B. Krichman

Localized Estimation of Tide Model Error and Mass Anomalies from GRACE/GRACE-FO Inter-Satellite Ranging

Despite improvements from the GOT5.6 ocean tide model adopted for RL07 processing, tide model error remains a significant source of temporal aliasing in GRACE gravimetry. This effect is felt particularly in shallow shelves with complex bathymetry and a larger than normal presence of nonlinear tides, as well as in regio...