Expected differences between buoy and radar altimeter estimates of wind speed and significant wave height and their implications on buoy‐altimeter comparisons
- 15 March 1988
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Oceans
- Vol. 93 (C3), 2285-2302
- https://doi.org/10.1029/jc093ic03p02285
Abstract
No abstract availableKeywords
This publication has 10 references indexed in Scilit:
- Validation of Geosat altimeter‐derived wind speeds and significant wave heights using buoy dataJournal of Geophysical Research: Oceans, 1987
- A Field Evaluation of NDBC Moored Buoy WindsJournal of Atmospheric and Oceanic Technology, 1987
- Further development of an improved altimeter wind speed algorithmJournal of Geophysical Research: Oceans, 1986
- A review of satellite altimeter measurement of sea surface wind speed: With a proposed new algorithmJournal of Geophysical Research: Oceans, 1985
- The sampling variability of estimates of spectra of wind‐generated gravity wavesJournal of Geophysical Research: Oceans, 1983
- The measurement of the synoptic scale wind over the oceanJournal of Geophysical Research: Oceans, 1983
- The wind-speed measurement capability of spaceborne radar altimetersIEEE Journal of Oceanic Engineering, 1981
- Satellite altimeter measurements of sea state—An algorithm comparisonJournal of Geophysical Research, 1979
- Backscattering from a Gaussian-distributed perfectly conducting rough surfaceIEEE Transactions on Antennas and Propagation, 1978
- The Equilibrium Energy Spectrum of Randomly Forced Two-Dimensional TurbulenceJournal of the Atmospheric Sciences, 1973