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Titlebook: Surface Waves and Fluxes; Volume II — Remote S G. L. Geernaert,W. L. Plant Book 1990 Kluwer Academic Publishers 1990 Ocean.Wind speed.remot

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Lewis B. Wetzelted in this volume, is a field of interest to topologists working in knot theory, as well as to various categorists. It extends the complete spreads in topology due to R. H. Fox (1957) but, unlike the classical theory, it emphasizes an unexpected connection with topos distributions in the sense of F
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W. J. Pierson Jr.to topologists working in knot theory, as well as to various categorists. It extends the complete spreads in topology due to R. H. Fox (1957) but, unlike the classical theory, it emphasizes an unexpected connection with topos distributions in the sense of F. W. Lawvere (1983). The constructions, tho
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F. C. Jackson,D. R. Lyzengated in this volume, is a field of interest to topologists working in knot theory, as well as to various categorists. It extends the complete spreads in topology due to R. H. Fox (1957) but, unlike the classical theory, it emphasizes an unexpected connection with topos distributions in the sense of F
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Quasi-Specular Scattering from the Air-Sea Interface,1963; Bass and Fuch, 1978; Desanto and Brown, 1986). When the surface shape changes with both time and space, this further complicates matters. Even describing the scattering as a random process does not simplify the analysis too much and the use of numerical methods has not proven to be very useful
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Bragg Scattering of Electromagnetic Waves from the Air/Sea Interface, wartime need to detect enemy aircraft. When the newly-discovered tool was put to use to detect targets on or near the surface of the sea, these targets were often obscured by strong echos from the ocean itself. This “sea echo” constituted a considerable nuisance to those engaged in locating enemy v
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