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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Book 1999re averaged for spatial footprints representing scales greater than 25 km (or typically 30 minutes or longer for typical windspeeds). While more and more data became available over the years, and the technology applied was more reliable, robust, and durable, the flux coefficients and other turbulent

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The Marine Atmospheric Boundary Layer During Swell, According to Recent Studies in the Baltic Sea,0-ies (Volkov 1970, Makova 1975; Benilov et al. 1974). Similar results were reported from measurements over Lake Michigan by Davidson and Frank (1973) and from waters outside the Australian coast by Antonia and Chambers (1980) and by Chambers and Antonia (1981).

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Flux Measurements at the Noordwijk Platform,ents. This has succesfully been done so far by Donelan et al. (1997) and Fairall et al. , (1997). In this way we can get a good approximation to the vertical wind, but what we need is w, the . vertical wind and the next problem is to find a place on board a ship where the flow is not severely distur

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