- Tropical air mass convection in a sky in constant flux
- W889710T
- Deep moisture below dry air in an unstable tropical air mass means a continual turning over of the air with updrafts and downdrafts. While some areas are thriving with new convection (banks of Cumulus Congestus), other parts have evaporating anvils or Altocumulus patches, all in a state of constant flux. The sky appear as a complex mix of different clouds although all of them are constantly changing.
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