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標(biāo)題: Titlebook: Climate Atlas of the Atlantic Ocean; Derived from the Com Ralf Lindau Book 2001 Springer-Verlag Berlin Heidelberg 2001 Atlantic Ocean.Cloud [打印本頁(yè)]

作者: 自由    時(shí)間: 2025-3-21 17:20
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作者: 欺騙世家    時(shí)間: 2025-3-21 20:43
Data and Data Treatmentcal study. Maps of monthly mean distribution are calculated not only for the basic ship observations as wind speed or air pressure but also for the indirectly derived climate variables such as evaporation or wind stress, which are obtained by parameterisations. For the derived variables the individu
作者: Flat-Feet    時(shí)間: 2025-3-22 02:17

作者: synovitis    時(shí)間: 2025-3-22 06:05
Evaluation eines Pilotprojektes,al parameters, cannot account for these contributions. For the North East Atlantic JOSEY & al. (1995) showed that the latent heat flux is overestimated by the crude climatological method. The negative correlation between wind speed and sea-air humidity difference causes an overestimation from 1–2 . in winter to 7 . in summer.
作者: 牲畜欄    時(shí)間: 2025-3-22 11:20
Data and Data Treatmental parameters, cannot account for these contributions. For the North East Atlantic JOSEY & al. (1995) showed that the latent heat flux is overestimated by the crude climatological method. The negative correlation between wind speed and sea-air humidity difference causes an overestimation from 1–2 . in winter to 7 . in summer.
作者: 商店街    時(shí)間: 2025-3-22 14:19

作者: 商店街    時(shí)間: 2025-3-22 19:24

作者: Overstate    時(shí)間: 2025-3-22 23:18

作者: 自作多情    時(shí)間: 2025-3-23 03:04
Book 2001mproving the calculations of air-sea fluxes, as performed by Isemer and Hasse, is no longer a complex and tricky venture, since flux parameterizations can be applied directly to the ship observations. Compared to the Bunker Altas we expanded the considered sea area and included also the South Atlant
作者: fringe    時(shí)間: 2025-3-23 07:35

作者: 改革運(yùn)動(dòng)    時(shí)間: 2025-3-23 09:44
Ressourcenorientierte Gruppenpsychotherapiee used as boundary conditions or sea truth for atmospheric and oceanic models and coupled models of the atmosphere-ocean system. The fast improvements that modeling has made in recent years also call for more detailed descriptions of processes at the air-sea interface, especially of the air-sea flux
作者: 四目在模仿    時(shí)間: 2025-3-23 17:17
Evaluation eines Pilotprojektes,cal study. Maps of monthly mean distribution are calculated not only for the basic ship observations as wind speed or air pressure but also for the indirectly derived climate variables such as evaporation or wind stress, which are obtained by parameterisations. For the derived variables the individu
作者: Control-Group    時(shí)間: 2025-3-23 19:10
Ralf LindauClear representation of extensive data.Internationally renown institute.Complete material in color on the enclosed CD-ROM
作者: 憲法沒(méi)有    時(shí)間: 2025-3-23 23:45

作者: ordain    時(shí)間: 2025-3-24 06:05

作者: Accolade    時(shí)間: 2025-3-24 09:29

作者: ELUDE    時(shí)間: 2025-3-24 13:27
Ressourcenorientierte NetzwerkmoderationAir-sea interaction is brought about by fluxes of momentum, heat and matter. Since these are not measured routineously, they are determined by parameterisations. In the following, we give a short account of the formulations that we selected.
作者: 污穢    時(shí)間: 2025-3-24 17:06
https://doi.org/10.1007/978-3-322-91476-7The net heat gain of the ocean is determined by summing the fluxes of shortwave (SR) and longwave radiation (LR) and the turbulent fluxes of sensible (H) and latent heat (LE) at the sea surface.
作者: 物種起源    時(shí)間: 2025-3-24 19:23

作者: arcane    時(shí)間: 2025-3-25 00:39

作者: cravat    時(shí)間: 2025-3-25 04:59

作者: Pessary    時(shí)間: 2025-3-25 08:37
Concluding RemarksThe climate data and air-sea fluxes presented in this work are based on the most comprehensive collection of marine meteorological observations and on the best available parameterisations for the open ocean.
作者: Stagger    時(shí)間: 2025-3-25 11:48
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作者: 遠(yuǎn)地點(diǎn)    時(shí)間: 2025-3-26 11:13
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作者: CHIP    時(shí)間: 2025-3-26 14:17
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作者: 玉米    時(shí)間: 2025-3-26 18:32
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作者: 枯燥    時(shí)間: 2025-3-26 21:19
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作者: 驚呼    時(shí)間: 2025-3-27 02:05
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作者: Adj異類(lèi)的    時(shí)間: 2025-3-27 07:22
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作者: ARBOR    時(shí)間: 2025-3-27 12:33
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作者: Libido    時(shí)間: 2025-3-27 17:33
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作者: sleep-spindles    時(shí)間: 2025-3-27 18:24
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