Synergism between the low-level jet and organized convection at its exit region
Previous studies suggest that the enhanced meridional extent of some South American low-level jet events (known as Chaco jets) is a consequence of a positive feedback between the low-level wind and strong convection that is usually observed at their exit region. To assess how this interaction takes...
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2007
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| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00270644_v135_n4_p1310_Saulo http://hdl.handle.net/20.500.12110/paper_00270644_v135_n4_p1310_Saulo |
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