Abstract
During convective outbreaks the integrated heating and drying of the large scale by the cumulonimbus activity has a magnitude of the order of 10°C day-1. The heat and moisture sources are dominated by the flux divergence terms, which account for over 90% of the variance. The observed warming is as large as ±1°C day -1 but is diurnally dominated and does not correspond to the latent heat release. The integrated moisture convergence has a high correlation with latent heat release but not with the measured moisture storage. The convective heat source is also highly correlated with middle tropospheric vertical velocity. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 2701-2713 |
| Number of pages | 13 |
| Journal | Monthly Weather Review |
| Volume | 117 |
| Issue number | 12 |
| DOIs | |
| State | Published - 1989 |