Surface effect of rain on microwave backscatter from the ocean: Measurements and modeling

The effect of rain on the ocean surface alters the relationship between the surface wind vector and microwave backscatter, presenting an obstacle to wind retrieval via scatterometry. To address the effect of rain on surface backscatter, we develop a physically based ocean surface wave model modified...

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Bibliographic Details
Published in:Journal of Geophysical Research - Oceans 2006-08, Vol.111 (C8), p.C08019-n/a
Main Authors: Contreras, Robert F., Plant, William J.
Format: Article
Language:English
Subjects:
Atmospheric Processes
backscatter
Earth sciences
Earth, ocean, space
Exact sciences and technology
Marine
Oceanography
Physical
Precipitation
rain
Remote sensing and electromagnetic processes
scatterometry
Surface waves and tides
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Summary:The effect of rain on the ocean surface alters the relationship between the surface wind vector and microwave backscatter, presenting an obstacle to wind retrieval via scatterometry. To address the effect of rain on surface backscatter, we develop a physically based ocean surface wave model modified by rain. Microwave backscatter is then calculated using a multiscale scattering model. Comparisons to observations at Ku band are used to validate and tune our surface model. Simulations give insight into backscattering surface features: ring waves result primarily from the collapse of the splash‐created stalk, and the impulse responsible for the generation of ring waves has a radius roughly 5 times the drop's radius. Comparisons also show that backscatter from stationary splash features is necessary to accurately reproduce the effect of rain at Ku band. For Ku band our simulations expand upon prior measurements showing that rain increases backscatter and diminishes azimuthal variations. There is, however, a wind relative azimuthal signature in the backscatter for most rainfall rates. Simulations at Ka band, C band, and L band without the contribution from stationary splash features show that rain‐created ring waves often alter backscatter. The effects are greatest at Ka band where they mirror changes to the very high‐frequency region of the surface wave spectrum. C band backscatter is increased at moderate and high incidence angles and is sensitive to rain‐induced damping. The effect of rain on L band is to decrease backscatter at high rain rate, and it is also dependent on rain‐induced damping.
ISSN:0148-0227
2169-9275
2156-2202
2169-9291
DOI:10.1029/2005JC003356