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Interannual variability of surface climate in the Amazon basin

Marengo, José A.·1992·International Journal of Climatology

Abstract

This empirical study examines the circulation mechanisms of anomalously wet and dry years in the Amazon basin. Data sources include surface ship observations in the tropical Atlantic, eastern Pacific, and Indian Oceans, as well as various hydrometeorological indices in Amazonia during 1951–1983. Rainfall and river water level anomalies in northern Amazonia are associated with distinct circulation patterns in the tropical Atlantic, particularly at the March–April peak of the rainy season. Thus, abundant rainfall in northern Amazonia and high Rio Negro water levels are accompanied by a strong North Atlantic high, steep meridional pressure gradient on its equatorward side, accelerated North‐east trades, and cool surface waters in the tropical North Atlantic. The intensified North‐east trades may entail enhanced boundary‐layer moisture transport from the tropical North Atlantic into the Amazon basin. This ensemble of atmospheric and oceanic anomalies is characteristic of, but not limited to, the high phase of the Southern Oscillation (defined by anomalously high/low pressure at Tahiti/Darwin).

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Metadata

Authors
Marengo, J. A.
Venue
International Journal of Climatology
Publisher
Wiley
Published
1992-12
Volume
12
Issue
8
Pages
853-863
ISSN
  • 0899-8418 (ISSN-L)
  • 1097-0088
OpenAlex
W2141537899
Cited by
277
References
0
FWCI
2.81
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Interannual variability of surface climate in the Amazon basin. https://app.cochat.ai/papers/10.1002/joc.3370120808
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Marengo, J. A. (1992). Interannual variability of surface climate in the Amazon basin. International Journal of Climatology. https://doi.org/10.1002/joc.3370120808

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