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2007-10-15 12:35:42 · 2 answers · asked by dupre1ke 1 in Science & Mathematics Weather

2 answers

You want to find the temperature that a parcel would have after all the latent heat of vaporization is added to it and then the parcel is taken back down to 1000 mb. Starting at whatever level you are at, follow a dry adiabat until the parcel is saturated, then follow a saturation adiabat to some high level, where there is essentially no water vapor left in the parcel. You can tell this because the saturation and dry adiabats become parallel at this pressure (200 mb will usually do). Then follow a dry adiabat back down to 1000 mb and read off the temperature. That will be the theta e.

2007-10-15 15:31:08 · answer #1 · answered by pegminer 7 · 0 0

I have no clue

2007-10-15 14:35:30 · answer #2 · answered by Anonymous · 0 0

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