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Titlebook: Climate Variability and Extremes during the Past 100 years; Stefan Br?nnimann,Jürg Luterbacher,Urs Neu Book 2008 Springer Science+Business

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31#
發(fā)表于 2025-3-26 21:07:01 | 只看該作者
978-94-007-8691-2Springer Science+Business Media B.V. 2008
32#
發(fā)表于 2025-3-27 02:24:58 | 只看該作者
Climate Variability and Extremes during the Past 100 years978-1-4020-6766-2Series ISSN 1574-0919 Series E-ISSN 2215-1621
33#
發(fā)表于 2025-3-27 07:16:20 | 只看該作者
34#
發(fā)表于 2025-3-27 12:09:15 | 只看該作者
Advances in Global Change Researchhttp://image.papertrans.cn/c/image/227655.jpg
35#
發(fā)表于 2025-3-27 17:09:32 | 只看該作者
P. Thomas Fletcher,Miaomiao Zhangd by natural influences to one significantly dominated by anthropogenic activities. This volume is a compilation of contributions to a workshop dealing with different aspects of climate change, variability, and extremes during the past 100 years. The individual contributions cover a broad range of t
36#
發(fā)表于 2025-3-27 17:51:01 | 只看該作者
https://doi.org/10.1007/978-3-319-22957-7gion was seen as the home of cyclones, which very often resulted in violent storms in northern latitudes and influenced the weather of middle latitudes. Between 1882 and 1945 Arctic climate features were observed starting from ground-based measurements of a temporary network of stations in the frame
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發(fā)表于 2025-3-27 22:05:44 | 只看該作者
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發(fā)表于 2025-3-28 03:10:31 | 只看該作者
39#
發(fā)表于 2025-3-28 09:44:33 | 只看該作者
The Structure of Riemannian Foliations,in other climate system components. Temperature in the free atmosphere is better studied than other parameters defining the upper-air climate, but nevertheless there exist numerous problems in the upper-air temperature trends. This paper gives the overview of the current status of radiosonde based e
40#
發(fā)表于 2025-3-28 13:01:02 | 只看該作者
Basic Properties of Riemannian Foliations,d rainfall. Climatological information, usually expressed as long-term averages and variability, is then presented over a geographical area or at a single location and time series of these quantities or of the observations themselves are examined for evidence of warming, more-frequent severe storms,
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