The effect of Amazonian deforestation on the northern hemisphere circulation and climate

Concern about tropical deforestation has often focused on local climate or ecological change. Less research has been carried out on its possible effects on the global climate, although possible mechanisms for such an occurrence have been proposed. Here we use a general circulation model (GCM) to sho...

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Bibliographic Details
Published inGeophysical research letters Vol. 27; no. 19; pp. 3053 - 3056
Main Authors Gedney, Nicola, Valdes, Paul J.
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 01.10.2000
American Geophysical Union
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Summary:Concern about tropical deforestation has often focused on local climate or ecological change. Less research has been carried out on its possible effects on the global climate, although possible mechanisms for such an occurrence have been proposed. Here we use a general circulation model (GCM) to show that complete Amazonian deforestation can result in changes in the climate far afield from the region of deforestation. In particular, the model predicts statistically significant changes to winter rainfall over the NE Atlantic, extending towards western Europe. These are associated with large‐scale circulation changes in middle and high latitudes. Simulation of these circulation changes with a simple model confirms the physical mechanism responsible (planetary wave propagation) implying that the result is robust and relatively independent of the GCM used.
Bibliography:istex:72F545569161A1E1FF447BDE90A7A0C2A07DDE8A
ark:/67375/WNG-T9VF9FZ3-T
ArticleID:2000GL011794
ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 23
ISSN:0094-8276
1944-8007
DOI:10.1029/2000GL011794