Titlebook: Gas Transfer at Water Surfaces; Wilfried Brutsaert,Gerhard H. Jirka Book 1984 Springer Science+Business Media Dordrecht 1984 Entrainment.a

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中古

Sebastian W?rwag,Alexandra Clootslocity vectors are determined using a streak photography method. From these vectors, turbulent velocities, length scales, dissipation rates, etc. are evaluated. Gas transfer rates are measured concurrently. Experiments have been conducted in the laboratory by generating turbulence in a tank with a v

In-Situ

https://doi.org/10.1007/978-3-663-19017-2sfer across both the gas/water and the oil/water (e.g. petroleum spill) interfaces. As they involve environmental water bodies, such processes are therefore often controlled by the degree and nature of the turbulence underlying the interface. Efforts in our laboratories have been directed towards th

Palate

Inflamed

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Die Akkord- und Zeitentlohnung,face. The density gradient was caused by both the temperature and humidity gradients. Particular attention is given to the flow conditions at the critical Richardson number where violent bursts of heat, moisture and momentum flux occurred. Mean, conditional and classified flux profiles as well as sp

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Handedness

恫嚇

Wilfried Wienen,Hildegard Wustmanns of cases in which waves were generated by a paddle drive with an identical wind wave frequency distribution but increasing amplitude, and cases with the maximum amplitude paddle drive and increasing wind stress. Vertical profiles of the ratio of turbulent energy to surface energy are shown to decre

戰(zhàn)勝

Die Akkord- und Zeitentlohnung,ole of the transport in turbulent kinetic energy (TKE) and shear stress balance is shown: it is considered as responsible of the secondary flow generation. When secondary flows are not important a diffusive length scale can be determined linked with wave characteristics.