The dissipating stage signifies the end of a thunderstorm as downdrafts take over from updrafts, leading to dissipation.
The dissipating stage marks the end of a thunderstorm when updrafts are overtaken by downdrafts, halting convective uplift. Cool air entrainment stabilizes the cloud, leading to the dissipation of the storm. As cool downdrafts dominate, the rain stops, and the storm gradually weakens.
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