2005
DOI: 10.1175/jcli-3266.1
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Climate Downscaling over Nordeste, Brazil, Using the NCEP RSM97

Abstract: The NCEP Regional Spectral Model (RSM), with horizontal resolution of 60 km, was used to downscale the ECHAM4.5 AGCM (T42) simulations forced with observed SSTs over northeast Brazil. An ensemble of 10 runs for the period January-June 1971-2000 was used in this study. The RSM can resolve the spatial patterns of observed seasonal precipitation and capture the interannual variability of observed seasonal precipitation as well. The AGCM bias in displacement of the Atlantic ITCZ is partially corrected in the RSM. … Show more

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Cited by 59 publications
(35 citation statements)
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“…Souza Filho & Lall 2003, Sun et al 2005, 2007 based on a complete arsenal of regional climatic statistical and numerical modelling (using various types of downscaling techniques). In collaboration with other national and international institutes (e.g.…”
Section: Discussionmentioning
confidence: 99%
“…Souza Filho & Lall 2003, Sun et al 2005, 2007 based on a complete arsenal of regional climatic statistical and numerical modelling (using various types of downscaling techniques). In collaboration with other national and international institutes (e.g.…”
Section: Discussionmentioning
confidence: 99%
“…In this approach, the regional climate model is forced by low-resolution fields from the AGCM. This method has been used in many problems, including seasonal precipitation forecasts over the northeast of Brazil (Sun et al, 2005(Sun et al, , 2006. The purpose of this work is to investigate whether the higher resolution of the regional model could improve upon the skill of the AGCM to simulate seasonal TC activity.…”
Section: Introductionmentioning
confidence: 99%
“…An example would be when a grid square is located mainly over the windward part of an mountain range, but we are interested in forecasting for a town on the inland, or leeward, side of the mountain range-a location whose rainfall anomaly tendency may be in the opposite sense to that of the average over the grid square. Resolving the often opposing anomalies may be done either statistically, as tested in South Africa (Landman et al 2009), or through use of a regional dynamical model, as was done for semi-arid northeast Brazil in an IRI project in the early 2000s (Sun et al 2005), or likewise in recent work focusing both there and in Chile, in the context of water management issues .…”
Section: Specialized or Tailored Forecastsmentioning
confidence: 99%