249979eq
SDSS J154453.60+255348.8361.84U Gem?16.90.032c2013 Apr 22?
HS 0218+3229428.02U Gem15.50.05c2012 Dec 2237159q
HS 1055+0939541.88U Gem15.50.025a2013 Apr 1524688eq

Notes. The E(B − V) data have been retrieved from: athe NASA/IPAC Extragalactic Database (NED); bGW Lib: Bullock et al. (2011), BD Pav: Sion et al. (2008); cthe three-dimensional map of interstellar dust reddening based on Pan-STARRS 1 and 2MASS photometry (Green et al. 2015); dthis work. The NED data are the Galactic colour excess and represent an upper limit for the actual reddening while the Pan-STARRS data are the actual reddening for the systems with a known distance. The last column reports the state of the system during the HST observations: eq – early quiescence, i.e. observed close to an outburst; q – quiescence; hs – high state; is – intermediate state.

The COS FUV detector consists of a photon-counting microchannel plate that converts the incoming photons into electronic pulses. An excessive photon flux could result in permanent damages, and even the loss, of the detector. This is very important in the framework of CV observations since these objects are characterized by periods of quiescence, in which the accretion on to the white dwarf is greatly reduced, interrupted by bright outbursts (thermal instabilities in the disc which cause a variation in the mass-transfer rate through the disc; Osaki 1974; Meyer & Meyer-Hofmeister 1984; Hameury et al. 1998). During an outburst, CVs typically brighten by 2–5 mag, occasionally up to 9 mag (Maza & Gonzalez 1983; Warner 1995; Templeton 2007). This increase in luminosity occurs rapidly, on the time-scale of about a day, first at optical wavelengths and hours to a day later in the ultraviolet (Hassall et al. 1983; Schreiber, Hameury & Lasota 2003; Schreiber, Hameury & Lasota 2004). Therefore, CVs can easily reach, and exceed, the COS detector safety threshold. The outburst recurrence time ranges from weeks to decades and these events are unpredictable. To avoid damage to the detectors, an intensive monitoring of each target was required before the observations. This monitoring programme was carried out by the global amateur community and some additional small telescopes [American Association of Variable Star Observers (AAVSO), Prompt and many others], and only their outstanding support has made this HST survey possible.

Among our 41 COS targets, only SDSS J154453.60+255348.8 could not be observed since it showed strong variations in its optical brightness in the days before the HST observation.

After an outburst, the white dwarf does not cool immediately to its quiescent temperature since it has been heated by the increased infall of material. The time required to cool back to the quiescent temperature has been modelled and is related to the outburst amplitude and duration (Sion 1995; Townsley & Bildsten 2004; Piro, Arras & Bildsten 2005). It has been observed that it can vary from days or weeks up to several years (Long, Blair & Raymond 1995; Gänsicke & Beuermann 1996; Slevinsky et al. 1999; Piro et al. 2005, see Szkody et al. 2016 for an extreme case). Therefore, the effective temperature measured in a system in which an outburst has recently occurred provides only an upper limit for its quiescent effective temperature and, consequently, for |$\langle \dot{M} \rangle$|⁠.

The right-hand panels of Fig. 2 show three sample COS ultraviolet spectra of quiescent CVs in which the white dwarf dominates the emission, as seen from the broad Ly α absorption centred on 1216 Å. The shape of the Ly α line changes with Teff, becoming more defined and narrower in the hotter white dwarfs, while the continuum slope of the spectrum becomes steeper.

HST/STIS spectra (left) and HST/COS spectra (right) for six objects in which the white dwarf dominates the far-ultraviolet. The geocoronal emission lines of Ly α (1216 Å) and O i (1302 Å) are plotted in grey.
Figure 2.

HST/STIS spectra (left) and HST/COS spectra (right) for six objects in which the white dwarf dominates the far-ultraviolet. The geocoronal emission lines of Ly α (1216 Å) and O i (1302 Å) are plotted in grey.

While the majority of the CVs in our sample have been observed in quiescence (Fig. 3), obvious signatures of the white dwarf were missing in the spectra of nine systems: seven of them experienced an outburst shortly before the HST observation while the remaining two systems are VY Scl stars (Fig. 4). This class of CVs is characterized by high mean accretion rates that keep the disc usually in a stable hot state, equivalent to a dwarf nova in permanent outburst. In this high state, the disc dominates the spectral appearance even in the FUV. However, occasionally the accretion rate drops (low state) and unveils the white dwarf (e.g. Gänsicke et al. 1999; Knigge et al. 2000; Hoard et al. 2004). The VY Scl stars in our sample (OR And and BB Dor) were caught in the high state and intermediate state, respectively, preventing a detection of the white dwarf. For the purpose of completeness, the spectra of these nine objects are shown in Fig. 5, but a detailed analysis of these systems is outside the scope of this paper and will be presented elsewhere (e.g. Godon et al. 2016). In Section 3, we analyse the 31 systems in which the white dwarf signature is easily recognizable from a broad Ly α absorption profile.

Sample light curves for four targets in our sample that have been observed in quiescence. The blue line represents the date of the HST observation, which has been subtracted from the Julian date on the x-axis. Note the different time range on the x-axis.
Figure 3.

Sample light curves for four targets in our sample that have been observed in quiescence. The blue line represents the date of the HST observation, which has been subtracted from the Julian date on the x-axis. Note the different time range on the x-axis.

Sample light curves for four targets in our sample that have been observed close to an outburst or in an intermediate state. The blue line represents the date of the HST observation, which has been subtracted from the Julian date on the x-axis. Note the different time range on the x-axis. The data have been retrieved from the AAVSO data base.
Figure 4.

Sample light curves for four targets in our sample that have been observed close to an outburst or in an intermediate state. The blue line represents the date of the HST observation, which has been subtracted from the Julian date on the x-axis. Note the different time range on the x-axis. The data have been retrieved from the AAVSO data base.

HST/COS spectra of the nine CVs dominated by emission from the accretion flow, outshining the white dwarf. Strong emission lines of C iii (1175 Å), N v (1242 Å), C ii (1335 Å), Si iv (1400 Å), C iv (1550 Å) and He ii (1640 Å) are clearly visible. The wavelength ranges affected by the geocoronal emission lines of Ly α (1216 Å) and O i (1302 Å) are plotted in grey.
Figure 5.

HST/COS spectra of the nine CVs dominated by emission from the accretion flow, outshining the white dwarf. Strong emission lines of C iii (1175 Å), N v (1242 Å), C ii (1335 Å), Si iv (1400 Å), C iv (1550 Å) and He ii (1640 Å) are clearly visible. The wavelength ranges affected by the geocoronal emission lines of Ly α (1216 Å) and O i (1302 Å) are plotted in grey.

2.2 STIS observations

The STIS data were collected as part of two snapshot programmes (programmes ID 9357 and 9724) in Cycle 11 and 12 (Table 2). Snapshot programmes are designed to fill short gaps in the weekly HST observing schedule; therefore, each CV was observed with exposure times of only 600–900 s, through the 52 arcsec × 0.2 arcsec aperture. We used the G140L grating at the central wavelength 1425 Å and the FUV-Multi-Anode Microchannel Array (MAMA) detector to obtain spectra covering the wavelength range 1150–1700 Å at a nominal resolution of R ≃ 1000.

Table 2.

Log of the HST/STIS observations. The systems are ordered by orbital period. The fourth column reports the instrumental magnitudes measured from the acquisition images, which were obtained through the F28 × 50LP filter.

SystemPorbTypeF28 × 50 LPE(B − V)ObservationNumberTotalState
(min)(mag)(mag)dateofexposure
orbitstime (s)
V485 Cen59.03SU UMa17.90.071a2004 Apr 151900q
V844 Her78.69SU UMa17.40.013b2003 Feb 231900q
UV Per93.44SU UMa17.90.0c2002 Oct 111900q
RZ Sge98.32SU UMa18.00.302a2003 Jun 131900q
CY UMa100.18SU UMa17.30.012a2002 Dec 271830q
QZ Ser119.75SU UMa16.90.038b2003 Oct 071900q
DV UMa123.62SU UMa18.60.014b2004 Feb 081900q
BD Pav258.19U Gem14.60.0c2003 Feb 091600q
SystemPorbTypeF28 × 50 LPE(B − V)ObservationNumberTotalState
(min)(mag)(mag)dateofexposure
orbitstime (s)
V485 Cen59.03SU UMa17.90.071a2004 Apr 151900q
V844 Her78.69SU UMa17.40.013b2003 Feb 231900q
UV Per93.44SU UMa17.90.0c2002 Oct 111900q
RZ Sge98.32SU UMa18.00.302a2003 Jun 131900q
CY UMa100.18SU UMa17.30.012a2002 Dec 271830q
QZ Ser119.75SU UMa16.90.038b2003 Oct 071900q
DV UMa123.62SU UMa18.60.014b2004 Feb 081900q
BD Pav258.19U Gem14.60.0c2003 Feb 091600q

Notes. The E(B − V) data have been retrieved from: athe NASA/IPAC Extragalactic Database (NED); bthe three-dimensional map of interstellar dust reddening based on Pan-STARRS 1 and 2MASS photometry (Green et al. 2015); cUV Per: Szkody (1985), BD Pav: Sion et al. (2008). The NED data are the Galactic colour excess and represent an upper limit for the actual reddening while the Pan-STARRS data are the actual reddening for the systems with a known distance. The last column reports the state of the system during the HST observations: q – quiescence.

Table 2.

Log of the HST/STIS observations. The systems are ordered by orbital period. The fourth column reports the instrumental magnitudes measured from the acquisition images, which were obtained through the F28 × 50LP filter.

SystemPorbTypeF28 × 50 LPE(B − V)ObservationNumberTotalState
(min)(mag)(mag)dateofexposure
orbitstime (s)
V485 Cen59.03SU UMa17.90.071a2004 Apr 151900q
V844 Her78.69SU UMa17.40.013b2003 Feb 231900q
UV Per93.44SU UMa17.90.0c2002 Oct 111900q
RZ Sge98.32SU UMa18.00.302a2003 Jun 131900q
CY UMa100.18SU UMa17.30.012a2002 Dec 271830q
QZ Ser119.75SU UMa16.90.038b2003 Oct 071900q
DV UMa123.62SU UMa18.60.014b2004 Feb 081900q
BD Pav258.19U Gem14.60.0c2003 Feb 091600q
SystemPorbTypeF28 × 50 LPE(B − V)ObservationNumberTotalState
(min)(mag)(mag)dateofexposure
orbitstime (s)
V485 Cen59.03SU UMa17.90.071a2004 Apr 151900q
V844 Her78.69SU UMa17.40.013b2003 Feb 231900q
UV Per93.44SU UMa17.90.0c2002 Oct 111900q
RZ Sge98.32SU UMa18.00.302a2003 Jun 131900q
CY UMa100.18SU UMa17.30.012a2002 Dec 271830q
QZ Ser119.75SU UMa16.90.038b2003 Oct 071900q
DV UMa123.62SU UMa18.60.014b2004 Feb 081900q
BD Pav258.19U Gem14.60.0c2003 Feb 091600q

Notes. The E(B − V) data have been retrieved from: athe NASA/IPAC Extragalactic Database (NED); bthe three-dimensional map of interstellar dust reddening based on Pan-STARRS 1 and 2MASS photometry (Green et al. 2015); cUV Per: Szkody (1985), BD Pav: Sion et al. (2008). The NED data are the Galactic colour excess and represent an upper limit for the actual reddening while the Pan-STARRS data are the actual reddening for the systems with a known distance. The last column reports the state of the system during the HST observations: q – quiescence.

Similar to the COS FUV detector, the MAMA detector is also subject to damage by excessive illumination but, contrary to the COS programme, the snapshot programmes did not have a long-term schedule that could allow detailed monitoring before the STIS observations. We analysed the STIS acquisition images to determine the source brightness immediately before the spectrum acquisition. These images were acquired with the F28 × 50LP filter (central wavelength of 7228.5 Å and full width at half-maximum of 2721.6 Å). We determined the corresponding magnitude following the method described in Araujo-Betancor et al. (2005b). By comparison with published magnitudes and the system brightness in the Sloan Digital Sky Survey (SDSS) and AAVSO Photometric All-Sky Survey (APASS), we verified that all the targets were observed in quiescence.

These snapshot programmes produced ultraviolet spectra of 69 CVs (e.g. Gänsicke et al. 2003; Rodríguez-Gil et al. 2004; Araujo-Betancor et al. 2005a). Here, we analyse the remaining eight objects in which the white dwarf dominates the ultraviolet emission. We show three sample STIS spectra of quiescent CVs in the left-hand panel of Fig. 2 where the broad Ly α absorption centred on 1216 Å reveals the white dwarf photosphere.

Three of the eight systems observed by STIS (BD Pav, QZ Ser and V485 Cen) are in common with the COS sample and we present a detailed comparison of the two data sets in Section 4.2.2.

Adding the five additional CVs observed with STIS to the 31 from the COS survey results in our total sample of 36 CVs in which the white dwarf dominates the overall spectral emission.

3 DATA ANALYSIS

Ultraviolet spectra are particularly suitable for the study of CV white dwarfs because, at these wavelengths, the spectral energy distribution is often dominated by the white dwarf while the donor star does not contribute at all. However, some contamination from the disc, the bright spot (the region where the ballistic stream from the companion intersects the disc) or the boundary layer (the interface between the accretion disc and the white dwarf) can dilute the emission from the white dwarf photosphere. As described in Section 2.1, the overall shape of a white dwarf ultraviolet spectrum is determined by its effective temperature: hotter white dwarfs have narrow Ly α profiles and steep blue continua, while cooler white dwarfs are characterized by broad Ly α profiles and flat continua. Therefore, the white dwarf effective temperature can be accurately measured by fitting the HST data with synthetic white dwarf atmosphere models.

In Fig. 6, we show the COS data of 1RXS J023238.8−371812 as an example of a typical CV spectrum from our sample. The broad Ly α absorption at ≃1216 Å, the quasi-molecular absorption bands of H|$_2^{+}$| at ≃1400 Å and several sharp absorption lines (e.g. C i 1460/1490 Å, Si ii 1526/1533 Å, C i 1657 Å) reveal the white dwarf photosphere. The white dwarf dominates the ultraviolet emission but the non-zero flux detected in the core of the Ly α suggests the presence of a secondary continuum component whose origin is still not clear. It has been argued that this second component could arise from the bright spot, from a hot boundary layer, or from the disc (Long et al. 1993; Godon et al. 2004; Gänsicke et al. 2005). In addition, we detect emission lines, which are broadened by the Keplerian velocity distribution of the disc. A model to fit the data has to account for these three contributions (white dwarf, second component and emission lines) detected in a CV spectrum.

HST/COS spectrum of 1RXS J023238.8−371812. Plotted in green are the emission lines of C iii (1175 Å), N v (1242 Å), C ii (1335 Å), Si iv (1400 Å), C iv (1550 Å) and He ii (1640 Å). The red band underlines the position of the H$_2^{+}$ quasi-molecular absorption bands. The blue band highlights the presence of a second, flat continuum component that, in this case, contributes ≃10 per cent of the observed flux. The geocoronal emission lines of Ly α (1216 Å) and O i (1302 Å) are plotted in grey.
Figure 6.

HST/COS spectrum of 1RXS J023238.8−371812. Plotted in green are the emission lines of C iii (1175 Å), N v (1242 Å), C ii (1335 Å), Si iv (1400 Å), C iv (1550 Å) and He ii (1640 Å). The red band underlines the position of the H|$_2^{+}$| quasi-molecular absorption bands. The blue band highlights the presence of a second, flat continuum component that, in this case, contributes ≃10 per cent of the observed flux. The geocoronal emission lines of Ly α (1216 Å) and O i (1302 Å) are plotted in grey.

We used tlusty and synspec (Hubeny 1988; Hubeny & Lanz 1995) to compute a grid of synthetic spectra of white dwarf atmospheres, covering Teff = 10 000–70 000 K in steps of 100 K, and metal abundances Z of 0.01, 0.10, 0.20, 0.50 and 1.00 times their solar values.2

Ideally, a spectral fit to the ultraviolet data would provide both Teff and the surface gravity (log g). However, these two quantities correlate: an increase in the temperature translates into a larger fraction of ionized hydrogen and narrower Lyman and Balmer lines; this effect can be counterbalanced by a higher gravity that increases pressure broadening. It is not possible to break this degeneracy from the sole analysis of the HST data, since they only provide the Ly α absorption profile that, in the case of cool CV white dwarfs, is limited to only the red wing of the line. Therefore, we needed to make an assumption on the surface gravity. Most previously published work analysing CV white dwarf ultraviolet spectra assumed log g = 8.00, corresponding to 0.6 M, the average mass of isolated white dwarfs (Koester, Schulz & Weidemann 1979; Liebert, Bergeron & Holberg 2005; Kepler et al. 2007), unless an independent white dwarf mass determination was available. However, Zorotovic et al. (2011) demonstrated that the average mass of white dwarfs in CVs is actually higher than that of isolated white dwarfs, ≃0.8 M (log g ≃ 8.35). Since the canonical assumption log g = 8.00 does not reflect the observed average mass of CV white dwarfs, we generated our grid of models assuming log g = 8.35.

The COS ultraviolet spectra are contaminated by geocoronal emission of Ly α and O i 1302 Å, and we masked these wavelength regions for our spectral analysis. Furthermore, we noticed the presence of an additional continuum component in all our systems, which contributes ≃10–30 per cent of the observed flux. In order to account for this, we included in the fit a blackbody, a power law or a constant flux3 (in Fλ), which can reproduce different slopes in the second component and are representative of different physical processes (thermalized emission in the case of the blackbody, optically thin emission in the case of the power law). Using a χ2 minimization routine, we fitted the grid of model spectra to the HST data and measured the effective temperatures of the 36 CV white dwarfs.

To investigate the influence of the disc emission lines on our fitting procedure, we carried out our spectral analysis using two different methods: (i) we masked all the emission lines (Mask); (ii) we included the emission lines as Gaussian profiles, allowing three free parameters: amplitude, wavelength and width (Gaussian fit).

We illustrate the differences between the two methods using 1RXS J023238.8−371812. Fig. 7 shows the COS spectrum along with the best-fitting models obtained masking the emission lines (left-hand panels) and including the lines in the fit (right-hand panels), for all three different second components (from top to bottom: blackbody, power law and constant). The temperatures measured with the two methods typically only differ by ≃3 K (see Table 3), demonstrating that including or masking the disc lines has no influence on the fit result (see also Szkody et al. 2010). Therefore, to use as much of the data as possible, we decided to include the lines in the fit (Gaussian fit).

HST/COS spectrum of 1RXS J023238.8−371812 [black – the disc emission lines of C iii (1175 Å), N v (1242 Å), C ii (1335 Å), C iv (1550 Å) and He ii (1640 Å) are clearly visible; weak emission from Si iv can be identified at ≃1400 Å], along with the best-fitting model (red) for the two different fitting methods: masking the emission lines (left-hand panels) and including them as Gaussian profiles (right-hand panels). The flux in the core of Ly α does not go to zero, implying the presence of a second continuum component (blue) that has been included in the fit in the form of a blackbody (BB), a power law (PL) or a constant (const). Masking the emission lines from the disc (grey in the left-hand panels) or including them as a Gaussian profile (green in the right-hand panels) returns very similar effective temperatures, within the statistical errors (Table 3). Note that the geocoronal emission lines, Ly α (1216 Å) and O i (1302 Å), have always been masked.
Figure 7.

HST/COS spectrum of 1RXS J023238.8−371812 [black – the disc emission lines of C iii (1175 Å), N v (1242 Å), C ii (1335 Å), C iv (1550 Å) and He ii (1640 Å) are clearly visible; weak emission from Si iv can be identified at ≃1400 Å], along with the best-fitting model (red) for the two different fitting methods: masking the emission lines (left-hand panels) and including them as Gaussian profiles (right-hand panels). The flux in the core of Ly α does not go to zero, implying the presence of a second continuum component (blue) that has been included in the fit in the form of a blackbody (BB), a power law (PL) or a constant (const). Masking the emission lines from the disc (grey in the left-hand panels) or including them as a Gaussian profile (green in the right-hand panels) returns very similar effective temperatures, within the statistical errors (Table 3). Note that the geocoronal emission lines, Ly α (1216 Å) and O i (1302 Å), have always been masked.

The uncertainties of the individual fits listed in Table 3 are purely statistical, as derived from the fitting procedure. They are unrealistically small and do not reflect the real uncertainties, which are instead dominated by several systematic effects, analysed in the following sections.

Table 3.

Results for 1RXS J023238.8−371812 for the two different fitting methods for the disc emission lines, in which we either mask the emission lines (Mask) or include them as Gaussian profiles (Gaussian fit). We fixed log g = 8.35. The last two rows (average) report the mean and the standard deviations for each method.

EmissionSecondTeff (K)dofχ2
linescomponent
MaskBlackbody13 543 ± 3618561794
MaskPower law13 574 ± 3618561808
MaskConstant13 462 ± 2818571861
Gaussian fitBlackbody13 540 ± 3421912170
Gaussian fitPower law13 573 ± 3421912186
Gaussian fitConstant13 466 ± 2621922245
MaskAverage13 526 ± 57
Gaussian fitAverage13 526 ± 55
EmissionSecondTeff (K)dofχ2
linescomponent
MaskBlackbody13 543 ± 3618561794
MaskPower law13 574 ± 3618561808
MaskConstant13 462 ± 2818571861
Gaussian fitBlackbody13 540 ± 3421912170
Gaussian fitPower law13 573 ± 3421912186
Gaussian fitConstant13 466 ± 2621922245
MaskAverage13 526 ± 57
Gaussian fitAverage13 526 ± 55
Table 3.

Results for 1RXS J023238.8−371812 for the two different fitting methods for the disc emission lines, in which we either mask the emission lines (Mask) or include them as Gaussian profiles (Gaussian fit). We fixed log g = 8.35. The last two rows (average) report the mean and the standard deviations for each method.

EmissionSecondTeff (K)dofχ2
linescomponent
MaskBlackbody13 543 ± 3618561794
MaskPower law13 574 ± 3618561808
MaskConstant13 462 ± 2818571861
Gaussian fitBlackbody13 540 ± 3421912170
Gaussian fitPower law13 573 ± 3421912186
Gaussian fitConstant13 466 ± 2621922245
MaskAverage13 526 ± 57
Gaussian fitAverage13 526 ± 55
EmissionSecondTeff (K)dofχ2
linescomponent
MaskBlackbody13 543 ± 3618561794
MaskPower law13 574 ± 3618561808
MaskConstant13 462 ± 2818571861
Gaussian fitBlackbody13 540 ± 3421912170
Gaussian fitPower law13 573 ± 3421912186
Gaussian fitConstant13 466 ± 2621922245
MaskAverage13 526 ± 57
Gaussian fitAverage13 526 ± 55

3.1 The unknown nature of the second component

The first systematic uncertainty in our fitting procedure arises from the unknown nature of the additional emission component. The blackbody, the power law or the constant are not constrained outside the ultraviolet wavelength range, and only serve to account for different slopes in the detected additional continuum component. They thus represent a very simplified model of the additional continuum contribution and it is likely that none of them provide a realistic physical description of this emission component.

From a statistical point of view, and owing to the limited wavelength coverage of our data, we cannot discriminate among the three of them, and they all result in fits of similar quality and in very similar temperatures for the white dwarf (see Table 3). These differences in Teff reflect a systematic effect related to presence of this additional flux. For this reason, we decided to adopt as final Teff measurement the mean of the results obtained with the three different additional components. To evaluate the magnitude of the related systematic uncertainty, we calculated both the standard deviation of the Teff values obtained with the three different additional components and the sum in quadrature of the statistical errors of the individual fits. We assumed as final and more realistic estimate for the systematic uncertainty the larger of these two. Additional systematic effects are analysed in the following sections.

3.2 The unknown white dwarf mass

As pointed out above, the temperature and mass of a white dwarf correlate. Table 4 reports the effective temperatures of 1RXS J023238.8−371812 allowing different log g (= different white dwarf masses). These results show that an assumption on log g translates into an accurate measurement of the temperature for a given mass (≃50 K), while the systematic uncertainty introduced considering different surface gravities is typically an order of magnitude larger (≃500 K). Therefore, the dominant source of error is the (unknown) white dwarf mass and we used the following approach to evaluate how this systematic uncertainty depends on Teff.

Table 4.

Teff for 1RXS J023238.8−371812 allowing different log g, corresponding to different white dwarf masses. These results have been obtained fitting the data including the emission lines as Gaussian profiles, and using three different models for the second component.

Teff (K)Teff (K)Teff (K)
Secondlog g = 8.00log g = 8.35log g = 8.60
componentMWD = 0.6 MMWD = 0.8 MMWD = 1.0 M
Blackbody13 016 ± 2813 540 ± 3413 938 ± 37
Power law13 045 ± 2913 573 ± 3413 972 ± 37
Constant12 949 ± 2313 466 ± 2613 848 ± 28
Average13 003 ± 4913 526 ± 5513 919 ± 64
Teff (K)Teff (K)Teff (K)
Secondlog g = 8.00log g = 8.35log g = 8.60
componentMWD = 0.6 MMWD = 0.8 MMWD = 1.0 M
Blackbody13 016 ± 2813 540 ± 3413 938 ± 37
Power law13 045 ± 2913 573 ± 3413 972 ± 37
Constant12 949 ± 2313 466 ± 2613 848 ± 28
Average13 003 ± 4913 526 ± 5513 919 ± 64
Table 4.

Teff for 1RXS J023238.8−371812 allowing different log g, corresponding to different white dwarf masses. These results have been obtained fitting the data including the emission lines as Gaussian profiles, and using three different models for the second component.

Teff (K)Teff (K)Teff (K)
Secondlog g = 8.00log g = 8.35log g = 8.60
componentMWD = 0.6 MMWD = 0.8 MMWD = 1.0 M
Blackbody13 016 ± 2813 540 ± 3413 938 ± 37
Power law13 045 ± 2913 573 ± 3413 972 ± 37
Constant12 949 ± 2313 466 ± 2613 848 ± 28
Average13 003 ± 4913 526 ± 5513 919 ± 64
Teff (K)Teff (K)Teff (K)
Secondlog g = 8.00log g = 8.35log g = 8.60
componentMWD = 0.6 MMWD = 0.8 MMWD = 1.0 M
Blackbody13 016 ± 2813 540 ± 3413 938 ± 37
Power law13 045 ± 2913 573 ± 3413 972 ± 37
Constant12 949 ± 2313 466 ± 2613 848 ± 28
Average13 003 ± 4913 526 ± 5513 919 ± 64

As shown by Zorotovic et al. (2011), the average mass of CV white dwarfs is 0.83 ± 0.23 M and we therefore investigated the correlation between effective temperature and log  g in the mass range 0.6 M(log  g = 8.00) to 1.0 M(log  g = 8.60). We fitted our HST data assuming log  g = 8.00, 8.35 and 8.60 for each metallicity and for each type of second component, resulting in 15 effective temperatures (five metallicities × three second components) for each log  g, for each object. We define4 as T8.00 = Teff (log  g = 8.00), T8.35 = Teff (log  g = 8.35) and T8.60 = Teff (log  g = 8.60), and calculated Δ+Teff = T8.00 − T8.35, and ΔTeff = T8.60 − T8.35.

We excluded from this analysis the eclipsing systems IY UMa, SDSS J040714.78−064425.1 and SDSS J100658.41+233724.4 for which disc absorption along the line of sight makes the identification of the continuum flux level difficult (Section 4.4). We also did not include CC Scl and SDSS J164248.52+134751.4 for which a reliable effective temperature determination was not possible (Section 4.2), and SDSS J153817.35+512338.0 because the core of its narrow Ly α line is strongly contaminated by geocoronal airglow emission that makes the data less sensitive to a change in the model surface gravity.

The remaining objects have typically Teff ≲ 21 000 K, with the exception of HS2214+2845 (Teff ≃ 26 000 K). To better constrain Δ+Teff and ΔTeff and to verify the validity of this relationship at high temperatures, we included in our analysis two additional hotter objects: SS Aur (Teff = 34 000 ± 2000 K for log  g = 8.8; Sion et al. 2008) and DW UMa (Teff = 50 000 ± 1000 K for log  g = 8.00 and Z = 0.71 Z; Araujo-Betancor et al. 2003). Both these objects have been observed with STIS, which allows the removal of the contamination from geocoronal emission and therefore, differently from SDSS1538 in our sample, they can be used to constrain the relationship at high temperatures.

We retrieved the STIS spectrum of SS Aur and the out-of-eclipse STIS low-state spectrum of DW UMa (Knigge et al. 2000) from the HST data archive. Following the same method as for the CVs in our sample, we fitted these data assuming log g = 8.00, 8.35 and 8.60. For SS Aur we found: T8.00 = 26 269 ± 275 K, T8.35 = 27 507 ± 282 K and T8.60 = 28 402 ± 270 K for Z = 0.1 Z. In the case of DW UMa, we assumed Z = 0.71 Z, and obtained T8.00 = 49 900 ± 844 K, in agreement with Araujo-Betancor et al. (2003), T8.35 = 52 532 ± 893 K and T8.60 = 54 282 ± 986 K, respectively.

Fig. 8 shows the trend of Δ+Teff and ΔTeff as a function of Teff (log  g = 8.35). These correlations are well fit with the following relation:
(1)
where a = 1054(2) K, b = 0.000 1052(7) K−1 for Δ+Teff, and a = −1417(2) K, b = 0.000 1046(5) K−1 for ΔTeff.
Best fit to Δ+ Teff = Teff(log g = 8.60) − Teff(log g = 8.35) and Δ− Teff = Teff(log g = 8.00) − Teff(log g = 8.35), as a function of Teff(log g = 8.35), for the five metallicities and the three additional continuum second components (red for blackbody, blue for power law and gold for constant). The fit excludes the effective temperatures of (i) the eclipsing systems IY UMa, SDSS J040714.78−064425.1 and SDSS J100658.41+233724.4 for which disc absorption along the line of sight makes the identification of the continuum flux level difficult (Section 4.4); (ii) CC Scl and SDSS J164248.52+134751.4 for which a reliable effective temperature determination was not possible (Section 4.2); (iii) SDSS J153817.35+512338.0 because the core of its narrow Ly α line is strongly contaminated by geocoronal airglow emission that makes the data less sensitive to a change in the model surface gravity. DW UMa was not included in the fit, but serves as independent test of the fit.
Figure 8.

Best fit to Δ+Teff = Teff(log g = 8.60) − Teff(log g = 8.35) and ΔTeff = Teff(log g = 8.00) − Teff(log g = 8.35), as a function of Teff(log g = 8.35), for the five metallicities and the three additional continuum second components (red for blackbody, blue for power law and gold for constant). The fit excludes the effective temperatures of (i) the eclipsing systems IY UMa, SDSS J040714.78−064425.1 and SDSS J100658.41+233724.4 for which disc absorption along the line of sight makes the identification of the continuum flux level difficult (Section 4.4); (ii) CC Scl and SDSS J164248.52+134751.4 for which a reliable effective temperature determination was not possible (Section 4.2); (iii) SDSS J153817.35+512338.0 because the core of its narrow Ly α line is strongly contaminated by geocoronal airglow emission that makes the data less sensitive to a change in the model surface gravity. DW UMa was not included in the fit, but serves as independent test of the fit.

We included the SS Aur temperatures in the fit of Δ+Teff and ΔTeff to better constrain the relationship at high temperatures. In contrast, we did not include the DW UMa temperatures and we only overplot them in Fig. 8 to illustrate that our best-fitting is in good agreement with this independent measurement.

The two best-fitting curves represent the systematic uncertainty |$\sigma _{T_{\mathrm{eff}}}$| due to the unknown mass of the white dwarf. The two curves are not symmetric (since the relationship between log  g and the white dwarf mass is not linear), resulting in asymmetric error bars with ΔTeff > Δ+Teff. However, to simplify our discussion, we adopted as final uncertainty the larger value derived from ΔTeff:
(2)

In summary, we found that the systematic uncertainty due to the unknown white dwarf mass lies in the range 300–1800 K. Once the masses for each system are accurately determined, the degeneracy between Teff and log  g will be broken, reducing the uncertainties in Teff to those related to the unknown nature of the second additional component (see Section 3.1).

3.3 Reddening

Reddening due to interstellar dust along the line of sight can introduce an additional systematic uncertainty in the effective temperature determination as it affects the overall slope of the ultraviolet spectra. However, CVs are intrinsically faint and thus we are observationally biased towards nearby systems, for which extinction is usually negligible. Moreover, owing to their colour similarity with quasars, CVs are often discovered by extragalactic surveys (such as SDSS), which cover high Galactic latitudes, and are therefore not heavily affected by reddening. To verify that reddening is a minor contribution to the total error budget, for all the systems in our sample, we compiled the colour excess of our CVs (Tables 1 and 2) using the three-dimensional map of interstellar dust reddening based on the Panoramic Survey Telescope and Rapid Response System (Pan-STARRS) 1 and the Two Micron All-Sky Survey (2MASS) photometry (Green et al. 2015) wherever possible, i.e. when the distance is known and the object is inside the field covered by this map. For the remaining objects, we report either the value from the literature where available or the Galactic E(B − V) from the NASA/IPAC Extragalactic Database (NED), which only represents an upper limit for the actual reddening. Finally, for CU Vel, we determined its colour excess below (Section 4.3.1).

To establish how the interstellar absorption affects our analysis, we considered one of the systems with zero colour excess, UV Per, and reddened its spectrum using the relationship given by Cardelli, Clayton & Mathis (1989) for a range of values in E(B − V). Since we previously determined the effective temperature for this CV white dwarf, Teff[E(B − V) = 0] = 14 389 ± 578 K, we can use this ‘artificially reddened’ data set to study the variation of Teff as a function of reddening. We fitted the reddened spectra following the prescription from Sections 3 and 3.1 and show the derived temperatures in Fig. 9. The interstellar absorption introduces a variation in Teff greater than the systematic uncertainties defined in Section 3.1 (blue dashed lines) for E(B − V) ≳ 0.1, which we assumed as the threshold above which the effect of the reddening cannot be neglected. Only one system in our sample has a colour excess significantly higher than this value: RZ Sge, E(B − V) = 0.302, as returned from the NED data base. However, Sagittarius lies on the Galactic plane and this E(B − V) represents an estimate over the entire Galactic column. Given the typical distances of CVs, the actual reddening of RZ Sge is likely to be lower than that. We assumed the mass–radius relationship from Verbunt & Rappaport (1988) and, using the scaling factors from the fit to the STIS data for different surface gravities (Section 3.2), we estimated the distance to RZ Sge to lie in the range 262 pc ≲ d ≲ 335 pc, for 0.6 M ≤ MWD ≤ 0.8 M. From the three-dimensional map of interstellar dust reddening (Green et al. 2015), we found 0.044 ≲ E(B − V) ≲ 0.070, well below the threshold we established above. We therefore considered negligible the reddening for this system.

Best-fitting effective temperatures for UV Per, obtained by reddening the HST/STIS data for increasing values of E(B − V). The blue lines show the systematic uncertainties on the effective temperature derived from the fit to the original data (E(B − V) = 0), following the method described in Section 3.1. They establish the threshold above which the effect of interstellar absorption on our Teff is greater than the systematic uncertainties, i.e. E(B − V) ≃ 0.1.
Figure 9.

Best-fitting effective temperatures for UV Per, obtained by reddening the HST/STIS data for increasing values of E(B − V). The blue lines show the systematic uncertainties on the effective temperature derived from the fit to the original data (E(B − V) = 0), following the method described in Section 3.1. They establish the threshold above which the effect of interstellar absorption on our Teff is greater than the systematic uncertainties, i.e. E(B − V) ≃ 0.1.

Finally, interstellar gas along the line of sight can also contaminate the observed spectrum with additional Ly α absorption. Using the relation between interstellar neutral hydrogen column density and reddening from Diplas & Savage (1994), we determined that this contribution is always of the order of few angstrom [≃3 Å for E(B − V) = 0.05 up to ≃7 Å for E(B − V) = 0.3] and therefore much narrower than the white dwarf Ly α absorption line. In fact, the interstellar Ly α absorption is located in the spectral region that we always masked owing to geocoronal airglow emission, which typically has a width of ≃18 Å, and therefore we concluded that interstellar Ly α absorption has no effect on our results.

3.4 Other possible systematic effects

To review all the systematic uncertainties in a way as comprehensive as possible, we need to discuss the possibility of Ly α absorption from the additional non-white dwarf component and inaccuracies in the instrument calibration.

Although not much is known about the physical origin of the second component, it is likely to arise from a hot optically thick (e.g. the bright spot) or a hot optically thin medium surrounding a cooler optically thick layer (e.g. the disc or the boundary layer). It is therefore possible that the second component can contribute, to some extent, to the observed Ly α absorption. The Ly α profile is, along with the spectral slope, the main tracer of the white dwarf temperature, and such a hypothetical contamination could systematically affect our results. Long et al. (2009) investigated an additional Ly β absorption in VW Hyi finding that it most likely originates from a hotspot region whose emission can be approximated by a stellar model with log  g ≃ 4. The Lyman absorption lines arising from such an environment are consequently significantly narrower than the white dwarf Ly α absorption itself, which is broadened by the higher pressure on the white dwarf surface at log g ≃ 8.35. Thus, although the model we used to describe the additional component does not account for the possibility of absorption in the Ly α region, such contamination (if present) would not appreciably affect our effective temperature determination.

Finally, limitations in the instrument calibration may affect our results. Massa et al. (2014) report that the systematic uncertainties in the COS G140L flux calibration are less than 2 per cent for λ < 1200 Å and 1 per cent for 1200 Å < λ < 1900 Å, with an increase up to 6 per cent at λ = 2150 Å. Owing to a decrease in the detector sensitivity in the red portion of the spectrum, we only considered the wavelength range 1150 Å < λ < 1730 Å, for which systematic uncertainties are less than 2 per cent. The maximum effect on our results can be evaluated by multiplying the COS spectra with a linear function with a 2 per cent slope. To assess also for possible dependences with the temperature of the white dwarf, we choose three systems representative of cool, warm and hot white dwarfs: 1RXS J105010.8−140431, SDSS J123813.73−033932.9 and HS 2214+2845. We fitted their spectra after applying the 2 per cent slope in flux calibration and find that the resulting Teff values are in agreement, within the uncertainties, with the one we derived from the original COS data. We therefore conclude that our analysis is not affected by the very small uncertainty in the COS instrument calibration.

Three objects in our sample have been observed both with STIS and COS. In Section 4.2.2, we compare the two data sets and, for this comparison to be reliable, we needed to verify that the STIS and COS calibrations agree. To do so, we retrieved from the HST archive the STIS and COS data of the flux standard WD 0308–565. We overplot the one available STIS spectrum and the COS data acquired at different epochs, finding that the STIS spectrum matches the flux level of all the COS data. With a linear fit to the ratio between the two data sets, we determined that they differ, on average, by ≃3 per cent. This comparison proves that uncertainties in the STIS calibration are comparable to the systematic uncertainties of COS and therefore they are negligible in our analysis. Finally, we can also conclude that the differences in the STIS and COS effective temperatures discussed in Sections 4.2.2 are not related to calibration issues of the two instruments.

We followed the procedure outlined in the previous sections to fit the HST data of the 36 CVs and summarize the results in Table 5. Fig. 10 shows three examples of best-fitting models obtained with this procedure: 1RXS J105010.8−140431 (top panel), SDSS J123813.73−033932.9 (middle panel) and HS 2214+2845 (bottom panel), which are representative of different temperature regimes (cool, intermediate and hot, respectively). All the spectra, along with their best-fitting models, are available in the online material.

Ultraviolet spectra (black) of cool, warm and hot CV white dwarfs in our sample along with the best-fitting model (red) assuming a blackbody second component. The quasi-molecular absorption bands of H$_2^{+}$ and of H2 are visible at ≃1400 Å and ≃1600 Å for Teff ≲ 19 000 K and Teff ≲ 13 500 K, respectively (Koester et al. 1985; Nelan & Wegner 1985). The geocoronal emission lines of Ly α (1216 Å) and O i (1302 Å) are plotted in grey.
Figure 10.

Ultraviolet spectra (black) of cool, warm and hot CV white dwarfs in our sample along with the best-fitting model (red) assuming a blackbody second component. The quasi-molecular absorption bands of H|$_2^{+}$| and of H2 are visible at ≃1400 Å and ≃1600 Å for Teff ≲ 19 000 K and Teff ≲ 13 500 K, respectively (Koester et al. 1985; Nelan & Wegner 1985). The geocoronal emission lines of Ly α (1216 Å) and O i (1302 Å) are plotted in grey.

Table 5.

Characteristics of the 45 CV white dwarfs observed with COS and STIS.

SystemPorbdMWDReferencesZTeff±WDInstrument
(min)(pc)(M)(Z)(K)(K)contribution
V485 Cen59.0310.515 20065556 per centSTIS
GW Lib76.78|$140^{+30}_{-20}$|2, 30.216 995↓81285 per centCOS
SDSS J143544.02+233638.778.0040.0111 94031584 per centCOS
OT J213806.6+26195778.1050.216 29275369 per centCOS
V844 Her78.69290 ± 303, 60.114 85062261 per centSTIS
SDSS J013701.06−091234.879.71300 ± 807, 80.114 54759477 per centCOS
SDSS J123813.73−033932.980.5211090.518 35892275 per centCOS
PU CMa81.6310COS
V1108 Her81.87130 ± 3011, 121.013 64350381 per centCOS
ASAS J002511+1217.282.00130 ± 3012, 130.112 83041677 per centCOS
SDSS J103533.02+055158.482.22170 ± 120.835 ± 0.00914, 150.0111 62044a85 per centCOS
CC Scl84.10160.216 855:80135 per centCOS
SDSS J075507.70+143547.684.76170.515 86271690 per centCOS
1RXS J105010.8−14043188.56100 ± 5018, 190.111 62227789 per centCOS
MR UMa91.17200.215 182↓65469 per centCOS
QZ Lib92.36120 ± 50190.0111 30323864 per centCOS
SDSS J153817.35+512338.093.11170.0133 855178594 per centCOS
UV Per93.44210.214 38957875 per centSTIS
1RXS J023238.8−37181295.04160220.213 52749178 per centCOS
SDSS J093249.57+472523.095.4817COS
RZ Sge98.32200.515 28766356 per centSTIS
CY UMa100.18230.115 23265861 per centSTIS
BB Ari101.2024, 250.214 948↓63283 per centCOS
DT Oct104.5424, 25COS
IY UMa106.43190 ± 600.79 ± 0.0426, 271.017 750↓1000a77 per centCOS
SDSS J100515.38+191107.9107.60170.215 94472374 per centCOS
RZ Leo110.17340 ± 11028, 290.515 01463883 per centCOS
CU Vel113.04150 ± 5029, 300.115 33666889 per centCOS
AX For113.04|$370^{+20}_{-60}$|25, 311.016 571↓77768 per centCOS
SDSS J164248.52+134751.4113.60321.017 710:87148 per centCOS
QZ Ser119.75|$460^{+150}_{-110}$|330.214 48158768 per centSTIS
DV UMa123.62504 ± 301.098 ± 0.02415, 341.018 874182a92 per centSTIS
IR Com125.3430022, 351.016 61878186 per centCOS
SDSS J001153.08−064739.2144.40360.113 85452563 per centCOS
OR And195.7025COS
BB Dor221.901500 ± 50037COS
SDSS J040714.78−064425.1245.04381.020 885110467 per centCOS
CW Mon254.3029725, 39COS
V405 Peg255.81|$149^{+26}_{-20}$|40COS
HS 2214+2845258.02410.526 443↓143684 per centCOS
BD Pav258.1950042, 430.517 77587692 per centSTIS
SDSS J100658.41+233724.4267.71676 ± 400.78 ± 0.12441.016 0001000a96 per centCOS
HM Leo268.9935045COS
HS 0218+3229428.021000460.217 99089370 per centCOS
HS 1055+0939541.8825COS
SystemPorbdMWDReferencesZTeff±WDInstrument
(min)(pc)(M)(Z)(K)(K)contribution
V485 Cen59.0310.515 20065556 per centSTIS
GW Lib76.78|$140^{+30}_{-20}$|2, 30.216 995↓81285 per centCOS
SDSS J143544.02+233638.778.0040.0111 94031584 per centCOS
OT J213806.6+26195778.1050.216 29275369 per centCOS
V844 Her78.69290 ± 303, 60.114 85062261 per centSTIS
SDSS J013701.06−091234.879.71300 ± 807, 80.114 54759477 per centCOS
SDSS J123813.73−033932.980.5211090.518 35892275 per centCOS
PU CMa81.6310COS
V1108 Her81.87130 ± 3011, 121.013 64350381 per centCOS
ASAS J002511+1217.282.00130 ± 3012, 130.112 83041677 per centCOS
SDSS J103533.02+055158.482.22170 ± 120.835 ± 0.00914, 150.0111 62044a85 per centCOS
CC Scl84.10160.216 855:80135 per centCOS
SDSS J075507.70+143547.684.76170.515 86271690 per centCOS
1RXS J105010.8−14043188.56100 ± 5018, 190.111 62227789 per centCOS
MR UMa91.17200.215 182↓65469 per centCOS
QZ Lib92.36120 ± 50190.0111 30323864 per centCOS
SDSS J153817.35+512338.093.11170.0133 855178594 per centCOS
UV Per93.44210.214 38957875 per centSTIS
1RXS J023238.8−37181295.04160220.213 52749178 per centCOS
SDSS J093249.57+472523.095.4817COS
RZ Sge98.32200.515 28766356 per centSTIS
CY UMa100.18230.115 23265861 per centSTIS
BB Ari101.2024, 250.214 948↓63283 per centCOS
DT Oct104.5424, 25COS
IY UMa106.43190 ± 600.79 ± 0.0426, 271.017 750↓1000a77 per centCOS
SDSS J100515.38+191107.9107.60170.215 94472374 per centCOS
RZ Leo110.17340 ± 11028, 290.515 01463883 per centCOS
CU Vel113.04150 ± 5029, 300.115 33666889 per centCOS
AX For113.04|$370^{+20}_{-60}$|25, 311.016 571↓77768 per centCOS
SDSS J164248.52+134751.4113.60321.017 710:87148 per centCOS
QZ Ser119.75|$460^{+150}_{-110}$|330.214 48158768 per centSTIS
DV UMa123.62504 ± 301.098 ± 0.02415, 341.018 874182a92 per centSTIS
IR Com125.3430022, 351.016 61878186 per centCOS
SDSS J001153.08−064739.2144.40360.113 85452563 per centCOS
OR And195.7025COS
BB Dor221.901500 ± 50037COS
SDSS J040714.78−064425.1245.04381.020 885110467 per centCOS
CW Mon254.3029725, 39COS
V405 Peg255.81|$149^{+26}_{-20}$|40COS
HS 2214+2845258.02410.526 443↓143684 per centCOS
BD Pav258.1950042, 430.517 77587692 per centSTIS
SDSS J100658.41+233724.4267.71676 ± 400.78 ± 0.12441.016 0001000a96 per centCOS
HM Leo268.9935045COS
HS 0218+3229428.021000460.217 99089370 per centCOS
HS 1055+0939541.8825COS

Notes. For each object, its orbital period, distance and white dwarf mass are compiled from the literature. The last columns report the results from this work: metallicity, effective temperatures, the systematic uncertainties arising from the unknown white dwarf mass, the percentage of the white dwarf contribution to the total flux and the instrument used. The white dwarf contribution has been calculated assuming a constant flux as second component. For the four systems with superscript ‘a’, a precise mass measurement is available. While the uncertainties on the effective temperature of IY UMa and SDSS1006 are dominated by the presence of the curtain of veiling gas (Section 4.4), the uncertainties reported for SDSS1035 and DV UMa are those related the unknown nature of the second additional component (Section 3.1). In particular, for DV UMa, we report the effective temperature obtained assuming log g = 8.78 (Section 4.3.2). The values flanked by a downwards arrow represent upper limits for the temperature of the systems. The values flanked by a colon represent unreliable effective temperature and are not considered in the discussion.

References – 1: Augusteijn et al. (1996); 2: Thorstensen (2003); 3: Thorstensen et al. (2002a); 4: Szkody et al. (2007); 5: Chochol et al. (2012); 6: Oizumi et al. (2007); 7: Pretorius et al. (2004); 8: Imada et al. (2007); 9: Aviles et al. (2010); 10: Thorstensen & Fenton (2003); 11: Price et al. (2004); 12: Ishioka, Sekiguchi & Maehara (2007); 13: Templeton et al. (2006); 14: Littlefair et al. (2006); 15: Savoury et al. (2011) 16: Chen et al. (2001); 17: Gänsicke et al. (2009); 18: Mennickent et al. (2001); 19: Patterson, Thorstensen & Kemp (2005a); 20: Patterson et al. (2005b); 21: Thorstensen & Taylor (1997); 22: Patterson (2011); 23: Thorstensen et al. (1996); 24: Uemura et al. (2010); 25: Ritter & Kolb (2003); 26: Steeghs et al. (2003); 27: Patterson et al. (2000); 28: Mennickent & Tappert (2001); 29: Mennickent & Diaz (2002); 30: Mennickent & Diaz (1996); 31: Imada et al. (2006); 32: Southworth et al. (2008); 33: Thorstensen et al. (2002b); 34: Feline et al. (2004); 35: Feline et al. (2005); 36: Rebassa-Mansergas et al. (2014); 37: Rodríguez-Gil et al. (2012); 38: Ak et al. (2005); 39: Szkody & Mateo (1986); 40: Thorstensen et al. (2009); 41: Aungwerojwit et al. (2006); 42: Barwig & Schoembs (1983); 43: Sion et al. (2008); 44: Southworth et al. (2009); 45: Thorstensen & Taylor (2001); 46: Rodríguez-Gil et al. (2009).

Table 5.

Characteristics of the 45 CV white dwarfs observed with COS and STIS.

SystemPorbdMWDReferencesZTeff±WDInstrument
(min)(pc)(M)(Z)(K)(K)contribution
V485 Cen59.0310.515 20065556 per centSTIS
GW Lib76.78|$140^{+30}_{-20}$|2, 30.216 995↓81285 per centCOS
SDSS J143544.02+233638.778.0040.0111 94031584 per centCOS
OT J213806.6+26195778.1050.216 29275369 per centCOS
V844 Her78.69290 ± 303, 60.114 85062261 per centSTIS
SDSS J013701.06−091234.879.71300 ± 807, 80.114 54759477 per centCOS
SDSS J123813.73−033932.980.5211090.518 35892275 per centCOS
PU CMa81.6310COS
V1108 Her81.87130 ± 3011, 121.013 64350381 per centCOS
ASAS J002511+1217.282.00130 ± 3012, 130.112 83041677 per centCOS
SDSS J103533.02+055158.482.22170 ± 120.835 ± 0.00914, 150.0111 62044a85 per centCOS
CC Scl84.10160.216 855:80135 per centCOS
SDSS J075507.70+143547.684.76170.515 86271690 per centCOS
1RXS J105010.8−14043188.56100 ± 5018, 190.111 62227789 per centCOS
MR UMa91.17200.215 182↓65469 per centCOS
QZ Lib92.36120 ± 50190.0111 30323864 per centCOS
SDSS J153817.35+512338.093.11170.0133 855178594 per centCOS
UV Per93.44210.214 38957875 per centSTIS
1RXS J023238.8−37181295.04160220.213 52749178 per centCOS
SDSS J093249.57+472523.095.4817COS
RZ Sge98.32200.515 28766356 per centSTIS
CY UMa100.18230.115 23265861 per centSTIS
BB Ari101.2024, 250.214 948↓63283 per centCOS
DT Oct104.5424, 25COS
IY UMa106.43190 ± 600.79 ± 0.0426, 271.017 750↓1000a77 per centCOS
SDSS J100515.38+191107.9107.60170.215 94472374 per centCOS
RZ Leo110.17340 ± 11028, 290.515 01463883 per centCOS
CU Vel113.04150 ± 5029, 300.115 33666889 per centCOS
AX For113.04|$370^{+20}_{-60}$|25, 311.016 571↓77768 per centCOS
SDSS J164248.52+134751.4113.60321.017 710:87148 per centCOS
QZ Ser119.75|$460^{+150}_{-110}$|330.214 48158768 per centSTIS
DV UMa123.62504 ± 301.098 ± 0.02415, 341.018 874182a92 per centSTIS
IR Com125.3430022, 351.016 61878186 per centCOS
SDSS J001153.08−064739.2144.40360.113 85452563 per centCOS
OR And195.7025COS
BB Dor221.901500 ± 50037COS
SDSS J040714.78−064425.1245.04381.020 885110467 per centCOS
CW Mon254.3029725, 39COS
V405 Peg255.81|$149^{+26}_{-20}$|40COS
HS 2214+2845258.02410.526 443↓143684 per centCOS
BD Pav258.1950042, 430.517 77587692 per centSTIS
SDSS J100658.41+233724.4267.71676 ± 400.78 ± 0.12441.016 0001000a96 per centCOS
HM Leo268.9935045COS
HS 0218+3229428.021000460.217 99089370 per centCOS
HS 1055+0939541.8825COS
SystemPorbdMWDReferencesZTeff±WDInstrument
(min)(pc)(M)(Z)(K)(K)contribution
V485 Cen59.0310.515 20065556 per centSTIS
GW Lib76.78|$140^{+30}_{-20}$|2, 30.216 995↓81285 per centCOS
SDSS J143544.02+233638.778.0040.0111 94031584 per centCOS
OT J213806.6+26195778.1050.216 29275369 per centCOS
V844 Her78.69290 ± 303, 60.114 85062261 per centSTIS
SDSS J013701.06−091234.879.71300 ± 807, 80.114 54759477 per centCOS
SDSS J123813.73−033932.980.5211090.518 35892275 per centCOS
PU CMa81.6310COS
V1108 Her81.87130 ± 3011, 121.013 64350381 per centCOS
ASAS J002511+1217.282.00130 ± 3012, 130.112 83041677 per centCOS
SDSS J103533.02+055158.482.22170 ± 120.835 ± 0.00914, 150.0111 62044a85 per centCOS
CC Scl84.10160.216 855:80135 per centCOS
SDSS J075507.70+143547.684.76170.515 86271690 per centCOS
1RXS J105010.8−14043188.56100 ± 5018, 190.111 62227789 per centCOS
MR UMa91.17200.215 182↓65469 per centCOS
QZ Lib92.36120 ± 50190.0111 30323864 per centCOS
SDSS J153817.35+512338.093.11170.0133 855178594 per centCOS
UV Per93.44210.214 38957875 per centSTIS
1RXS J023238.8−37181295.04160220.213 52749178 per centCOS
SDSS J093249.57+472523.095.4817COS
RZ Sge98.32200.515 28766356 per centSTIS
CY UMa100.18230.115 23265861 per centSTIS
BB Ari101.2024, 250.214 948↓63283 per centCOS
DT Oct104.5424, 25COS
IY UMa106.43190 ± 600.79 ± 0.0426, 271.017 750↓1000a77 per centCOS
SDSS J100515.38+191107.9107.60170.215 94472374 per centCOS
RZ Leo110.17340 ± 11028, 290.515 01463883 per centCOS
CU Vel113.04150 ± 5029, 300.115 33666889 per centCOS
AX For113.04|$370^{+20}_{-60}$|25, 311.016 571↓77768 per centCOS
SDSS J164248.52+134751.4113.60321.017 710:87148 per centCOS
QZ Ser119.75|$460^{+150}_{-110}$|330.214 48158768 per centSTIS
DV UMa123.62504 ± 301.098 ± 0.02415, 341.018 874182a92 per centSTIS
IR Com125.3430022, 351.016 61878186 per centCOS
SDSS J001153.08−064739.2144.40360.113 85452563 per centCOS
OR And195.7025COS
BB Dor221.901500 ± 50037COS
SDSS J040714.78−064425.1245.04381.020 885110467 per centCOS
CW Mon254.3029725, 39COS
V405 Peg255.81|$149^{+26}_{-20}$|40COS
HS 2214+2845258.02410.526 443↓143684 per centCOS
BD Pav258.1950042, 430.517 77587692 per centSTIS
SDSS J100658.41+233724.4267.71676 ± 400.78 ± 0.12441.016 0001000a96 per centCOS
HM Leo268.9935045COS
HS 0218+3229428.021000460.217 99089370 per centCOS
HS 1055+0939541.8825COS

Notes. For each object, its orbital period, distance and white dwarf mass are compiled from the literature. The last columns report the results from this work: metallicity, effective temperatures, the systematic uncertainties arising from the unknown white dwarf mass, the percentage of the white dwarf contribution to the total flux and the instrument used. The white dwarf contribution has been calculated assuming a constant flux as second component. For the four systems with superscript ‘a’, a precise mass measurement is available. While the uncertainties on the effective temperature of IY UMa and SDSS1006 are dominated by the presence of the curtain of veiling gas (Section 4.4), the uncertainties reported for SDSS1035 and DV UMa are those related the unknown nature of the second additional component (Section 3.1). In particular, for DV UMa, we report the effective temperature obtained assuming log g = 8.78 (Section 4.3.2). The values flanked by a downwards arrow represent upper limits for the temperature of the systems. The values flanked by a colon represent unreliable effective temperature and are not considered in the discussion.

References – 1: Augusteijn et al. (1996); 2: Thorstensen (2003); 3: Thorstensen et al. (2002a); 4: Szkody et al. (2007); 5: Chochol et al. (2012); 6: Oizumi et al. (2007); 7: Pretorius et al. (2004); 8: Imada et al. (2007); 9: Aviles et al. (2010); 10: Thorstensen & Fenton (2003); 11: Price et al. (2004); 12: Ishioka, Sekiguchi & Maehara (2007); 13: Templeton et al. (2006); 14: Littlefair et al. (2006); 15: Savoury et al. (2011) 16: Chen et al. (2001); 17: Gänsicke et al. (2009); 18: Mennickent et al. (2001); 19: Patterson, Thorstensen & Kemp (2005a); 20: Patterson et al. (2005b); 21: Thorstensen & Taylor (1997); 22: Patterson (2011); 23: Thorstensen et al. (1996); 24: Uemura et al. (2010); 25: Ritter & Kolb (2003); 26: Steeghs et al. (2003); 27: Patterson et al. (2000); 28: Mennickent & Tappert (2001); 29: Mennickent & Diaz (2002); 30: Mennickent & Diaz (1996); 31: Imada et al. (2006); 32: Southworth et al. (2008); 33: Thorstensen et al. (2002b); 34: Feline et al. (2004); 35: Feline et al. (2005); 36: Rebassa-Mansergas et al. (2014); 37: Rodríguez-Gil et al. (2012); 38: Ak et al. (2005); 39: Szkody & Mateo (1986); 40: Thorstensen et al. (2009); 41: Aungwerojwit et al. (2006); 42: Barwig & Schoembs (1983); 43: Sion et al. (2008); 44: Southworth et al. (2009); 45: Thorstensen & Taylor (2001); 46: Rodríguez-Gil et al. (2009).

4 DISCUSSION

4.1 log g correction of published Teff values

The two most commonly used techniques to measure effective temperatures of CV white dwarfs are spectroscopy, which is by fitting ultraviolet or optical spectra with white dwarf atmosphere models, and photometry, i.e. from the analysis of light curves to study the white dwarf ingress and egress in eclipsing systems. Townsley & Gänsicke (2009, hereafter TG09) present an analysis of CV white dwarf effective temperatures and selected only those systems for which a reliable Teff determination is available. They consider a measurement unreliable when obtained from (i) spectra in which the white dwarf could not be unambiguously detected or, (ii) in the case of eclipse light-curve analyses, oversimplified models or data of poor quality were used. Following these criteria, TG09 compiled 43 systems with a reliable temperature measurement (see their table 1).

Among the 43 measurements from TG09, 15 were obtained from light-curve analyses (which also delivers the white dwarf mass) or have white dwarf mass measurements independent from the spectral fit. For the remaining 28 objects, an independent mass determination was not available and the white dwarf Teff was evaluated via spectroscopic analyses, following methods similar to the one described here, but assuming log g = 8.00. As discussed in Section 3, this assumption does not reflect the average mass in CV white dwarfs, M ≃ 0.8 M, corresponding to log g = 8.35. To combine our results with those of TG09, we need therefore to evaluate the corresponding Teff for log g = 8.35 for those 28 objects.

The systematic correction that we need to apply is ΔTeff = Teff (log  g = 8.35) − Teff (log  g = 8.00), which is the opposite of the quantity ΔTeff we calculated in Section 3.2. Using the relationship −ΔTeff = 1417 × log (Teff × 0.000 1046), we corrected the Teff values for those 28 systems from TG09 that did not have an independent mass measurement to the average CV white dwarf mass (i.e. log  g = 8.35), therefore enabling a consistent combinations of these values with the 36 temperatures that we derived for the COS+STIS data.

4.2 Notes on individual objects

4.2.1 Systems observed close to an outburst

As explained in Section 2, if a CV experienced an outburst shortly before the ultraviolet observation, its spectrum could be contaminated by disc emission. Furthermore, the white dwarf photosphere is heated by the increased infall of material and different subtypes of CVs have different cooling time-scales on which they return to their quiescent temperature (Sion 1995; Piro et al. 2005). A spectroscopic analysis of these systems can therefore provide only an upper limit on the white dwarf effective temperature.

For each system, we inspected the light curves retrieved from the AAVSO web site plus a total of additional ∼2000 images (collected with the Mount John University Observatory OC61 Telescope, the New Mexico State University Observatory TMO61 telescope and the Prompt telescopes located in Chile), covering two months before the HST/COS observations. We found that nine systems in which the white dwarf dominates the ultraviolet flux went into outburst within this time interval: AX For, BB Ari, HS 2214+2845, IY UMa, MR UMa, QZ Ser, V485 Cen (Fig. 11), CC Scl (Fig. 12, left) and SDSS J164248.52+134751.4 (SDSS1642, Fig. 12, right). QZ Ser and V485 Cen have STIS observations (Section 4.2.2) from which we determined the quiescent temperature while, for the remaining systems, the results that we report here only represent an upper limit for their quiescent Teff.

Light curves for seven targets in our sample that experienced an outburst within two months before the HST observations (indicated with the blue lines). The HST observation date has been subtracted from the Julian date. Note the different time range on the x-axis. The data have been retrieved from the AAVSO data base.
Figure 11.

Light curves for seven targets in our sample that experienced an outburst within two months before the HST observations (indicated with the blue lines). The HST observation date has been subtracted from the Julian date. Note the different time range on the x-axis. The data have been retrieved from the AAVSO data base.

Left: Prompt and OC61 light curve for CC Scl. Right: AAVSO light curve for SDSS J164248.52+134751.4. The blue line represents the date of the HST observations that has been subtracted from the Julian date.
Figure 12.

Left: Prompt and OC61 light curve for CC Scl. Right: AAVSO light curve for SDSS J164248.52+134751.4. The blue line represents the date of the HST observations that has been subtracted from the Julian date.

For CC Scl and SDSS1642, we found that the white dwarf contributes only ≃35 per cent (Fig. 13, top) and ≃50 per cent of the total flux (Fig. 13, bottom), respectively. Owing to this strong disc contamination, the derived effective temperatures do not fulfil the requirement of a reliable measurement as defined in TG09, and we do not include them in the following analysis. Furthermore CC Scl is an Intermediate Polar (IP) and its response to accretion and disc instabilities is more complicated than that of a non-magnetic CV. This system will be analysed in more detail by Szkody et al. (in preparation).

HST/COS spectra (black) of CC Scl (top) and SDSS J164248.52+134751.4 (bottom) along with the best-fitting model (red) assuming a blackbody second component. The white dwarf emission (blue) only contributes ≃35 per cent (CC Scl) and ≃50 per cent (SDSS1642) of the total flux. The geocoronal emission lines of Ly α (1216 Å) and O i (1302 Å) are plotted in grey.
Figure 13.

HST/COS spectra (black) of CC Scl (top) and SDSS J164248.52+134751.4 (bottom) along with the best-fitting model (red) assuming a blackbody second component. The white dwarf emission (blue) only contributes ≃35 per cent (CC Scl) and ≃50 per cent (SDSS1642) of the total flux. The geocoronal emission lines of Ly α (1216 Å) and O i (1302 Å) are plotted in grey.

4.2.2 Systems with COS and STIS observations

QZ Ser and V485 Cen have been observed both with COS and STIS (Table 6). Inspecting their spectra (middle and bottom panel of Fig. 14), the COS observations have a higher flux compared to the STIS observations, which is also reflected in their effective temperatures; the STIS data return a lower value (QZ Ser: Teff = 14 481 ± 587 K, V485 Cen: Teff = 15 200 ± 655 K) compared to the COS data (QZ Ser: Teff = 15 425 ± 676 K, V485 Cen: Teff = 16 208 ± 746 K). This difference is not related to difference in the calibration of the two instruments (see Section 3.4) and it is rather expected given that the magnitudes derived from the STIS acquisition images suggest that these systems were observed by STIS during the quiescent phase (see Section 2.2), whereas the COS spectra were obtained relatively shortly after an outburst (Fig. 11). Since the temperatures derived from the STIS spectra are representative of the quiescent properties of these systems, we use these values in the discussion below.

HST/COS spectra (black) in comparison with the HST/STIS spectra (red) of BD Pav, QZ Ser and V485 Cen. The geocoronal Ly α emission (1216 Å) is plotted in grey.
Figure 14.

HST/COS spectra (black) in comparison with the HST/STIS spectra (red) of BD Pav, QZ Ser and V485 Cen. The geocoronal Ly α emission (1216 Å) is plotted in grey.

Table 6.

Results for BD Pav, QZ Ser and V485 Cen derived from the COS and the STIS data.

ObjectInstrumentTeff (K)
BD PavSTIS17 775 ± 876
COS18 915 ± 964
QZ SerSTIS14 481 ± 587
COS15 425 ± 676
V485 CenSTIS15 200 ± 655
COS16 208 ± 746
ObjectInstrumentTeff (K)
BD PavSTIS17 775 ± 876
COS18 915 ± 964
QZ SerSTIS14 481 ± 587
COS15 425 ± 676
V485 CenSTIS15 200 ± 655
COS16 208 ± 746
Table 6.

Results for BD Pav, QZ Ser and V485 Cen derived from the COS and the STIS data.

ObjectInstrumentTeff (K)
BD PavSTIS17 775 ± 876
COS18 915 ± 964
QZ SerSTIS14 481 ± 587
COS15 425 ± 676
V485 CenSTIS15 200 ± 655
COS16 208 ± 746
ObjectInstrumentTeff (K)
BD PavSTIS17 775 ± 876
COS18 915 ± 964
QZ SerSTIS14 481 ± 587
COS15 425 ± 676
V485 CenSTIS15 200 ± 655
COS16 208 ± 746

COS and STIS observations are available for one additional system: BD Pav (top panel of Fig. 14). The difference observed among the two data sets (STIS: Teff = 17 775 ± 876 K, COS: Teff = 18 915 ± 964 K) could be explained by its eclipsing nature if the STIS snapshot observations were obtained (partly) during the eclipse phase, resulting in a lower observed flux. Unfortunately, a reliable ephemeris is not available for this object and we cannot verify this hypothesis. On the other hand, the two spectra are characterized by a different slope and the derived effective temperatures differ by ≃1 200 K, which could suggest that an outburst occurred before the COS observations. Since BD Pav is a U Gem type CV, its outburst frequency and cooling time are expected to be similar to those of U Gem itself, ∼ 120 and ∼ 60 d, respectively (Sion et al. 1998), i.e. BD Pav is expected to experience a few outbursts every year. In fact, AAVSO observations of BD Pav (available since 1987) show a rough average of one outburst per year, with up to two outbursts observed in years of intense monitoring. No outburst is clearly identifiable in the AAVSO light curve for the period 2012/2013 (Fig. 15) but, owing to the relatively sparse sampling, we cannot completely rule out this hypothesis and therefore we consider in the discussion below the lower effective temperature derived from the STIS data.

Left: light curves for BD Pav over the period 2012 June to 2013 July. Right: close up of the days before the HST observations (highlighted with the blue line), which has been subtracted from the Julian date. The system only shows ellipsoidal variations. The data have been retrieved from the AAVSO data base.
Figure 15.

Left: light curves for BD Pav over the period 2012 June to 2013 July. Right: close up of the days before the HST observations (highlighted with the blue line), which has been subtracted from the Julian date. The system only shows ellipsoidal variations. The data have been retrieved from the AAVSO data base.

4.3 Systems with previous Teff measurements

Among the 36 systems in our sample, four CVs have a previous Teff determination in the TG09 sample: SDSS J103533.02+055158.4 (SDSS1035), CU Vel, GW Lib and DV UMa, which can be used for comparison with our results. Among them, SDSS1035 and DV UMa have also a previous mass determination and we analyse them in Section 4.3.2.

4.3.1 Previous ultraviolet measurements

CU Vel: CU Vel is located in the Vela constellation at a distance of 150 ± 50 pc (Mennickent & Diaz 2002). Although Vela lies in the Galactic plane, given the low distance to the system, CU Vel is not likely severely affected by interstellar reddening. To verify this, we retrieved from the archive the IUE spectra of CU Vel, which cover the wavelength range ≃1150–3300 Å. Inspecting the data, we did not detect the main signature of interstellar dust absorption, i.e. the bump at ≃2175 Å. To estimate the colour excess, we dereddened the spectrum assuming E(B − V) in the range 0.01–0.5. We noticed that for E(B − V) ≳ 0.02, a positive bump started to be visible in the spectrum, suggesting that we were overestimating the extinction. The low resolution and low signal-to-noise ratio of the IUE data did not allow us to accurately measure the colour excess, and we assumed E(B − V) = 0.02 as an upper limit, well below the E(B − V) ≃0.1 threshold defined in Section 3.3, concluding that the results for CU Vel are not affected in an appreciable way by interstellar dust absorption.

From the same IUE spectrum, Gänsicke & Koester (1999) derived Teff = 18 500 ± 1500 K. This temperature is significantly higher than Teff = 15 336 ± 668 K derived here from the COS data. To rule out any possible calibration differences among the two instruments, we compared the IUE and COS spectra for the flux standard white dwarf WD 0308–565. The flux levels of the different data sets are in good agreement, with an average difference of ≃3 per cent, and therefore the difference in the effective temperatures are not related to instrument calibration issues. Inspecting the AAVSO light curve of CU Vel, we find that the system experienced an outburst 20 d before the IUE observations (Fig. 16), which explains the higher ultraviolet flux observed with IUE compared to that of our new HST/COS data (Fig. 17), and the higher temperature determined by Gänsicke & Koester (1999).

Light curve for CU Vel over the period 1995 January–April. The blue line represents the date of the IUE observations, which has been subtracted from the Julian date. The data have been retrieved from the AAVSO data base.
Figure 16.

Light curve for CU Vel over the period 1995 January–April. The blue line represents the date of the IUE observations, which has been subtracted from the Julian date. The data have been retrieved from the AAVSO data base.

HST/COS spectrum (black, Teff = 15 336 ± 668 K) in comparison with the IUE spectrum (red, Teff = 18 500 ± 1 500 K; Gänsicke & Koester 1999) of CU Vel. The geocoronal Ly α emission (1216 Å) is plotted in grey.
Figure 17.

HST/COS spectrum (black, Teff = 15 336 ± 668 K) in comparison with the IUE spectrum (red, Teff = 18 500 ± 1 500 K; Gänsicke & Koester 1999) of CU Vel. The geocoronal Ly α emission (1216 Å) is plotted in grey.

GW Lib: GW Lib has been observed with HST before (2002 January; Szkody et al. 2002b) and after (2010 March and 2011 April; Szkody et al. 2012) its superoutburst in 2007 April. In these works, the authors assume log  g = 8.0 and 8.7, respectively, so we cannot directly compare our and their results.

Toloza et al. (2016) present a new analysis of all these HST observations. They refit the data assuming log  g = 8.35 and find |$T_\mathrm{eff} = 14\,695^{+13}_{-11}\,\mathrm{K}$| for the 2002 data set, Teff = 17 980 ± 14 K and Teff = 15 915 ± 9 K for the 2010 and 2011 observations, respectively.

GW Lib is a very peculiar system and a comparison between our (Teff = 16 995 ± 813 K) and these previous temperature measurements has to be considered with some caution. Indeed, GW Lib not only hosts a pulsating white dwarf but it also showed variations in Teff of ≃3000 K throughout the course of the HST observations (Toloza et al. 2016). Moreover, assuming log  g = 8.35, Szkody et al. (2016) derived Teff = 17 560 ± 9 K from 2015 HST/COS data, showing that the system has not cooled back to its quiescent temperature yet. Therefore, the Teff derived here is only an upper limit for the quiescent white dwarf temperature and therefore, in the following analysis, we assume as Teff for GW Lib the one derived for the 2002 data set by Toloza et al. (2016) for log  g = 8.35, Teff = 14 695 K. The mass of the white dwarf in GW Lib has been measured by Szkody et al. (2012, MWD = 0.79 ± 0.08 M) and van Spaandonk et al. (2010, MWD = 0.84 ± 0.02 M). However, these mass estimates depend on using velocity amplitude of the secondary star derived from the narrow Ca ii emission lines during outburst (assuming they originate on the irradiated face of the donor star), and do not fulfil the accuracy requirement to be included in the sample from Zorotovic et al. (2011), which represents the reference for our analysis. We therefore preferred a more conservative approach and assumed as uncertainty of the effective temperature, the one related to the unknown mass of the white dwarf, ± 812 K (Section 3.2).

4.3.2 Systems with a measured mass

As discussed in Section 3, it is not possible to break the degeneracy between Teff and log  g solely from the fit to the HST data and therefore we assumed log g = 8.35 (MWD = 0.8 M). Although several CVs in our sample have published mass estimates (e.g. BD Pav, SDSS J123813.73−033932.9), only four of them have a mass measurement that is accurate enough to be included in the study of Zorotovic et al. (2011, see their table 1): SDSS J103533.02+055158.4 (SDSS1035), IY UMa, DV UMa and SDSS J100658.41+233724.4 (SDSS1006). A previous Teff that can be considered reliable is only available for SDSS1035 and DV UMa, which we discuss in the following.

Littlefair et al. (2006) carried out a colour analysis of the SDSS1035 light curves during the white dwarf eclipse. From the observed shape of the white dwarf and bright spot eclipses, they measured a white dwarf mass of MWD = 0.835 ± 0.009 M and an effective temperature of Teff = 10 100 ± 200 K. The effective temperature we derived here, Teff = 11 620 ± 44 K, is ≃1500 K higher than the temperature measured by Littlefair et al. (2006). Since our assumption of log g = 8.35 is consistent with the measured white dwarf mass, we can conclude that this difference is related to the different methods used (light-curves analysis versus spectroscopic analysis).

While the masses of SDSS1035 correspond, within the errors, to log  g = 8.35, the mass of DV UMa is substantially higher: MWD = 1.098 ± 0.024 M (Savoury et al. 2011), which corresponds to log  g = 8.78. To take into account the independently measured surface gravity, we repeated the fit assuming log  g = 8.78, which returned Teff(log  g = 8.78) = 18 874 ± 182 K. As expected, this value is higher than the temperature we obtained for log g = 8.35, i.e. Teff(log g = 8.35) = 18 176 ± 108 K, and demonstrates that, if the masses were known, we could measure effective temperatures with an accuracy of ≃200 K, appreciably more accurate than the uncertainty estimate recommended here for all systems without measured masses.

Feline et al. (2004) and Savoury et al. (2011) measured the temperature of DV UMa from light-curve analyses and report Teff = 20 000 ± 1500 K and Teff = 15 500 ± 2400 K. Our result is in agreement with the temperature from Feline et al. (2004) while it is hotter than the measurement from Savoury et al. (2011). Comparing the DV UMa spectrum (Fig. 2, bottom) to the spectra of cooler systems (Fig. 2, top and middle panels), it is easily recognizable that the narrower Ly α profile and the absence of quasi-molecular bands require T ≳ 19 000 K. Thus, we are confident that our measurement is a realistic measure of the temperature of the white dwarf. DV UMa exemplifies how space-based ultraviolet spectroscopic measurements can give Teff to about 1 per cent accuracy compared to the ≃10–15 per cent accuracy achievable from ground-based optical light-curve analysis.

As a final caveat, we have to bear in mind that comparing effective temperatures measured at different epochs is always a delicate matter, since a genuine temperature change can occur owing to increase of the system mass-transfer rate above its quiescent value.

4.4 Eclipsing systems

In eclipsing CVs, the line of sight can pass through material extending above the disc, giving rise to strong absorption features. This has been observed for example in OY Car, where a forest of blended Fe ii absorption lines (the so-called iron curtain) veil the white dwarf emission (Horne et al. 1994). Our sample contains seven eclipsing systems: BD Pav, DV UMa, IR Com, IY UMa, SDSS J040714.78−064425.1 (SDSS0407), SDSS1006 and SDSS1035. While the observations of BD Pav, IR Com and SDSS1035 are not strongly affected by the veiling gas, in the spectra of the remaining systems the curtain signature is revealed by several absorption features (Fig. 18), which modify the overall slope of the spectrum and contaminate the core of the Ly α line, the main tracers for the white dwarf effective temperature.

HST/COS spectrum of SDSS J040714.78−064425.1. The arrows highlight the position of those lines that are contaminated by or arise from absorption within the veiling gas: C iii (1175 Å), N v (1242 Å), Si ii (1260 Å), Si iii (1298 Å), C ii (1335 Å), Si iv (1400 Å), C iv (1550 Å) and broad absorption bands from Fe ii (1568 Å and 1636 Å). The geocoronal emission lines of Ly α (1216 Å) and O i (1302 Å) are plotted in grey.
Figure 18.

HST/COS spectrum of SDSS J040714.78−064425.1. The arrows highlight the position of those lines that are contaminated by or arise from absorption within the veiling gas: C iii (1175 Å), N v (1242 Å), Si ii (1260 Å), Si iii (1298 Å), C ii (1335 Å), Si iv (1400 Å), C iv (1550 Å) and broad absorption bands from Fe ii (1568 Å and 1636 Å). The geocoronal emission lines of Ly α (1216 Å) and O i (1302 Å) are plotted in grey.

In order to estimate how our measurements and their uncertainties are affected by the presence of the veiling gas, we carried out an exploratory study of each eclipsing CV. Inspecting their spectra, we identify strong C iv (1550 Å) lines, suggesting the presence of hot gas along the line of sight, but also broad absorption bands from Fe ii (≃1568 Å and ≃1636 Å), which instead imply cold veiling gas. We therefore assumed that the white dwarf spectrum is attenuated by two homogeneous slabs, one cold (T ≃ 10 000 K) and one hot (T ≃ 80 000–100 000 K). We used synspec to generate models for the monochromatic opacity of the slabs which, combined with the column densities, returns the absorption due to the curtain.

The purpose of this study is not to determine the best-fitting model for the curtains (which will be done in a subsequent paper), but to determine the white dwarf effective temperature and realistic uncertainties. We varied the curtain parameters manually, exploring the space of four free parameters defining each slab (effective temperature Teff, electron density ne, turbulence velocity Vt and column density NH) and the white dwarf Teff and scaling factor. We started from the white dwarf effective temperature determined following the prescription from Section 3. Since the problem already contains a large number of free parameters, we used a constant as second additional component. We attenuated the white dwarf emission using the best matching model for the curtain we could identify and then changed the white dwarf temperature and scaling factor to better reproduce the observed spectrum. We repeated this procedure iteratively until we found the optimal set of parameters (Table 7), which define the final white dwarf Teff. This exercise allowed us to estimate that the systematic uncertainties introduced by the curtain are of the order of ≃1000 K for IY UMa, SDSS0407 and SDSS1006. Except for SDSS0407, this uncertainty is bigger than the systematic due to the unknown mass of the white dwarf and it is the value we use in the following analysis. In Fig. 19, we show the spectrum of SDSS1006 (black), which is dominated by several strong absorption bands. A white dwarf model alone (red, left) cannot adequately reproduce the observed flux level, which instead is well modelled including additional absorption from two slabs with different temperatures (red, right).

HST/COS spectrum (black) of SDSS J100658.41+233724.4 along with the best model (red) assuming a constant second component, with (right) and without (left) absorption from two slabs with different temperatures. The geocoronal emission lines of Ly α (1216 Å) and O i (1302 Å) are plotted in grey.
Figure 19.

HST/COS spectrum (black) of SDSS J100658.41+233724.4 along with the best model (red) assuming a constant second component, with (right) and without (left) absorption from two slabs with different temperatures. The geocoronal emission lines of Ly α (1216 Å) and O i (1302 Å) are plotted in grey.

Table 7.

Optimal set of parameters for the two homogeneous slabs, one cold and one hot, veiling the white dwarf spectrum in the eclipsing systems.

Cold slab parametersHot slab parameters
SystemTeff (K)log (ne · cm3)log (NH · cm2)Vt (km s−1)Teff (K)log (ne · cm3)log (NH · cm2)Vt (km s−1)
IY UMa10 00012.020.5200100 00018.720.3200
DV UMa10 00012.019.85080 00018.020.720
SDSS J040714.78−064425.110 00012.019.9250100 00018.719.9200
SDSS J100658.41+233724.410 00012.021.6200100 00018.021.8200
Cold slab parametersHot slab parameters
SystemTeff (K)log (ne · cm3)log (NH · cm2)Vt (km s−1)Teff (K)log (ne · cm3)log (NH · cm2)Vt (km s−1)
IY UMa10 00012.020.5200100 00018.720.3200
DV UMa10 00012.019.85080 00018.020.720
SDSS J040714.78−064425.110 00012.019.9250100 00018.719.9200
SDSS J100658.41+233724.410 00012.021.6200100 00018.021.8200
Table 7.

Optimal set of parameters for the two homogeneous slabs, one cold and one hot, veiling the white dwarf spectrum in the eclipsing systems.

Cold slab parametersHot slab parameters
SystemTeff (K)log (ne · cm3)log (NH · cm2)Vt (km s−1)Teff (K)log (ne · cm3)log (NH · cm2)Vt (km s−1)
IY UMa10 00012.020.5200100 00018.720.3200
DV UMa10 00012.019.85080 00018.020.720
SDSS J040714.78−064425.110 00012.019.9250100 00018.719.9200
SDSS J100658.41+233724.410 00012.021.6200100 00018.021.8200
Cold slab parametersHot slab parameters
SystemTeff (K)log (ne · cm3)log (NH · cm2)Vt (km s−1)Teff (K)log (ne · cm3)log (NH · cm2)Vt (km s−1)
IY UMa10 00012.020.5200100 00018.720.3200
DV UMa10 00012.019.85080 00018.020.720
SDSS J040714.78−064425.110 00012.019.9250100 00018.719.9200
SDSS J100658.41+233724.410 00012.021.6200100 00018.021.8200

Finally, in the case of DV UMa (Fig. 20), the main source of contamination comes from the iron bands in the red portion of the spectrum. Weaker absorption features are present at shorter wavelengths but they do not contaminate the Ly α region. For this reason, we found that the veiling gas has no effect on the white dwarf temperature and therefore our result from Section 4.3.2 remains unchanged.

HST/STIS spectrum (black) of DV UMa along with the best model (red) assuming a constant second component, with (right) and without (left) absorption from two slabs with different temperatures. The geocoronal emission line of Ly α (1216 Å) is plotted in grey.
Figure 20.

HST/STIS spectrum (black) of DV UMa along with the best model (red) assuming a constant second component, with (right) and without (left) absorption from two slabs with different temperatures. The geocoronal emission line of Ly α (1216 Å) is plotted in grey.

4.5 Testing models for the present-day CV population

In Fig. 21, we show our sample (circles, red for COS data and blue for STIS data) and the corrected effective temperatures for the non-magnetic systems from TG09 (green triangles). While TG09 also included magnetic CVs observed in low state, we only observed non-magnetic systems (except for CC Scl, which is an IP). We exclude the magnetic systems from the following discussion, as their evolution may differ from that of non-magnetic CVs due to (potential) suppression of MB (Webbink & Wickramasinghe 2002; Araujo-Betancor et al. 2005b; Ferrario, de Martino & Gänsicke 2015).

Top: effective temperature as function of the orbital period from this work (circles, red for COS data, blue for STIS data) and for the non-magnetic system from TG09 (green triangles). Systems for which only an upper limit has been determined are shown with a downward arrow. The systems for which a mass measurement is available (DV UMa, SDSS1035 and SDSS1006) are shown with a starred symbol. IY UMa, for which a mass measurement is available but only an upper limit on its effective temperature has been determined, is shown with an open star. The uncertainties associated with SDSS1035 and DV UMa are too small to be seen. Some temperatures in the TG09 sample do not have an associated error. In these cases, we estimated the corresponding uncertainty using our equation (2) as described in Section 4.1. The solid lines represent the evolutionary tracks for a system with a 0.8 M⊙ white dwarf accreting from a donor with an initial mass 0.65 M⊙, and an initial orbital period of 12 h. The red track has been generated with the classical recipe for CV evolution (GR only below the period gap) while the black track includes a ‘residual’ MB equal to the GR AML when the donor has no radiative core. The two tracks overlap above the period gap. The small bump at Porb ≃ 100 min is a computational artefact arising in the change of equation of state table describing the secondary internal structure. The grey band highlights the period gap while, on the right, a mapping to $\langle \dot{M} \rangle$ calculated through equation 1 from TG09 is shown for M = 0.8, 0.6 and 1.0 M⊙, respectively. Bottom: close-up of the systems below the period gap.
Figure 21.

Top: effective temperature as function of the orbital period from this work (circles, red for COS data, blue for STIS data) and for the non-magnetic system from TG09 (green triangles). Systems for which only an upper limit has been determined are shown with a downward arrow. The systems for which a mass measurement is available (DV UMa, SDSS1035 and SDSS1006) are shown with a starred symbol. IY UMa, for which a mass measurement is available but only an upper limit on its effective temperature has been determined, is shown with an open star. The uncertainties associated with SDSS1035 and DV UMa are too small to be seen. Some temperatures in the TG09 sample do not have an associated error. In these cases, we estimated the corresponding uncertainty using our equation (2) as described in Section 4.1. The solid lines represent the evolutionary tracks for a system with a 0.8 M white dwarf accreting from a donor with an initial mass 0.65 M, and an initial orbital period of 12 h. The red track has been generated with the classical recipe for CV evolution (GR only below the period gap) while the black track includes a ‘residual’ MB equal to the GR AML when the donor has no radiative core. The two tracks overlap above the period gap. The small bump at Porb ≃ 100 min is a computational artefact arising in the change of equation of state table describing the secondary internal structure. The grey band highlights the period gap while, on the right, a mapping to |$\langle \dot{M} \rangle$| calculated through equation 1 from TG09 is shown for M = 0.8, 0.6 and 1.0 M, respectively. Bottom: close-up of the systems below the period gap.

The uncertainties in the two samples are dominated by the unknown white dwarf mass. It is important to notice that these uncertainties are of the order of ≃300–1800 K (see Section 3.2); therefore, the overall shape of the distribution is unlikely to change once the white dwarf masses are accurately determined.

The white dwarf Teff is set by the compressional heating of the accreted material (Townsley & Bildsten 2004) and provides a measurement of the secular mean accretion rate |$\langle \dot{M} \rangle$| as defined by Townsley & Bildsten (2003). By comparing the distribution shown in Fig. 21 with results from population synthesis calculations (see e.g. the |$\dot{M}\text{--}P_\mathrm{orb}$| plane in fig. 2b from Goliasch & Nelson 2015), we can test the models for the present-day CV population. Our results qualitatively agree with theoretical predictions, with the evolution of long period systems driven by MB and typical mass-transfer rates of |$\dot{M} \sim 10^{-10}$| to ∼10−9 Myr−1. In contrast, systems below the period gap, driven only by GR,5 are characterized by a lower average |$\dot{M} \sim 5 \times 10^{-11}\,\mathrm{M}_{\odot } \mathrm{yr}^{-1}$|⁠.

However, there are some clear discrepancies between the standard model and our results, as illustrated by an evolutionary track6 (red line) for a system with a 0.8 M white dwarf accreting from a donor with initially M2 = 0.65 M and an initial orbital period of 12 h. Above the period gap, several systems with Teff ≃ 40 000–50 000 K are present in the range Porb ≃ 180–240 min. These objects are known as VY Scl systems and are usually characterized by high temperatures, which indicate very high accretion rates on to the white dwarf, with |$\langle \dot{M} \rangle$| about 10 times above the value predicted by the standard evolution theory (TG09; Howell, Nelson & Rappaport 2001). Goliasch & Nelson (2015) suggested that these objects could arise naturally from systems close to the regime of unstable mass transfer – where the mass of the donor star is similar to the white dwarf mass – but this hypothesis needs to be investigated in more detail.

The effective temperatures at Porb ≳ 3 h indicate that there is more diversity above the period gap than expected from the results of TG09. Considering only the green points (non-magnetic CV from TG09), the systems above the period gap present clearly higher temperatures than the systems below. In contrast, the new systems from this work (red and blue circles) are characterized by surprisingly low temperatures, and the difference between CVs above and below the gap is not as pronounced as before. The interpretation of these results is not straightforward since we are limited by the small number of available effective temperatures in this period range, which is mainly populated by the so-called nova-like systems. Nova-likes are non-magnetic CVs and are further subdivided into VY Scl systems, which have been detected at least once during a state of low accretion activity, and UX UMa systems, which have no recorded low states (Dhillon 1996). This dichotomy is naturally subject to observational biases. Since the white dwarfs in nova-like CVs are always/often hidden by the disc emission, it is difficult to measure their effective temperature and more observations are needed to increase the number of systems with an accurate Teff above the period gap. Additional constraints will be provided in the next few years by Gaia: from its accurate parallaxes, we will determine an upper limit on the white dwarf effective temperatures of all disc-dominated CVs for which ultraviolet spectroscopy is available, improving our understanding of CV evolution above the period gap.

At short orbital periods, we note the presence of an extreme outlier, SDSS J153817.35+512338.0, with an effective temperature of Teff = 33 855 ± 1 785 K. This is much hotter than expected given its short orbital period (Porb = 93.11 min), i.e. for CVs with Porb ≲ 2 h, Teff ≃ 15 000 K. This temperature is incompatible with mere accretion heating, but suggests that the system is either a young CV that just formed at this orbital period, that it had a recent period of sustained high-mass transfer, or that it recently experienced a nova explosion and the white dwarf has not cooled down yet. We are obtaining follow-up observation for a detailed study of this system and the results will be presented in a future paper.

The bottom panel of Fig. 21 shows a close-up of the systems below the period gap. We note two unexpected features: (i) there is a large scatter near Porb ≃ 80 min, in contrast to theoretical predictions that suggest a well-defined Teff at the period minimum and (ii) the effective temperatures show a steeper decrease towards short periods, and a mean accretion rate about twice above that expected from pure GR AML. For comparison, we overplot a second evolutionary track (black) computed including a ‘residual’ MB equal to the GR AML when the donor has no radiative core. The new track agrees better with the observed Teff decrease and the observed orbital period minimum than the standard recipe for CV evolution. Although the new track does not accurately reproduce the observed slope towards the period minimum, its better match to the measured effective temperatures strongly supports the ideas of additional AML mechanisms than GR below the period gap, which have been suggested as ‘residual magnetic braking’ by Patterson (1998) and Knigge et al. (2011) and, more recently, as consequential angular momentum loss (CAML) by Schreiber, Zorotovic & Wijnen (2016) and Nelemans et al. (2016).

Finally, reaching the minimum period, CVs are expected to evolve back towards longer periods with mean accretion rates of |$\dot{M} \lesssim 2 \times 10^{-11}\,\mathrm{M}_{\odot }\,\mathrm{yr}^{-1}$|⁠, corresponding to Teff ≲ 11 500 K. These systems are the so-called ‘period bouncers’ and the standard model of CV evolution predicts that about 70 per cent of the present-day CVs should be found in this phase. However, we find only two period bouncer candidates in our sample: 1RXS J105010.8−140431 (Porb = 88.56 min, Teff = 11 622 ± 277 K) and QZ Lib (Porb = 92.36 min, Teff = 11 303 ± 238 K) that are characterized by effective temperatures ≃3000–4000 K lower than those of the other systems at similar orbital periods, and both have also been identified as possible period bouncers by Patterson (2011). However, these two systems have still higher temperatures than predicted by the theory and do not fall on to either of the lower two branches of the evolutionary tracks in Fig. 21. This could suggest the presence of enhanced AML in the post-bounce regime. This would consequently imply faster evolution than predicted by the standard theory, which could be a possible explanation for the dearth of this component of the CV population in the observed samples.

The lack of unambiguous period bouncers in our sample cannot be explained by selection biases: we selected our targets among CVs that experience rare outbursts and for which the white dwarf is visible in their optical spectra. However, given their extremely low mass-transfer rate, period bouncers are expected to be intrinsically faint. In fact, assuming the average distance of the CVs in our sample 〈d〉 ≃ 320 pc, the expected apparent V-band magnitude for a period bouncer with Teff ≃ 9000 K and log g = 8.35 would be V ≃ 20.5 mag (calculated using synthetic colours and evolutionary sequences of hydrogen atmosphere white dwarfs;7 Holberg & Bergeron 2006; Kowalski & Saumon 2006; Bergeron et al. 2011; Tremblay, Bergeron & Gianninas 2011) and therefore it is possible that we are limited by the present observational technologies that are not sensitive enough to identify these elusive systems.

4.6 CVs as Type Ia supernova progenitors

The evolution and the final fate of CV white dwarfs are, as for all types of accreting white dwarfs, of key interest in the framework of Type Ia supernova (SNe Ia) progenitors. Although early work showed the average mass of CV white dwarfs to lie in the range 〈MWD〉 ≃ 0.8–1.2 M (Warner 1973; Ritter 1987), higher than that of isolated white dwarfs 〈MWD〉 ≃ 0.6 M (Koester et al. 1979; Liebert et al. 2005; Kepler et al. 2007), historically CVs have not been considered as a major component of the SNe Ia progenitor population. This is because most models for classical novae – i.e. the thermonuclear ignition of the accreted hydrogen – predict that not only most (if not all) of the accreted matter (Prialnik & Kovetz 1995) but also some of the underlying core (Epelstain et al. 2007) would be ejected during the eruption (as supported by the observed abundances of nova ejecta; Gehrz et al. 1998), preventing mass growth. Nevertheless, Zorotovic et al. (2011) showed that CV white dwarfs masses are genuinely higher than both those of their detached progenitors and those of single white dwarfs, suggesting that CV white dwarfs may grow in mass.

Wijnen, Zorotovic & Schreiber (2015) investigated the effect on CV evolution of white dwarf mass growth either during nova cycles or through thermal time-scale mass transfer during the pre-CV phase, finding that this cannot explain the discrepancy between the mean masses of isolated and CV white dwarfs. Recent alternative explanations are CAML and asymmetric mass ejection during nova explosions, which could lead to dynamically unstable mass transfer in CVs hosting low-mass white dwarfs, potentially merging these semidetached binaries into single objects (Nelemans et al. 2016; Schreiber et al. 2016). On the other hand, the recent work by Hillman et al. (2016) shows that quasi-steady helium burning after several nova cycles can lead a CV white dwarf to reach the Chandrasekhar limit. At present, neither of these hypotheses have definitive arguments to rule out the other one and the debate on whether mass growth can occur or not is still wide open. It is therefore fundamental to improve our understanding of the long-term evolution of CVs in order to investigate their potential role as SNe Ia progenitors.

Against this background, it appears urgent to resolve the major discrepancy between observations and theory highlighted by our results. Particularly, below the period gap, the additional AML mechanisms required in order to better reproduce the measured effective temperatures could play a crucial role in the SNe Ia debate and a detailed theoretical analysis is needed to understand their origin. Finally, an observational effort is needed in order to enlarge the sample of CV white dwarfs with an accurate mass determination, presently limited to 32 (Zorotovic et al. 2011). Next year, the ESA Gaia mission will provide accurate parallaxes in the second data release DR2 for all the targets in our sample. From the knowledge of the temperature and the distance, the white dwarf mass can then be estimated assuming a mass–radius relationship, thus doubling also the number of systems with an accurate mass determination.

5 CONCLUSIONS

From a large HST survey of 45 CVs, we find 36 systems in which the white dwarf dominates the ultraviolet flux, as revealed by broad Ly α absorption. We determine the white dwarf effective temperatures by fitting the HST data with atmosphere models.

Combining our results with the 43 CVs from TG09, we almost double the number of objects with an accurate temperature measurement. Comparing the TeffPorb distribution with the mean accretion rate |$\dot{M}$|Porb distribution from population models, we test the model for the present-day CV population. The systems above the period gap have, on average, mean accretion rates about one order of magnitude higher than those of the systems below the period gap. This is in accordance with the AML mechanisms that are thought to dominate the different phases of CV evolution (MB above and GR below the period gap).

However, besides this qualitative agreement between observations and theoretical predictions, some clear discrepancies are present.

  • VY Scl systems dominate the orbital period range Porb ≃ 180–240 min, with Teff ≃ 40 000–50 000 K. These temperatures correspond to a |$\langle \dot{M} \rangle$| about 10 times above the value predicted by the standard evolution theory.

  • The results at Porb ≳ 3 h present a much more variegated scenario than in the smaller sample analysed by TG09, with the new systems showing surprisingly low temperatures. To improve our understanding of CV evolution above the period gap, we need to increase the number of well-characterized systems in this period range.

  • At short orbital periods, the temperatures imply higher mass-transfer rates than predicted by pure GR. Moreover, near the period minimum the data show a large scatter that is not accounted for by the models.

  • The standard model of CV evolution predicts that period bouncers should make up for about 70 per cent of the present-day CV population. We identify only two period bouncer candidates in our sample and, since the lack of these systems cannot be explained by selection effects, we conclude that the present methods used to identify CVs are not sensitive enough to spot these faint systems.

We note that our results are dominated by a systematic uncertainty of ∼ 300–1800 K due to the unknown white dwarf mass. Once additional constraints on the masses – dynamical and/or distances – become available, the white dwarf effective temperatures will be known with an accuracy of about ≃200 K. While a significant improvement, the overall shape of the distribution will not drastically change and our conclusions will remain unchanged.

Finally, we identify an exceptional outlier (SDSS J153817.35+512338.0) below the period gap, whose extremely high temperature (Teff = 33 855 ± 1 785 K) for its short orbital period (Porb = 93.11 min) could be explained by a young CV just formed at this Porb.

We will continue with a detailed analysis of the individual systems in the sample, measuring rotation rates and abundances. This enlarged sample of well-characterized CV white dwarfs will provide robust observational constraints on the response of white dwarfs to the accretion of mass, angular momentum and energy.

Acknowledgments

This work is based on observations made with the NASA/ESA Hubble Space Telescope, obtained at the Space Telescope Science Institute, which is operated by the Association of Universities for Research in Astronomy, Inc., under NASA contract NAS 5–26555. These observations are associated with programme GO–9357, GO–9724, GO–12870 and GO–13807.

We gratefully acknowledge the variable star observations from the AAVSO International Database contributed by observers worldwide and used in this research. We are indebted to the global amateur community for their outstanding support, which made the HST survey possible.

We are also extremely grateful for the tireless efforts of the operations and COS teams at STScI, including Amber Armstrong, Elena Mason, Charles Proffitt, Nolan Walborn and Alan Welty, in implementing this challenging programme.

The research leading to these results has received funding from the European Research Council under the European Union's Seventh Framework Programme (FP/2007–2013)/ERC Grant Agreement no. 320964 (WDTracer).

DDM acknowledges support from ASI–INAF I/037/12/0. MRS thanks for support from Fondecyt (1141269). TRM acknowledges STFC ST/L000733. PG is pleased to thank William (Bill) Blair for his kind hospitality at the Rowland Department of Physics and Astronomy at the Johns Hopkins University, Baltimore, MD.

This research has made use of the APASS data base, located at the AAVSO web site. Funding for APASS has been provided by the Robert Martin Ayers Sciences Fund.

This research has made use of the NASA/IPAC Extragalactic Database (NED), which is operated by the Jet Propulsion Laboratory, California Institute of Technology, under contract with the National Aeronautics and Space Administration.

Visiting at the Johns Hopkins University, Henry A. Rowland Department of Physics, Astronomy, Baltimore, MD 21218, USA.

1

A temperature measurement is defined reliable when the white dwarf can be unambiguously detected either in the ultraviolet spectrum (from a broad Ly α absorption profile and, possibly, sharp absorption metal lines) or its ingress and egress can be seen in eclipse light curves.

2

Using a single metallicity is sufficient to account for the presence of the metal lines in the fit, which are relatively weak. Possible deviations of single element abundances from the overall scaling with respect to the solar values do not affect the results of the χ2 minimization routine. In fact, varying the abundances of individual elements has no effect on the measured Teff.

3

The constant is a special case of a power law and accounts for the easiest case with no slope, as it requires only one free parameter (a scaling factor), while power law and blackbody require two (respectively, a temperature and an exponent, plus a scaling factor). For this reason, we included the constant flux as an additional mode for the second component.

4

We found that the effective temperature derived for different metallicities were consistent within the uncertainties. To simplify our analysis, we do not distinguish between different Z in this discussion.

5

When the secondary star becomes fully convective (Porb ≃ 3 h), it loses its radiative core, and the magnetic stellar wind, which sustains MB, is thought to be greatly reduced. In fact, there is good observation evidence for a decrease in the efficiency of MB in CVs (Schreiber et al. 2010) as well as in single stars (Reiners & Basri 2008). At this point, in the standard model of CV evolution, the evolution of the system is thought to be driven only by GR. However, there are arguments for an AML that is larger than produced by pure GR below the period gap, suggesting the presence of a ‘residual’ MB at short periods (Patterson 1998; Knigge et al. 2011).

6

Evolutionary track computed using mesabinary revision 8845 and in lists provided by Paxton et al. (2015) for the CV case (their fig. 5).

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