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F.A.S.T F.A.S.T
wrote...
Posts: 2792
7 years ago
Once a parcel of air rises above the lifting condensation level, the rate of cooling slows because:
A) the air surrounding the parcel is cooler.
B) water droplets absorb visible light much better than water vapor does.
C) the parcel of air continues to cool at the dry adiabatic lapse rate.
D) latent heat is released when water vapor condenses.
Textbook 
Understanding Weather and Climate

Understanding Weather and Climate


Edition: 5th
Authors:
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spinachspinach
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Posts: 1376
7 years ago
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F.A.S.T Author
wrote...
7 years ago
Thanks so much, I needed this today
wrote...
7 years ago
If you need anything else, resources for example, in this field, feel free to reply back
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