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Thermodynamic retrieval analysis applied to a composite of dual-Doppler radar data obtained in the 10–11 June 1985 PRE-STORM (Preliminary Regional Experiment for STORM-Central) squall line and a model simulation of a similar squall line show that the upper-level downdrafts located ahead of and behind the main convective updraft zone were generally positively buoyant. As a result, the upper-level downdrafts contributed negatively to the system heat flux.
Thermodynamic retrieval analysis applied to a composite of dual-Doppler radar data obtained in the 10–11 June 1985 PRE-STORM (Preliminary Regional Experiment for STORM-Central) squall line and a model simulation of a similar squall line show that the upper-level downdrafts located ahead of and behind the main convective updraft zone were generally positively buoyant. As a result, the upper-level downdrafts contributed negatively to the system heat flux.
| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 899 | 778 | 22 |
| PDF Downloads | 109 | 42 | 2 |
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