
but that's probably the worst explanation of
dewpoint and RH I have ever read. He doesn't explain what either one is, and the typo in the phrase "closeness the air is the saturation" will
probably confuse almost everyone who reads it. Even if he got the words right "closeness the air is TO saturation" it is very awkward and doesn't
fully explain the physics. There's no easy way to describe these terms other than directly: relative humidity is a measure of how much water vapor
the air contains as a function of how much water it could contain at any particular temperature. At 50% RH the air contains half the water vapor it
could contain at that temperature. How much water vapor the air can contain is a function of temperature. The warmer the air, the more water vapor
it can hold. Dewpoint is the temperature at which the air becomes fully saturated (RH=100%). Cooled to the dewpoint, the air can't hold any more
water vapor and the water vapor begins to condense (clouds form, windows fog up, etc.) On a cold day outside, warm air inside is cooled next to a
window (which is cold). If the temperature of the air adjacent to the window reaches the dewpoint, it can't hold any more water vapor and the water
vapor condenses into water droplets on the inside of the window. The same thing is happening on the outside of my scotch glass right now, which is
probably why I didn't do a better job of explaining this 

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