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Climate downscaling over South America for 1961–1970 using the Eta Model

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Abstract

This study shows the results from a regional climate simulation of the present-day climate, corresponding to the period 1961–1970 over South America, using the regional Eta Model nested within the HadAM3P model from the UK Hadley Centre. The simulation analysis is focused on assessing the capability of the nested regional model in representing spatial patterns of seasonal mean climate and the annual cycle of precipitation and temperature. The goals of this 10-year run for South America are to verify if the Eta Model can be used in climate-change scenarios and to verify if this model has the ability to generate added value for the South American continent. The Eta Model was chosen because there are few investigations using the Eta Model for long integrations over South America and because the vertical coordinate system used in this model is recommended for use over South America due to the presence of the Andes range. In the present 10-year simulation, the regional model reproduced many of the South American mesoscale climate features and together added new value to the driver model. Value was also added to the driver model by reducing seasonal biases in austral winter relative to austral summer. The regional model also exhibits better performance in the representation of low-level circulation, such as the topographically induced northwesterly flux.

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Authors and Affiliations

  1. National Institute for Space Research (INPE), São José dos Campos, São Paulo, Brazil

    José Fernando Pesquero, Sin Chan Chou, Carlos Afonso Nobre & José Antonio Marengo

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  1. José Fernando Pesquero
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  2. Sin Chan Chou
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  3. Carlos Afonso Nobre
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  4. José Antonio Marengo
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Correspondence to José Fernando Pesquero.

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Pesquero, J.F., Chou, S.C., Nobre, C.A. et al. Climate downscaling over South America for 1961–1970 using the Eta Model. Theor Appl Climatol 99, 75–93 (2010). https://doi.org/10.1007/s00704-009-0123-z

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  • DOI: https://doi.org/10.1007/s00704-009-0123-z

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