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- W4230169117 abstract "Publisher SummaryClimate of the Southern Andes is strongly influenced by three factors—namely, the Southern Westerlies, the meridional barrier to air flow imposed by the Andean cordillera, and the cold offshore current. The air stream of the Southern Westerlies, the dominant factor, originates offshore, its strength regulated by pressure differences between 40° and 60°S. Temperature and precipitation regimes range from subtropical to subantarctic. Meteorological parameters inland from the Pacific are dictated by topography embraced by the Cordillera de la Costa, Valle Central, and Andes. Hyperhumid, cool-temperate conditions on the Pacific side of the Andes beyond 42°S are most intense among the islands and waterways lying outermost between Golfo de Penas (47°S) and Cabo de Hornos (56°S0). Climatic conditions become less humid in southernmost Patagonia and Fuegia. The climatic pattern in the Southern Andes results from the action of two principal atmospheric circulation centers. Among additional factors, exerting climatic control, are solar forcing, Hadley cell circulation, and the E Niño/ Southern Oscillation (ENSO). ENSO the system of atmospheric-oceanic contrasts represents the out-of-phase relationship currently in effect between sea-level pressure in the Australia–Indonesia region and the eastern tropical Pacific." @default.
- W4230169117 created "2022-05-11" @default.
- W4230169117 date "2003-01-01" @default.
- W4230169117 modified "2023-09-27" @default.
- W4230169117 title "Chapter 4 Climate" @default.
- W4230169117 doi "https://doi.org/10.1016/s1571-0866(03)80007-6" @default.
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