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...
Guardado en:
| Autores principales: | Saulo, C., Ruiz, J., García Skabar, Y. |
|---|---|
| Formato: | JOUR |
| Materias: | |
| Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_00270644_v135_n4_p1310_Saulo |
| Aporte de: |
Ejemplares similares
-
Synergism between the low-level jet and organized convection at its exit region
Publicado: (2007) -
Diurnal cycle in convergence patterns in the boundary layer east of the Andes and convection
por: Nicolini, M., et al. -
Diurnal cycle in convergence patterns in the boundary layer east of the Andes and convection
por: Nicolini, María Gabriela -
Diurnal cycle in convergence patterns in the boundary layer east of the Andes and convection
por: Nicolini, Matilde
Publicado: (2011) -
The South American low-level jet experiment
por: Vera, C., et al.