- Orographic convection: Cumulus clouds bubbling over mountains
- W838611S
- Orographic convection: mountains topped by bubbling Cumulus towers in dry air. The mountain at lower left is causing repeated cloud development. As each Congestus tower forms, it drops a small shower that cools the air and temporarily stops new updrafts. It then drifts to the right as it freezes and evaporates, allowing a new cloud to form at the original location.
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