Recent studies have shown that global warming and associated sea-surface temperature (SST) changes may trigger an important rainfall increase in Southeastern South America (SESA) during the austral summer (December-January-February, DJF). The goal of this paper is to provide some insight into processes which may link global and SESA changes. For this purpose, a “two-way nesting” system coupling interactively the regional and global versions of the LMDZ4 atmospheric model is used to study the response to prescribed SST changes. The regional model is a variable grid version of the global model, with a zoom focused over South America. An ensemble of simulations forced by distinct patterns of DJF SST changes has been carried out using a decomp...
During austral summer, persistent tropical-extratropical (TE) cloud bands, such as the South Atlanti...
Nine models from the Coupled Model Intercomparison Project version 3 dataset are employed to examin...
In this study, we investigate atmospheric blocking over east South America in austral summer for the...
International audienceRecent studies have shown that global warming and associated sea-surface tempe...
December–January–February (DJF) rainfall variability in southeastern South America (SESA) is studied...
Southeastern South America (SESA) is one of the few subtropical regions where WCRP/CMIP3 coupled gen...
The climate changes observed in the last decades have raised concern among policy and decision maker...
Observed austral summertime (November through April) rainfall in southeastern South America (SESA)—i...
Austral summer (DJF) precipitation over tropical South America (SA) is characterized by the South Am...
Impacts of the main South American orographic structures (the Andes, the Brazilian Plateau and the G...
The regional influence of the Madden–Julian oscillation (MJO) on South America is described. Maps of...
A reconstructed rainfall dataset, and satellite estimates are used to analyze interannual to decadal...
The Community Climate Model (CCM3) from the National Center for Atmospheric Research (NCAR) is used ...
The representation of the South American Monsoon System (SAMS) by general circulation models (GCMs) ...
During austral summer, persistent tropical-extratropical (TE) cloud bands, such as the South Atlanti...
Nine models from the Coupled Model Intercomparison Project version 3 dataset are employed to examin...
In this study, we investigate atmospheric blocking over east South America in austral summer for the...
International audienceRecent studies have shown that global warming and associated sea-surface tempe...
December–January–February (DJF) rainfall variability in southeastern South America (SESA) is studied...
Southeastern South America (SESA) is one of the few subtropical regions where WCRP/CMIP3 coupled gen...
The climate changes observed in the last decades have raised concern among policy and decision maker...
Observed austral summertime (November through April) rainfall in southeastern South America (SESA)—i...
Austral summer (DJF) precipitation over tropical South America (SA) is characterized by the South Am...
Impacts of the main South American orographic structures (the Andes, the Brazilian Plateau and the G...
The regional influence of the Madden–Julian oscillation (MJO) on South America is described. Maps of...
A reconstructed rainfall dataset, and satellite estimates are used to analyze interannual to decadal...
The Community Climate Model (CCM3) from the National Center for Atmospheric Research (NCAR) is used ...
The representation of the South American Monsoon System (SAMS) by general circulation models (GCMs) ...
During austral summer, persistent tropical-extratropical (TE) cloud bands, such as the South Atlanti...
Nine models from the Coupled Model Intercomparison Project version 3 dataset are employed to examin...
In this study, we investigate atmospheric blocking over east South America in austral summer for the...