On 2004/09/06, at 13:48, Mike Geary wrote: > > Humidity depends upon the temperature of the air and the moisture > available > to saturate the air. The number of grains of water vapor varys with > temperature. Each degree of temperature rise will support an ever > greater > number of grains of moisture. At any specific temperature air will > support > a specific number of grains of moisture, beyond that point the moisture > condenses out. The measure of grains of water vapor in the air is the > humidity of the air. Relative humidity is the measure of humidity > relative > to the amount of humidity the air could hold at that temperature. If > there > is plenty of moisture being supplied to a mass of hot air it could > reach > 100%, in which case it would be raining. Comfort depends on the > relative > humidity-- if the air mass around Memphis is say 97 degrees and a > steady > supply of moisture is being pumped up from the Gulf of Mexico to mix > with > that air mass then the relative humidity could easily be 95% which it > often > is in Memphis in summer. This air would feel wetter than 97 degrees > at > Myrtle Beach with 85% relative humidity (if, say, the wind is blowing > from > inland) because the rate of sweat evaporation would be appreciably > less in > the 95% relative humidity of Memphis and one's skin would tend to > become wet > with perspiration. Count on the air-conditioning expert. One contributing factor may be the direction of prevailing winds, carrying moist air toward the land or dry air toward the sea. John McCreery ------------------------------------------------------------------ To change your Lit-Ideas settings (subscribe/unsub, vacation on/off, digest on/off), visit www.andreas.com/faq-lit-ideas.html