Fig. 1From: Impact of the combination and replacement of SLR-based low-degree gravity field coefficients in GRACE solutionsMass differences in Greenland and Antarctica due to various replacements of C20 and C30 values in the GRACE series. The COST-G GRACE solution was subtracted from each of the models shown. The line represents the 3-month moving average. Note the scale difference for each regionBack to article page