Abstract
The transient behavior of meridional moisture transport across the South American continent is examined with the reanalysis data provided by the European Centre for Medium-range Weather Forecasts (ECMWF). The results show clearly the effects of the valley between the Andes and the Brazilian Plateau in canalizing the southward moisture transport: an intense jet is episodically formed in this valley. The synoptic variability of this low-level jet and its relation to the large-scale atmospheric circulation are studied.
| Original language | English |
|---|---|
| Pages (from-to) | 1409-1412 |
| Number of pages | 4 |
| Journal | Geophysical Research Letters |
| Volume | 26 |
| Issue number | 10 |
| DOIs | |
| Publication status | Published - 15 May 1999 |
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