RegCM3 nested in HadAM3 scenarios A2 and B2: projected changes in extratropical cyclogenesis, temperature and precipitation over the South Atlantic Ocean


Autoria(s): Krueger, Luiz Fernando; da Rocha, Rosmeri Porfirio; Reboita, Michelle Simoes; Ambrizzi, Tercio
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

04/11/2013

04/11/2013

2012

Resumo

The RegCM3 (Regional Climate Model-version 3) was nested in HadAM3 model to simulate present (1975-1989, referred hereafter as RegHad) and two future climate scenarios (A2 and B2 from 2071 to 2085, referred as RegA2 and RegB2) over the South America (SA) and South Atlantic Ocean (SAO). Projected changes in the air temperature, precipitation, low level circulation and cyclogenesis climatology were investigated. The cyclogenesis were identified using an automatic scheme for tracking based on the minimum of relative vorticity (zeta) from 10-m height wind. During summer, a general decrease (increase) in the precipitation is projected by RegA2 and RegB2 over the northeastern SA (center-west and south Brazil, north Argentina and Uruguay). For winter, an anomalous low level anticyclonic circulation is associated with the reduction in the rainfall over the central part of southern Brazil in RegA2 and RegB2 scenarios. Similar to HadAM3, RegCM3 projects larger warming in A2 scenario. For the present climate, when compared to HadAM3, RegHad defines better both the location of the main cyclogenetic areas and its annual cycle near southwestern SAO. The projections indicate a reduction in the total number of cyclones of -7.2% and -4.7% for RegA2 and RegB2, respectively, while HadAM3 reduction is -4.5% for both scenarios. The decrease is larger for initially intense cyclones (zeta <=-<= 2.5 x 10(-5) s-(1)): -20.9% (RegA2) and -11.3% (RegB2). For the lifetime, distance traveled and mean velocity of the cyclones, the A2 and B2 scenarios present mean values close to the present climate ( 3 days, 1900 km, and 9 m s(-1), respectively). Regarding the initial mean vorticity of the systems, RegB2 simulates values similar to the present climate, but they are initially weaker in RegA2. In general, RegA2 and RegB2 show a large decrease in the number of cyclones over the southern SAO due to an anticyclonic anomaly covering SAO between 30-55A degrees S. The reduction is larger in the scenario with higher concentrations of greenhouse gases (RegA2).

CAPES (Coordenacao de Aperfeicoamento de Nivel Superior)

Coordenacao de Aperfeicoamento de Nivel Superior (CAPES)

Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) of Brazil [Proc. 307519/2008-2, 476361/2006-0]

Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) of Brazil

CLARISLPB (A EuropeSouth America Network for Climate Change Assessment and Impact Studies in La Plata Basin) European Community

CLARIS-LPB (A Europe-South America Network for Climate Change Assessment and Impact Studies in La Plata Basin) European Community

CNPq

CNPq

CNPq/FAPESP INCT for Climate Change

CNPq/FAPESP INCT for Climate Change

FAPESP

FAPESP

Identificador

CLIMATIC CHANGE, DORDRECHT, v. 113, n. 41367, supl., Part 3, pp. 599-621, AUG, 2012

0165-0009

http://www.producao.usp.br/handle/BDPI/40863

10.1007/s10584-011-0374-4

http://dx.doi.org/10.1007/s10584-011-0374-4

Idioma(s)

eng

Publicador

SPRINGER

DORDRECHT

Relação

CLIMATIC CHANGE

Direitos

closedAccess

Copyright SPRINGER

Palavras-Chave #REGIONAL CLIMATE MODELS #LATE 20-1ST CENTURY #CYCLONE CLIMATOLOGY #WINTER CYCLONE #STORM TRACKS #SEA-ICE #HEMISPHERE #SIMULATION #AMERICA #VARIABILITY #ENVIRONMENTAL SCIENCES #METEOROLOGY & ATMOSPHERIC SCIENCES
Tipo

article

original article

publishedVersion