Figure 1.
(a) Difference between mean gravity changes of 2010 March–2011 February and 2011 April–2012 March estimated from the post-processed CSR RL06 GRACE data with SH degree up to 60. (b) Surface mass changes in millimeter of equivalent water height (EWH) computed from (a). (c) FM result based on the distribution of (b). The ocean signals are barely seen because of the small intensity compared to the land mass change signals.

(a) Difference between mean gravity changes of 2010 March–2011 February and 2011 April–2012 March estimated from the post-processed CSR RL06 GRACE data with SH degree up to 60. (b) Surface mass changes in millimeter of equivalent water height (EWH) computed from (a). (c) FM result based on the distribution of (b). The ocean signals are barely seen because of the small intensity compared to the land mass change signals.

Close
This Feature Is Available To Subscribers Only

Sign In or Create an Account

Close

This PDF is available to Subscribers Only

View Article Abstract & Purchase Options

For full access to this pdf, sign in to an existing account, or purchase an annual subscription.

Close