TO THE QUESTION OF USE OF TERRESTRIAL RADAR RADARS FOR MEASURING THE SPEED OF THE WIND OVER THE SEA SURFACE
DOI:
https://doi.org/10.30888/2415-7538.2020-16-01-003Keywords:
sea surface, radar, effective scattering area, geophysical model functionAbstract
The paper considers a model for extracting wind information from radar images using the effective scattering area (ESA). The considered aspects of using ESA allow us to state that ESA models combine microwave scattering with the wave energy conservation e
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References
P.W.Vachon and F.W.Dobson Validation of wind vector retrieval from ERS-1 SAR images over the Ocean. Global Atmos. Ocean Syst.,vol.5,pp.177-187,1996.
G.Engen, H.Johnson SAR-ocean wave inversion using image cross spectra.- IEEE Trans. Geoscience Remote Sensing.- 1995., July, vol.33, pp.1047-1056.
Monaldo at al. Comparison of SAR-derived win speed.- IEEE Trans. Geoscience Remote Sensing .2001, vol.39.,n 12, December
Kudryavtsev V., D. Hauser, G. Caudal, B.Chapron (2003a) A semiimpirical model of the normalized radar cross-section of the sea surface: 1. The background model, J. Geophys.Res., 108(C3),8054,doi:10.1029/2001JC001003
References.
P.W.Vachon and F.W.Dobson Validation of wind vector retrieval from ERS-1 SAR images over the Ocean. Global Atmos. Ocean Syst.,vol.5,pp.177-187,1996.
G.Engen, H.Johnson SAR-ocean wave inversion using image cross spectra.- IEEE Trans. Geoscience Remote Sensing.- 1995., July, vol.33, pp.1047-1056.
Monaldo at al. Comparison of SAR-derived win speed.- IEEE Trans. Geoscience Remote Sensing .2001, vol.39.,n 12, December
Kudryavtsev V., D. Hauser, G. Caudal, B.Chapron (2003a) A semiimpirical model of the normalized radar cross-section of the sea surface: 1. The background model, J. Geophys.Res., 108(C3),8054,doi:10.1029/2001JC001003
