Atmospheric convection
From FIS Freestyle wiki

Atmospheric convection is the result of a parcel-environment instability, or temperature difference, layer in the atmosphere. It is often responsible for adverse weather throughout the world.
Atmospheric convection is the result of a parcel-environment instability, or temperature difference, layer in the atmosphere.
It is often responsible for adverse weather throughout the world.
[edit] Also see
[edit] Reference
- Wikipedia Atmospheric convection [1]
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