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Earth's surface mass transport derived from GRACE, evaluated by GPS, ICESat, hydrological modeling and altimetry satellite orbits

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Figure

Figure 1. Correlations between the G-NET station uplift and the ice-induced crustal deformations due to dynamic loading of the crustallayer obtained using the temporal gravity field solutions
Figure 4. Antarctic linear ice sheet mass change estimates peryear from different GRACE solutions (CSR RL05, GFZ RL05a andGFZ RBF) from January 2003 to December 2013
Figure 5. Mean annual ice mass change (Gt a−1) for the GreenlandIce Sheet and selected drainage basins (separated by red lines) andaggregations derived from different GRACE solutions and ICESatlaser altimetry data over the period from October 2003 to Octo-ber 2009.
Figure 7. Comparative correlations of catchment aggregated val-ues from GRACE results against hydrology; the plot depicts therelative difference (%) in each basin between the correlations oftwo time series with respect to the hydrological model (WGHM).Blue
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