Titlebook: Air-Sea Exchange: Physics, Chemistry and Dynamics; G. L. Geernaert Book 1999 Springer Science+Business Media Dordrecht 1999 Coast.Ocean.at

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https://doi.org/10.1007/978-3-0346-0150-4ss and different surface heat flux over the sea. The modelling problem is particularly difficult with offshore flow of warm air over a cool water surface (Section 4). The development of stratus and other cloud regimes in the coastal zone is beyond the scope of this survey. This chapter will assume f

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Das Verr?tselte: Emblematische Architekturature on gravity capillary waves and also offers infrared images of their microscale breaking.) These waves can be an additional significant source of direct C-band radar backscatter for grazing angles between 60° and 10° (Plant 1997) as well as at smaller grazing angles (Smith et al. 1996). They ca

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https://doi.org/10.1007/978-3-0346-0150-4ithms cannot be developed for poorly understood or heretofore unknown structures. To reduce these problems, we develop a multi-pronged statistical approach that makes synergistic use of Principal COmponents Analysis, Fourier Spectral Analysis, and Fractal Dimension Analysis. Once identified by this

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