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Titlebook: Meteorology of the Southern Hemisphere; David J. Karoly,Dayton G. Vincent Book 1998 American Meteorological Society 1998 Mesoscale Meteoro

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書(shū)目名稱Meteorology of the Southern Hemisphere
編輯David J. Karoly,Dayton G. Vincent
視頻videohttp://file.papertrans.cn/632/631815/631815.mp4
概述This eBook available on-line, for the first time, an AMS publication previously only in print.Presents an overview of detailed meteorology research work carried out in the Southern Hemisphere
叢書(shū)名稱Meteorological Monographs
圖書(shū)封面Titlebook: Meteorology of the Southern Hemisphere;  David J. Karoly,Dayton G. Vincent Book 1998 American Meteorological Society 1998 Mesoscale Meteoro
描述This book looks at the circulation features of the Southern Hemisphere, both for the atmosphere and oceans. It includes observational techniques based on satellites, anchored and drifting buoys, and the research carried out at research stations in the Southern Hemisphere. The book was originally published in 1972 by the American Meteorological Society. It has been revised and updated in 1999, following? the expansion of research bases and the development of research in the region at the time.
出版日期Book 1998
關(guān)鍵詞Mesoscale Meteorology; Meteorology of the Antarctic; Satellite Observational Techniques; Southern Hemis
版次1
doihttps://doi.org/10.1007/978-1-935704-10-2
isbn_ebook978-1-935704-10-2Series ISSN 0065-9401
issn_series 0065-9401
copyrightAmerican Meteorological Society 1998
The information of publication is updating

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Mesoscale Meteorology has been stimulated in large part by the practical benefits of such research, since mesoscale phenomena account for most of our significant “weather.” Nonetheless, it should be acknowledged that we still have a long way to go in understanding mesoscale weather systems.
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General Circulationeasons, and particularly in middle latitudes. More detailed discussions of the features in the Tropics and in high southern latitudes, and of the variability of the SH circulation, are given in chapters 3, 4, and 8, respectively.
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Indonesia, Papua New Guinea, and Tropical Australia: The Southern Hemisphere Monsoonritime continent (Ramage 1968). It is the location of one of the three global tropical heat sources and is the primary region of latent heat release associated with both the Southern Oscillation and the Madden-Julian oscillation (MJO; see chapter 8 for more details). Thus, it plays an important role in the dynamics of the global climate.
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Africa and Surrounding Waters or the oceans on either side. In addition, the weather along the subtropical belt has not been allocated for separate discussion; therefore, South African conditions, being intimately related with events farther north, are included in the discussion.
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