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. 2017 Sep 13;92(3):299–319. doi: 10.1007/s00190-017-1063-5

Fig. 16.

Fig. 16

Differences of SMB-based and GRACE-based de-trended mass anomaly time-series for individual drainage systems and entire Greenland. GRACE-based time-series were computed with (red) and without (green) data weighting. a N, b NE, c NW, d SE, e SW, f GrIS