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contributor authorMisra, Vasubandhu
date accessioned2017-06-09T16:30:12Z
date available2017-06-09T16:30:12Z
date copyright2009/12/01
date issued2009
identifier issn1525-755X
identifier otherams-69034.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210659
description abstractThe remote influence of the El Niño?Southern Oscillation (ENSO) strongly manifests over the equatorial Amazon (EA)?including parts of southern Venezuela, Guyana, French Guiana, and Suriname?when there is a large-scale anomalous upper-level divergence over continental tropical South America. Modeling studies conducted in this paper suggest that it is because of the modulation of the local diurnal cycle of the moisture flux convergence, which results in the local amplification of the ENSO signal over the EA. Further, it is shown that the local land surface feedback plays a relatively passive but important role of maintaining these interannual precipitation anomalies over the EA region.
publisherAmerican Meteorological Society
titleThe Amplification of the ENSO Forcing over Equatorial Amazon
typeJournal Paper
journal volume10
journal issue6
journal titleJournal of Hydrometeorology
identifier doi10.1175/2009JHM1108.1
journal fristpage1561
journal lastpage1568
treeJournal of Hydrometeorology:;2009:;Volume( 010 ):;issue: 006
contenttypeFulltext


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