A regional response in mean westerly circulation and rainfall to projected climate warming over Tasmania, Australia
Coupled ocean–atmosphere general circulation models (GCMs) lack sufficient resolution to model the regional detail of changes to mean circulation and rainfall with projected climate warming. In this paper, changes in mean circulation and rainfall in GCMs are compared to those in a variable resolutio...
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Veröffentlicht in: | Climate dynamics 2013-04, Vol.40 (7-8), p.2035-2048 |
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Sprache: | eng |
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