Atmospheric convection

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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

1. Wikipedia Atmospheric convection [1]

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