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dc.contributor.authorSwann, Abigail L.S.
dc.contributor.authorLongo, Marcos
dc.contributor.authorKnox, Ryan G.
dc.contributor.authorEunjee, Lee
dc.contributor.authorMoorcroft, Paul R.
dc.date.accessioned2020-06-11T17:53:26Z
dc.date.available2020-06-11T17:53:26Z
dc.date.issued2015-12
dc.identifier.citationA. L. S. Swann, M. Longo, R. G. Knox, E. Lee, and P. R. Moorcroft. Future deforestation in the amazon and consequences for south american climate. Agricultural and Forest Meteorology, 214–215:12–24, 12 2015.en_US
dc.identifier.otherdoi: 10.1016/j.agrformet.2015.07.006
dc.identifier.urihttp://hdl.handle.net/1773/45559
dc.descriptionThis dataset provides the model output used in this study, in particular the data needed to create the figures included in the published paper. The data is provided in matlab binary format.en_US
dc.description.abstractOngoing agricultural expansion in Amazonia and the surrounding areas of Brazil is expected to continue over the next several decades as global food demand increases. The transition of natural forest and savannah ecosystems to pastureland and agricultural crops is predicted to create warmer and drier atmospheric conditions than the native vegetation. Using a coupled ecosystem regional atmospheric model (EDBRAMS) we investigate the expected impacts of predicted future land use on the climate of South America. The climate response in the model simulations is generally consistent with expectations from previous global modeling simulations with drier conditions resulting from deforestation, however the changes in precipitation are relatively small (on order of a few percent). Local drying is driven primarily by decreases in evapo-transpiration associated with the loss of forest, and concomitant increases in runoff. Significant changes in convectively available potential energy (CAPE) and convective inhibition (CIN) during the transition to the wet season indicate that the decrease in surface latent heat flux is indeed leading to a drier atmosphere, however these changes occur around a mean climatological state that is already very favorable for convection, and thus lead to relatively small changes in precipitation. If, however, these land use changes were to occur under a background state of drier conditions, such as those predicted for the future global climate model experiments, this additional atmospheric drying may be sufficient to decrease precipitation more substantially.en_US
dc.description.sponsorshipWe acknowledge National Science Foundation Awards AGS- 1321745 and EF-1340649 to the University of Washington, as well as National Science Foundatiaon Award AGS-0449793 and National Aeronautics and Space Administration Grant NNG06GD63G to the Massachusetts Institute of Technology. This work was partially conducted while A.L.S.S. and E.L. were Giorgio Ruffolo Fellows in the Sustainability Science Program at Harvard University, for which support from Italy’s Ministry for Environment, Land and Sea is gratefully acknowledged. M.L. was supported by Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq). Britaldo Soares Filho provided the SimAmazonia scenarios.en_US
dc.language.isoen_USen_US
dc.publisherAgriculture and Forest Meteorologyen_US
dc.rightsAttribution-NonCommercial-ShareAlike 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/3.0/us/*
dc.subjectModel outputen_US
dc.subjectdeforestationen_US
dc.subjectAmazonen_US
dc.titleData in support of: Future deforestation in the Amazon and consequences for South American climateen_US
dc.typeDataseten_US


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