atmosphere_stability_k_index

The atmosphere_stability_k_index is an index that indicates the potential of severe convection and is often referred to a simply the k index. The index is derived from the difference in air temperature between 850 and 500 hPa, the dew point temperature at 850 hPa, and the difference between the air temperature and the dew point temperature at 700 hPa.

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Proposls with this term version:

Proposal: Jonathan Wrotny [new standard name: atmosphere_stability_]

Proposal: Jonathan Gregory [Modify description of atmosphere_stabili]

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