Abstract
The relationships among convectively generated gravity waves and multi-scale organization of convection were investigated. The multi-scale organization and scale-selection of moist convection in a large-scale domain was analyzed using a cloud-resolving model. It was found that the vertical heating profile affected the amplitude of the fast and slow modes of gravity waves, where fast wave was a response to deep heating. Temperature and moisture perturbations beyond the leading edge of the slow wave were found to be insensitive to the heating profile.
| Original language | English |
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| Pages | 631-632 |
| Number of pages | 2 |
| State | Published - 2004 |
| Event | 26th Conference on Hurricanes and Tropical Meteorolgy - Miami, FL., United States Duration: May 3 2004 → May 7 2004 |
Conference
| Conference | 26th Conference on Hurricanes and Tropical Meteorolgy |
|---|---|
| Country/Territory | United States |
| City | Miami, FL. |
| Period | 05/3/04 → 05/7/04 |