Open AccessSouth American climate during the Last Glacial Maximum: Delayed onset of the South American monsoon
Author(s) -
Cook K. H.,
Vizy E. K.
Publication year - 2006
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2005jd005980
Subject(s) - last glacial maximum , climatology , monsoon , precipitation , southern hemisphere , northern hemisphere , climate model , wet season , foothills , environmental science , westerlies , amazon rainforest , geology , climate change , tropical monsoon climate , glacial period , geography , oceanography , meteorology , geomorphology , ecology , biology , cartography
The climate of the Last Glacial Maximum (LGM) over South America is simulated using a regional climate model with 60‐km resolution, providing a simulation that is superior to those available from global models that do not resolve the topography and regional‐scale features of the South American climate realistically. LGM conditions on SST, insolation, vegetation, and reduced atmospheric CO 2 on the South American climate are imposed together and individually. Remote influences are not included. Annual rainfall is 25–35% lower in the LGM than in the present day simulation throughout the Amazon basin. A primary cause is a 2–3 month delay in the onset of the rainy season, so that the dry season is about twice as long as in the present day. The delayed onset occurs because the low‐level inflow from the tropical Atlantic onto the South American continent is drier than in the present day simulation due to reduced evaporation from cooler surface waters, and this slows the springtime buildup of moist static energy that is needed to initiate convection. Once the monsoon begins in the Southern Hemisphere, LGM rainfall rates are similar to those in the present day. In the Northern Hemisphere, however, rainfall is lower throughout the (shortened) rainy season. Regional‐scale structure includes slight precipitation increases in the Nordeste region of Brazil and along the eastern foothills of the Andes, and a region in the center of the Amazon basin that does not experience annual drying. In the Andes Mountains, the signal is complicated, with regions of significant rainfall increases adjacent to regions with reduced precipitation.