Resolution of the Scripps/NOAA Marine Gravity Field from satellite altimetry

The July 1995 declassification of the entire Geosat GM satellite altimeter data set enabled a joint Scripps/NOAA effort to compute a new (version 7.2) marine gravity field on a 2‐minute grid. This gravity field covers the world' oceans between 72°N and 72°S, and is derived from a combination of ERS‐1 and Geosat GM and ERM data. An earlier NOAA Geosat‐only gravity field solution was confined to the southern latitudes because the 1992 declassification was limited to GM data south of 30°S. A simple coherence analysis between accurately‐navigated ship gravity profiles and comparable gravity profiles obtained from the gravity grids reveals that the Scripps/NOAA gravity field is coherent with ship gravity down to ∼≥ 23–30 km. This slight increase in resolution over the previous NOAA Geosat‐only gravity field (short‐wavelength resolution of ∼26–30 km) implies that the increased spatial coverage provided by the ERS‐I altimeter, when combined with Geosat, improves the solution. Coherence analyses between satellite gravity and ship topography, and ship gravity and ship topography, show that even shorter wavelength gravity anomalies (∼13 km) are present in sea‐surface measurements made by ship. Even so, the Scripps/NOAA marine gravity field does an excellent job of resolving most of the short‐wavelength gravity anomalies covering the world’ oceans.