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Progress in Earth and Planetary Science
Fig. 8 | Progress in Earth and Planetary Science

Fig. 8

From: Impact of the combination and replacement of SLR-based low-degree gravity field coefficients in GRACE solutions

Fig. 8

The ice sheet loss from time-variable gravity field signal up to degree and order 60 of the Greenland (top), West Antarctica (middle) and East Antarctica (bottom) recovered from GRACE/GRACE-FO COST-G (green), COST-G with TN14 (brown), COST-G with SLR (blue) and combination (orange). The delta sign indicates that the COST-G was subtracted from each solutions

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