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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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21#
發(fā)表于 2025-3-25 05:46:24 | 只看該作者
North-Atlantic Decadal Climate Variability in a Coupled Atmosphere/Ocean/Sea-Ice Model of Moderate the Greenland Sea, the Labrador Sea and the area close to Bermuda (Deser and Blackmon 1993, Kushnir 1994). Unstable air/sea interactions might well occur in this area, potentially affecting climate variability on various time-scales.
22#
發(fā)表于 2025-3-25 08:43:37 | 只看該作者
Antonio NavarraBroad coverage of the topic (observations, models).The contributing authors represent the most active research groups in the field.Includes supplementary material:
23#
發(fā)表于 2025-3-25 11:52:51 | 只看該作者
http://image.papertrans.cn/b/image/185178.jpg
24#
發(fā)表于 2025-3-25 19:40:46 | 只看該作者
https://doi.org/10.1007/978-3-642-58369-8Climate Variability; Climatology; Klima; Klimatologie; Klima?nderung; Monsoon Dynamics; Monsun; Monsundynam
25#
發(fā)表于 2025-3-25 20:13:27 | 只看該作者
978-3-642-63556-4Springer-Verlag Berlin Heidelberg 1999
26#
發(fā)表于 2025-3-26 00:08:33 | 只看該作者
27#
發(fā)表于 2025-3-26 06:32:22 | 只看該作者
David Hogan,Trivina Kang,Melvin Chane properties of the equatorial thermocline because of an influx of water from higher latitudes. The influx affects equatorial sea surface temperatures and hence the tropical and extra-tropical winds that in turn affect the influx. Such processes can give rise to continual interdecadal oscillations.
28#
發(fā)表于 2025-3-26 08:59:09 | 只看該作者
29#
發(fā)表于 2025-3-26 14:52:51 | 只看該作者
International Handbook of Urban Educationed by simple and more complete general circulation ocean models (see the review by Duchene and Frankignoul (1990)). Details of this circulation specially difficult to simulate are the subject of recent studies with high resolution models (Johns et al. (1990), Schott and Boening (1991)).
30#
發(fā)表于 2025-3-26 19:03:29 | 只看該作者
Simulations of the Variability of the Tropical Atlantic,ed by simple and more complete general circulation ocean models (see the review by Duchene and Frankignoul (1990)). Details of this circulation specially difficult to simulate are the subject of recent studies with high resolution models (Johns et al. (1990), Schott and Boening (1991)).
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