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• W9137317 abstract "We explore how the moist deep convection over the Amazonian region responds to glacial forcings compared to the pre-indrustrial climate and how this change might interact with the meridional shift of rainfall over Nordeste, Pacific and Atlantic tropical Oceans. The objective is to assess and investigate the individual contributions of greenhouse gases concentration, ice sheet topography and/or albedo on the hydrological changes over tropical South America and their links to the Hadley and Walker circulations. We employ coupled ocean-atmosphere simulations for the Last Glacial Maximum and sensitivity experiments for each Last Glacial Maximum forcing. We show that the Last Glacial Maximum reduced greenhouse gases alone can explain the observed rainfall changes over tropical South America through the induced increase in tropical and northern extra-tropical dry static stability and altered Hadley circulation. Furthermore, we show that the topography of the North American ice sheet reinforces the equatorward shift of the descending branch of the Hadley cell leading to stronger subsidence and drying over the northern tropics. However, we show that the Laurentide ice sheet has also a significant influence on the simulated enhanced rainfall over Nordeste and Southeastern Brazil via the eastward shift of the Walker circulation, with a mechanism analogous to the atmospheric thermodynamical response to El-Nino conditions." @default.
• W9137317 created "2016-06-24" @default.
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• W9137317 date "2009-01-01" @default.
• W9137317 modified "2023-09-25" @default.
• W9137317 title "Sensitivity of South American Tropical Climate to Last Glacial Maximum Boundary Conditions: Focus on Teleconnections with Tropics and Extratropics" @default.
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• W9137317 doi "https://doi.org/10.1007/978-90-481-2672-9_9" @default.
• W9137317 hasPublicationYear "2009" @default.
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