Expected differences between buoy and radar altimeter estimates of wind speed and significant wave height and their implications on buoy-altimeter comparisons

Author:

Monaldo Frank

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference23 articles.

1. Backscattering from a Gaussian distributed, perfectly conducting rough surface;Brown;IEEE Trans. Antennas Propag.,1978

2. The wind speed measurement capability of spaceborne radar altimeters;Brown;IEEE J. Oceanic Eng.,1981

3. A review of satellite altimeter measurement of sea surface wind speed: With a proposed new algorithm;Chelton;J. Geophys. Res.,1985

4. Further development of an improved altimeter wind speed algorithm;Chelton;J. Geophys. Res.,1986

5. Statistics of the sea surface derived from sun glitter;Cox;J. Mar. Res.,1954

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