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Titlebook: Mesoscale Meteorology and Forecasting; Peter S. Ray Book 1986 American Meteorological Society 1986 Mesoscale Classifications.Mesoscale Con

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發(fā)表于 2025-3-30 08:57:58 | 只看該作者
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發(fā)表于 2025-3-30 16:14:27 | 只看該作者
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發(fā)表于 2025-3-30 18:43:46 | 只看該作者
Mesoscale Convective Complexes in the Middle Latitudesby Maddox (1980), Fritsch and Maddox (1981), Fritsch .. (1981), Bosart and Sanders (1981), Wetzel .. (1983), and Maddox (1983). It is termed Mesoscale Convective Complex (MCC). The satellite images in Fig. 17.1 show the infrared enhancement temperatures from two MCCs over central portions of the Uni
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發(fā)表于 2025-3-31 00:21:02 | 只看該作者
Tornadoes and Tornadogenesis“supercell”) have stimulated much research, both theoretical and applied. Over the past decade or so, several new developments have allowed for great advances in our understanding of the tornado. However, there is no single theory that explains all the commonly observed features. Our knowledge is fr
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發(fā)表于 2025-3-31 04:56:17 | 只看該作者
Upslope Precipitation Eventse climatologically prevailing westerlies; moisture-bearing easterly currents are driven up the slopes of the lee-side plains, toward the mountains, by synoptic circulations. “Upslope storms” have been so named under the presumption that advection over the generally rising terrain induces lifting, cl
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發(fā)表于 2025-3-31 09:01:08 | 只看該作者
https://doi.org/10.1007/978-1-935704-20-1Mesoscale Classifications; Mesoscale Convective Systems; Mesoscale Forecasting Techniques; Mesoscale Me
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發(fā)表于 2025-3-31 10:07:33 | 只看該作者
Peter S. RayHighly illustrated book with extensive bibliographic references.It is useful as a self-study guide or a textbook.The book is in conformance with the quality standards of the scientific community. It h
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發(fā)表于 2025-3-31 14:03:35 | 只看該作者
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發(fā)表于 2025-3-31 20:11:54 | 只看該作者
American Meteorological Society 1986
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發(fā)表于 2025-4-1 00:07:19 | 只看該作者
Fronts and Jet Streaks: A Theoretical Perspectivehis chapter is to explain from a theoretical perspective the existence of bands of concentrated gradients in temperature and momentum, and the reason distributions of temperature and momentum are not more uniform.
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