Physics
Scientific paper
Mar 2009
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009georl..3606601s&link_type=abstract
Geophysical Research Letters, Volume 36, Issue 6, CiteID L06601
Physics
1
Oceanography: Physical: Eddies And Mesoscale Processes, Oceanography: General: Remote Sensing And Electromagnetic Processes (0689, 2487, 3285, 4455, 6934), Oceanography: General: Instruments And Techniques, Geodesy And Gravity: Satellite Geodesy: Technical Issues (6994, 7969), General Or Miscellaneous: Techniques Applicable In Three Or More Fields
Scientific paper
We compare sea surface height anomalies observed by satellite altimeters in exact repeat mission orbits to anomalies observed by altimeters in geodetic or drifting orbits. One experiment compares data from the drift of TOPEX between its Tandem and Interleaved missions to repeat-orbit data from Jason-1, ERS-2 and GFO. A second experiment compares data from the ERS-1 non-repeating Geodetic Phases E and F to the repeating TOPEX data. Both studies cover the North Atlantic from 0° to 82°W and 15° to 55°N in order to sample both the Gulf Stream and quieter regions. Height anomalies are obtained along repeat and non-repeat orbits alike by use of a mean sea surface model. Each experiment is performed twice, once with the EGM2008 and once with the DNSC08 models, showing that the results are model-independent DNSC08 yields an insignificant 2 mm lower RMS misfit. To compare anomalies between repeat and non-repeat orbits with different spatio-temporal sampling we grid the 1-Hz along-track point data and interpolate the grid to point values. RMS differences between grids and point values are around 4 cm in quiet areas and 6 cm over the entire region, with negligible difference between misfits to repeat and non-repeat data. A mapped sea surface height anomaly grid built solely from ERS-1 geodetic data captures at least 85% of the variance in repeat-track TOPEX point data. From these results we can conclude that altimeters in suitable non-repeating orbits are as useful for mesoscale oceanographic studies as are repeat orbit missions.
Scharroo Remko
Smith Walter H. F.
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