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...
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Veröffentlicht in: | Bulletin of the American Meteorological Society 2005-01, Vol.86 (1), p.37 |
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description | 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. |
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source | American Meteorological Society; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; JSTOR Archive Collection A-Z Listing |
subjects | Mesoscale convective complexes Moisture Sensible heat Sensitivity analysis Simulation Soil moisture Soil types Soils |
title | GENESIS OF MESOSCALE CONVECTIVE SYSTEMS ABOVE UNEVEN SOIL MOISTURE CONDITIONS |
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