“Time Variable Earth Gravity Field Models From the First Spaceborne Laser Ranging Interferometer"

The Gravity Recovery and Climate Experiment Follow‐On (GRACE‐FO), launched May 22, 2018 and collecting science data since June 2018, is extending the 15‐year data record of Earth mass change established by its predecessor GRACE mission (2002–2017). The GRACE‐FO satellites carry onboard a novel technology demonstration instrument for intersatellite ranging, the Laser Ranging Interferometer (LRI), in addition to the microwave interferometer (MWI) carried on GRACE. The LRI has out‐performed its in‐orbit performance requirements both in terms of accuracy as well as the duration of tracking. Here, we compare and validate LRI‐based gravity solutions for January 2019 to September 2020 against the MWI solutions. The comparison between the two sets of gravity solutions shows great similarities in general and nearly perfect consistency at a large hydrologic basin spatial scale (100,000 km(2) and above), commonly viewed as the spatial resolution established by GRACE. The comparison in the spectral domain shows differences at the higher degrees of the spectrum, with lower error in the zonal and near zonal terms for the LRI solutions. We conclude that the LRI observations can be used to recover time‐varying gravity signals to at least the level of accuracy established by the MWI‐based solutions. This is a promising finding, especially when considering the benefits of using the LRI over the MWI, such as the great stability of the instrument and the low occurrence of instrument reboot events.