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

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https://doi.org/10.1007/978-1-4020-5199-9 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.

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David Hogan,Trivina Kang,Melvin ChanNiño, but as part of a decadal climate fluctuation that is governed by different physical processes. Whereas interannual fluctuations, including El Niño, amount primarily to a horizontal redistribution of warm surface waters within the tropics, interdecadal climate fluctuations involve changes in th

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International Handbook of Violence Research to the abyssal ocean. It is organized in basin-scale coherent current systems, which are globally connected through the Southern Ocean (see e.g. Schmitz 1995 for a review and Macdonald and Wunsch 1996 for a recent quantitative estimate). The flow is driven by surface heat and freshwater (i.e. buoya

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Reference work 2019Latest editionare coming to be recognized as having climates that are among the most variable in the world. The variability is on timescales of interannual-to-decadal and beyond, with the decadal variability being among the most pronounced so far identified in the historical climate records of the 20th Century.

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International Handbook of Universities 2019ature (SST) in the regulation of the climatic variability. Namias (1959, 1963) proposed that the low-frequency variability over North America might be connected with the SST variations over the equatorial and tropical Pacific Ocean. An early attempt to produce long-range forecasts based on SST was attempted by Adem and Jacob (1968).

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Climate Variability in Northern Africa: Understanding Droughts in the Sahel and the Maghreb,are coming to be recognized as having climates that are among the most variable in the world. The variability is on timescales of interannual-to-decadal and beyond, with the decadal variability being among the most pronounced so far identified in the historical climate records of the 20th Century.

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SST-Forced Experiments and Climate Variability,ature (SST) in the regulation of the climatic variability. Namias (1959, 1963) proposed that the low-frequency variability over North America might be connected with the SST variations over the equatorial and tropical Pacific Ocean. An early attempt to produce long-range forecasts based on SST was attempted by Adem and Jacob (1968).