1. Equivalent potential temperatureEquivalent potential temperature, commonly referred to as theta-e, is a quantity related to the stability of a column of air in the atmosphere. is the temperature a parcel of air would reach if all the water vapor in the parcel were to condense, releasing its latent heat, and the parcel was brought adiabatically to a standard reference pressure, usually 1000 hPa which is roughly equal to atmospheric pressure at sea level. In stable conditions, increases with altitude.
Read “Equivalent potential temperature” on English Wikipedia
Read “相当温位” on Japanese Wikipedia
Read “Equivalent potential temperature” on DBpedia
Read “Equivalent potential temperature” on English Wikipedia
Read “相当温位” on Japanese Wikipedia
Read “Equivalent potential temperature” on DBpedia
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