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Titlebook: Coupling Processes in the Lower and Middle Atmosphere; Eivind V. Thrane,Tom A. Blix,David C. Fritts Book 1993 Springer Science+Business Me

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31#
發(fā)表于 2025-3-27 00:06:34 | 只看該作者
Der Einfluss von Kultur auf die Wirtschaft,ence and turbulence as a wave damping process. We show that random occurence of turbulent patches may lead to . and spectral effects of this process are discussed. A few facts observed in the free troposphere and lower stratosphere by . experiments and pertinent to that dicussion are summarized.
32#
發(fā)表于 2025-3-27 04:24:40 | 只看該作者
33#
發(fā)表于 2025-3-27 08:45:15 | 只看該作者
34#
發(fā)表于 2025-3-27 13:32:10 | 只看該作者
35#
發(fā)表于 2025-3-27 15:09:56 | 只看該作者
Der Einfluss von Kultur auf die Wirtschaft,ards the extratropics in the stratosphere and downward cross-tropopause mass flux at middle to higher latitudes. The paper is focusing on the latter part of the exchange system. Calculations of downward fluxes derived from dynamical arguments (downward control principle) are compared with estimates
36#
發(fā)表于 2025-3-27 18:33:44 | 只看該作者
37#
發(fā)表于 2025-3-27 23:11:13 | 只看該作者
Operationalisierung von Wirtschaftskultur,scales. Planetary wave breaking exerts a strong influence on the dynamics, thermal structure, and distribution of trace chemical species in the winter stratosphere because it drives the mean meridional circulation and promotes quasi-horizontal mixing. In principle, the mechanism of wave breaking can
38#
發(fā)表于 2025-3-28 04:09:54 | 只看該作者
Der Einfluss von Kultur auf die Wirtschaft,ransport is reviewed. Previous GCM and idealized modeling work on the forcing mechanisms for extratropical planetary waves in the troposphere and middle atmosphere has given contradictory results. Some studies indicate that orographic forcing is dominant while others have indicated that the forcing
39#
發(fā)表于 2025-3-28 09:32:07 | 只看該作者
40#
發(fā)表于 2025-3-28 11:13:58 | 只看該作者
Der Einfluss von Kultur auf die Wirtschaft,and some of them are more particularly studied in this paper. Nevertheless several mechanisms can act simultaneously to generate tidal variations, some time rendering observations difficult to delineate.
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