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標(biāo)題: Titlebook: Air-Sea Exchange of Heat and Moisture During Storms; R. S. Bortkovskii,Edward C. Monahan Book 1987 Springer Science+Business Media B.V. 19 [打印本頁]

作者: Pessimistic    時間: 2025-3-21 18:28
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作者: jocular    時間: 2025-3-21 23:06
The Sea State, and Jacobs, 1977), on the gas exchange between the ocean and the atmosphere (Ariel’, 1979b; Monahan and Spillane, 1984), on the propagation of radio waves in the atmospheric surface layer, and on the radiothermal emission of the ocean surface (Martsinkevich and Melent’ev, 1975). A very important ap
作者: Essential    時間: 2025-3-22 03:37
Book 1987in particular, was it possible to proceed to a solution of this problem. This book presents the results of laboratory and field studies of the spray field in the air layer above the surface of a stormy sea. Since there is a dose correlation between the generation of spray and the breaking of wind wa
作者: Genetics    時間: 2025-3-22 06:14
Air-Sea Exchange of Heat and Moisture During Storms
作者: 含水層    時間: 2025-3-22 12:39

作者: 讓步    時間: 2025-3-22 13:13

作者: APRON    時間: 2025-3-22 18:35
1383-8601 he spray field in the air layer above the surface of a stormy sea. Since there is a dose correlation between the generation of spray and the breaking of wind wa978-90-481-8429-3978-94-017-0687-2Series ISSN 1383-8601 Series E-ISSN 2215-162X
作者: 鐵砧    時間: 2025-3-23 00:47
https://doi.org/10.1007/978-94-017-0687-2Storm; air; atmosphere; energy; marine; moisture; ocean; water; wind
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作者: 幼稚    時間: 2025-3-23 15:20
Sebastian Oberthür,Hermann E. Ottwhich are important for the transfer of energy and mass are closely related to the breaking of wind waves. These conclusions provided a basis for evaluating the intensity of the spray generation associated with the bursting of bubbles. There is an obvious need to study the quantitative characteristi
作者: sclera    時間: 2025-3-23 20:29
Sebastian Oberthür,Hermann E. Ott the intensity of spray generation. As the vertical spray flow .. increases, it begins to play a substantial role in the transfer of momentum, heat, and moisture in the lower marine atmospheric boundary layer.
作者: 摸索    時間: 2025-3-23 22:51

作者: invade    時間: 2025-3-24 05:55
https://doi.org/10.1007/978-3-642-91175-0acter of the energy and mass transfer during a storm. Of the various transfer mechanisms operating at the air-sea interface during a storm, we have considered in detail only one: the transfer of heat and mass by the spray, which under these conditions fills the air layer immediately above the water.
作者: parsimony    時間: 2025-3-24 09:10
Atmospheric and Oceanographic Sciences Libraryhttp://image.papertrans.cn/a/image/151862.jpg
作者: 肌肉    時間: 2025-3-24 11:26
Air-Sea Exchange of Heat and Moisture During Storms978-94-017-0687-2Series ISSN 1383-8601 Series E-ISSN 2215-162X
作者: lymphoma    時間: 2025-3-24 15:30
Sebastian Oberthür,Hermann E. Ott the intensity of spray generation. As the vertical spray flow .. increases, it begins to play a substantial role in the transfer of momentum, heat, and moisture in the lower marine atmospheric boundary layer.
作者: Estimable    時間: 2025-3-24 20:59
The Oceanic and Atmospheric Boundary Layers Under Windy Conditions,king of the steep crests of wind waves. However, from this essentially trivial conclusion we still have a long way to go before we understand how the droplets become separated from the water surface. This process, which is utilized in a number of engineering devices and which in applied science is c
作者: STYX    時間: 2025-3-25 00:43

作者: 馬籠頭    時間: 2025-3-25 06:34
The Transfer of Energy and Mass in the Spray-Filled Lower Marine Atmospheric Boundary Layer, the intensity of spray generation. As the vertical spray flow .. increases, it begins to play a substantial role in the transfer of momentum, heat, and moisture in the lower marine atmospheric boundary layer.
作者: BUCK    時間: 2025-3-25 07:40

作者: 健忘癥    時間: 2025-3-25 12:03
Conclusion,acter of the energy and mass transfer during a storm. Of the various transfer mechanisms operating at the air-sea interface during a storm, we have considered in detail only one: the transfer of heat and mass by the spray, which under these conditions fills the air layer immediately above the water.
作者: 割讓    時間: 2025-3-25 17:43

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作者: 轉(zhuǎn)折點    時間: 2025-3-26 11:12
The Role Played by Storms in Macroscale and Mesoscale Processes,ms from the mean, ‘nonstorm’ values of the sea-air temperature (Δ.) and humidity (Δ.) differences. The probability distribution of the modulus of the wind speed over the ocean has been studied repeatedly on the basis of various sets of observational data (Davidan .., 1978; Dubov, 1974; Rzheplinskii, 1972; Sorkina and Gnevko, 1968).
作者: 高度表    時間: 2025-3-26 15:02
Book 1987sfer and moisture transfer at the sea surface, all increase with an intensification of the wind, reaching high values during a storm. This belief is based on the results of gradient and eddy correlation measurements in the air layer over the water, as weIl as on data concerning the effect of storms
作者: Hdl348    時間: 2025-3-26 18:38
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