Fig. 2From: 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 modified solution with C20 and C30 replaced from TN14, along with SLR S, and GRACE CSR solution. The line represents the 3-month moving average. Note the scale difference for each regionBack to article page