Range estimates from a radar altimeter have biases which are a function of the significant wave height (SWH) and the satellite attitude angle. Based on results of pre-launch Geosat modeling and simulation by the Johns Hopkins Applied Physics Laboratory, a correction for SWH and attitude was already applied to the sea surface height estimates from Geosat's production data processing. By fitting a detailed model radar return waveform to Geosat waveform sampler data, we can provide an independent estimate of the height bias due to SWH and attitude angle. The waveform fitting also produces independent estimates of the SWH and of the attitude angle. The waveform fitting has been carried out for 10-s averages of Geosat waveform sampler data over a wide range of SWH and attitude values. Our results confirm that Geosat sea surface height correction is good to well within the original decimeter-level specification but that an additional height correction can be made at the several centimeter level. Our results are expressed as additive corrections to the NOAA-distributed Geosat estimates of sea surface height, SWH, and attitude, and we provide coefficients for the polynomial expressions for these corrections.
[1]
G. S. Hayne,et al.
Sea-state-related altitude errors in the Seasat radar altimeter
,
1982
.
[2]
Ernesto Rodriguez,et al.
Altimetry for non‐Gaussian oceans: Height biases and estimation of parameters
,
1988
.
[3]
D. Hancock,et al.
Waveform analysis for Geosat day 96
,
1987
.
[4]
Edward J. Walsh,et al.
Pulse Compression and Sea Level Tracking in Satellite Altimetry
,
1989
.
[5]
Ernesto Rodriguez,et al.
Extracting ocean surface information from altimeter returns - The deconvolution method
,
1989
.
[6]
Bruce C. Douglas,et al.
GEOSAT altimeter geophysical data record user handbook
,
1987
.
[7]
G. Brown.
The average impulse response of a rough surface and its applications
,
1977
.