1986
DOI: 10.1109/tgrs.1986.289622
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The Influence of Surface Oil on C-and Ku-Band Ocean Backscatter

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Cited by 44 publications
(32 citation statements)
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“…Figure 4 shows K r as function of the incidence angle for moderate (curve 1) and small (2) roughness of the small-scale spectrum. In our case, K r means the ratio between the backscatter cross sections for two surfaces which have a small roughness, as is indicated above, and a large-scale roughness with γ = 0.32 (curve 1) and 0.1 (2). It is seen that K r can reach values up to 20 dB depending on the slope value.…”
Section: Numerical Resultsmentioning
confidence: 80%
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“…Figure 4 shows K r as function of the incidence angle for moderate (curve 1) and small (2) roughness of the small-scale spectrum. In our case, K r means the ratio between the backscatter cross sections for two surfaces which have a small roughness, as is indicated above, and a large-scale roughness with γ = 0.32 (curve 1) and 0.1 (2). It is seen that K r can reach values up to 20 dB depending on the slope value.…”
Section: Numerical Resultsmentioning
confidence: 80%
“…However, most measurements of the radar backscatter from slicks have been interpreted in terms of the small perturbation theory (see, for example, [5]). As a result, the experimental observations not always agree with the theoretical conclusions [2].…”
Section: Introductionmentioning
confidence: 73%
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“…Scatterometer systems have been tested for the determination of liquid versus ice content in precipitating clouds, 10 ocean vector winds measurements for hurricane prediction, 11 dry snowpack measurements, 12 crop canopy yields, 13 and oil spill classification. 14 The first two applications are spaceborne and likely out of scope for airborne or unmanned aerial systems.…”
Section: Ku-band Earth Monitoring Assessmentmentioning
confidence: 99%