Why do moist air parcels have a better chance


Question: Why do "moist" air parcels (which have net condensation occurring) have a better chance to remain positively buoyant as they rise (compared to "dry" parels)? a. "moist" air parcels always have a greater density than "dry" parcels, which makes it more prone to rising. b. the release of latent heat of condensation causes them to coo more slowly as they rise. c. the release of latent heat of condensation causes the parcels to get warmer overall as they rise. d. "noise" parcels cool more rapidly than "dry" air parcels as they rise

 

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