A Squared
Well-known member
- Joined
- Nov 26, 2001
- Posts
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Why does dew point decrease?
We all know that when air is lifted, the temperature and dewpoint converge at approximately 2.5 degrees C/1000 feet Now I understand the process of adiabatic cooling, and that it occurs at about 3 degrees C per 1000 feet. The other part though I'm having a little difficulty with. As the air is lifted the *dewpoint* decreases at approximately 0.5 degrees/ 1000 feet, leaving you with a convergence of 2.5 degrees/1000 feet.
So my question is this, *why* does the dewpoint decrease? If you take a parcel of air and raise it 1000 feet, you still have the same number of water molecules and the same number of air molecules, why would the dewpoint be lower? All the references on my shelf merely state that the dewpoint decreases 0.5 C/1000 feet and leave it at that. No explanation. Any weather whizes out there? Or am I just missing something embarrassingly simple.
We all know that when air is lifted, the temperature and dewpoint converge at approximately 2.5 degrees C/1000 feet Now I understand the process of adiabatic cooling, and that it occurs at about 3 degrees C per 1000 feet. The other part though I'm having a little difficulty with. As the air is lifted the *dewpoint* decreases at approximately 0.5 degrees/ 1000 feet, leaving you with a convergence of 2.5 degrees/1000 feet.
So my question is this, *why* does the dewpoint decrease? If you take a parcel of air and raise it 1000 feet, you still have the same number of water molecules and the same number of air molecules, why would the dewpoint be lower? All the references on my shelf merely state that the dewpoint decreases 0.5 C/1000 feet and leave it at that. No explanation. Any weather whizes out there? Or am I just missing something embarrassingly simple.
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