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Abstract GRACE and GRACE‐FO gravimetry data are unique in its ability to observe global water mass variability and has frequently been applied for the determination of global mass rates to quantify the impacts of climate change and human activity on global freshwater availability and land ice evolution. However, its relatively coarse spatial resolution of ∼300‐500 km at monthly intervals precludes its direct use to measure mass changes in smaller drainage basins and individual glacier systems. We present a new global high‐resolution mascon product that improves spatial resolution and signal recovery by estimating trends directly from more than 16 years of Level 1B GRACE and GRACE‐FO data. We compare this product to independent gravimetry spherical harmonic trend estimates and to ice sheet mass rates derived from ICESat and ICESat‐2 laser altimetry. We demonstrate enhanced global signal recovery and improved agreement with ICESat/ICESat‐2 and discuss likely causes for the remaining discrepancies between the gravimetry and laser altimetry solutions.
Loomis et al. (Wed,) studied this question.