Thermodynamic retrieval analysis applied to a composite of dual-Dopple
r radar data obtained in the 10-11 June 1985 PRE-STORM (Preliminary Re
gional Experiment for STORM-Central) squall line and a model simulatio
n of a similar squall line show that the upper-level downdrafts locate
d ahead of and behind the main convective updraft zone were generally
positively buoyant. As a result, the upper-level downdrafts contribute
d negatively to the system heat flux.