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dc.contributor.authorNegrón-Juárez, Robinson I.-
dc.contributor.authorChambers, Jeffrey Quintin-
dc.contributor.authorGuimarães, Giuliano Piotto-
dc.contributor.authorZeng, Hongcheng-
dc.contributor.authorRaupp, Carlos Frederico Mendonça-
dc.contributor.authorMarra, Daniel Magnabosco-
dc.contributor.authorRibeiro, Gabriel Henrique Pires de Mello-
dc.contributor.authorSaatchi, Sassan S.-
dc.contributor.authorNelson, Bruce Walker-
dc.contributor.authorHiguchi, Niro-
dc.date.accessioned2020-06-15T21:53:24Z-
dc.date.available2020-06-15T21:53:24Z-
dc.date.issued2010-
dc.identifier.urihttps://repositorio.inpa.gov.br/handle/1/18291-
dc.description.abstractClimate change is expected to increase the intensity of extreme precipitation events in Amazonia that in turn might produce more forest blowdowns associated with convective storms. Yet quantitative tree mortality associated with convective storms has never been reported across Amazonia, representing an important additional source of carbon to the atmosphere. Here we demonstrate that a single squall line (aligned cluster of convective storm cells) propagating across Amazonia in January, 2005, caused widespread forest tree mortality and may have contributed to the elevated mortality observed that year. Forest plot data demonstrated that the same year represented the second highest mortality rate over a 15-year annual monitoring interval. Over the Manaus region, disturbed forest patches generated by the squall followed a power-law distribution (scaling exponent α = 1.48) and produced a mortality of 0.3-0.5 million trees, equivalent to 30% of the observed annual deforestation reported in 2005 over the same area. Basin-wide, potential tree mortality from this one event was estimated at 542 ± 121 million trees, equivalent to 23% of the mean annual biomass accumulation estimated for these forests. Our results highlight the vulnerability of Amazon trees to wind-driven mortality associated with convective storms. Storm intensity is expected to increase with a warming climate, which would result in additional tree mortality and carbon release to the atmosphere, with the potential to further warm the climate system. © 2010 by the American Geophysical Union.en
dc.language.isoenpt_BR
dc.relation.ispartofVolume 37, Número 16pt_BR
dc.rightsRestrito*
dc.subjectDeforestationen
dc.subjectPrecipitation (meteorology)en
dc.subjectStormsen
dc.subjectAmazon Forestsen
dc.subjectAmazoniaen
dc.subjectBiomass Accumulationen
dc.subjectClimate Systemen
dc.subjectConvective Stormsen
dc.subjectExtreme Precipitationen
dc.subjectForest Patchesen
dc.subjectForest Plotsen
dc.subjectMortality Rateen
dc.subjectPower Law Distributionen
dc.subjectScaling Exponenten
dc.subjectSquall Linesen
dc.subjectStorm Intensityen
dc.subjectTree Mortalityen
dc.subjectWarming Climateen
dc.subjectClimate Changeen
dc.subjectAtmospheric Pollutionen
dc.subjectBiomassen
dc.subjectBiomonitoringen
dc.subjectCarbon Emissionen
dc.subjectCluster Analysisen
dc.subjectConvective Systemen
dc.subjectDeforestationen
dc.subjectGlobal Warmingen
dc.subjectMortalityen
dc.subjectPopulation Distributionen
dc.subjectPower Law Distributionen
dc.subjectPrecipitation (climatology)en
dc.subjectQuantitative Analysisen
dc.subjectSquall Lineen
dc.subjectStormen
dc.subjectTreeen
dc.subjectVulnerabilityen
dc.subjectClimatesen
dc.subjectDeforestationen
dc.subjectPrecipitationen
dc.subjectAmazonasen
dc.subjectBrasilen
dc.subjectManausen
dc.titleWidespread Amazon forest tree mortality from a single cross-basin squall line eventen
dc.typeArtigopt_BR
dc.identifier.doi10.1029/2010GL043733-
dc.publisher.journalGeophysical Research Letterspt_BR
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