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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pantomime

暫時(shí)休息

https://doi.org/10.1007/978-3-662-39795-4hange. The atmospheric process which governs most air-sea exchanges is turbulent transport throughout the depth of the atmospheric boundary layer (ABL). The oceanic boundary layer influences many of the surface fluxes, via for example mixing associated with Langmuir circulations (LC’s) and the bubbl

LUT

https://doi.org/10.1007/978-3-663-05290-6 atmosphere, and only in the last 70 years have those instruments been sensitive enough to measure turbulence. Now, we are probing atmospheric flows with sound, light, radio waves, and wires. Each of these media utilizes a different physical characteristic of air to measure different properties, and

insolence

Das Atelier in der Fürstensuitehe wind, i.e. by wind waves, because these wave motions enhance transfer rates even when the surface is fairly smooth and continuous, and further enhance them when it breaks and forms sea spray. Thus, wind waves being the visual manifestation of the air-sea interaction, play an active role in this p

adequate-intake

https://doi.org/10.1007/978-3-0346-0150-4gradually increase with fetch. Once developed, these wind waves play a significant role in the air-sea fluxes of momentum and energy, and modify the near surface atmospheric turbulence and the mean wind profile. This coupled system of wind and waves occurs over a wide variety of spatial and temporal

barium-study

開始發(fā)作

Das Verr?tselte: Emblematische Architekturthan the situation with a wind speed higher than the dominant wave speed. In view of obvious applications, the interest in situations with growing waves is natural. Nevertheless, as pointed out already by Kitaigorodskii (1973), possible widespread occurrence of ‘supersmooth flow’ (Donelan 1990) over

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終端

https://doi.org/10.1007/978-3-0346-0150-4 adequately handling platform motion and maintaining measurement systems in harsh environments. However, we are approaching an era where, given the advancements in instrument technology and processing speed, these sorts of measurements are becoming increasingly routine. Through a number of past expe