Time‐variable gravity observations of ice sheet mass balance: Precision and limitations of the GRACE satellite data

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Reducing leakage error in GRACE-observed long-term ice mass change: a case study in West Antarctica (2015, methodology): “The GRACE mission has launched a new era in studying the Earth’s gravity field and mass redistribution within the Earth system, and greatly improved understanding of large-scale mass redistribution in various components of the climate system, including the atmosphere, oceans, terrestrial water, and ”
GIA Model Statistics for GRACE Hydrology, Cryosphere, and Ocean Science (2018, methodology): “…(e.g., Save et al., 2012; Swenson & Wahr, 2006), the uncertainty level for inferring mass changes is ∼1 cm/yr water height equivalent over spatial scales of 300–450 km, though this estimate is highly dependent upon the target geometry and submonthly time dependence (e.g., Velicogna & Wahr, 2013).”
Continuity of the Mass Loss of the World's Glaciers and Ice Caps From the GRACE and GRACE Follow‐On Missions (2020, methodology): “Following Velicogna and Wahr (2013), we assume that the error is equal to the correction.”