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Titlebook: Beyond El Ni?o; Decadal and Interdec Antonio Navarra Book 1999 Springer-Verlag Berlin Heidelberg 1999 Climate Variability.Climatology.Klima

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31#
發(fā)表于 2025-3-26 21:54:58 | 只看該作者
32#
發(fā)表于 2025-3-27 04:00:18 | 只看該作者
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發(fā)表于 2025-3-27 09:01:35 | 只看該作者
34#
發(fā)表于 2025-3-27 13:28:18 | 只看該作者
35#
發(fā)表于 2025-3-27 13:52:21 | 只看該作者
The Indian Summer Monsoon and its Variability,urce of fresh water for millions of people in India. The influence of the monsoon also extends to many regions remote from India. For example, the arrival of dry summer weather over Turkey and surrounding areas can be related to the development of the Asian Summer Monsoon (Rod-well and Hoskins 1996).
36#
發(fā)表于 2025-3-27 21:05:05 | 只看該作者
Dynamics of Interdecadal Variability in Coupled Ocean-Atmosphere Models,ually are. The forcing of interdecadal climate variability by volcanos is well established and therefore less controversial, and major volcanic eruptions can be easily seen in regional and globally averaged temperature records (e. g. Robock and Mao (1995)).
37#
發(fā)表于 2025-3-28 01:20:29 | 只看該作者
International Handbook of Universities 2019increased. One important question is thus the following: what is the minimum number of runs necessary to overcome the model internal variability and to study, with confidence, the model’s response to external forcing ? It is clear that the answer depends upon the signal to study and the method used to detect the signal.
38#
發(fā)表于 2025-3-28 06:05:52 | 只看該作者
39#
發(fā)表于 2025-3-28 08:17:05 | 只看該作者
Impact of Ensemble Size on the Assessment of Model Climate Signal,increased. One important question is thus the following: what is the minimum number of runs necessary to overcome the model internal variability and to study, with confidence, the model’s response to external forcing ? It is clear that the answer depends upon the signal to study and the method used to detect the signal.
40#
發(fā)表于 2025-3-28 13:52:09 | 只看該作者
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