GENESIS OF MESOSCALE CONVECTIVE SYSTEMS ABOVE UNEVEN SOIL MOISTURE CONDITIONS
Heterogeneities in vegetation type, soil type, or soil moisture can induce physiographically forced mesoscale circulations through sensible heat flux gradients at the surface. These mesoscale circulations can provide regions of convergence, triggering deep convection. Here, Cheng and Cotton examine...
Gespeichert in:
Veröffentlicht in: | Bulletin of the American Meteorological Society 2005-01, Vol.86 (1), p.37 |
---|---|
Hauptverfasser: | , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
Zusammenfassung: | Heterogeneities in vegetation type, soil type, or soil moisture can induce physiographically forced mesoscale circulations through sensible heat flux gradients at the surface. These mesoscale circulations can provide regions of convergence, triggering deep convection. Here, Cheng and Cotton examine the sensitivity of a simulation of the genesis of a mesoscale convective system to the initial soil moisture distribution. |
---|---|
ISSN: | 0003-0007 1520-0477 |