Air’s ability to hold water vapor increases exponentially as temperature increases, meaning that warmer air can contain significantly more moisture than cooler air, which plays a critical role in weather patterns, humidity levels, and the formation of precipitation.
Air @ 90o F (32o C)& 90% Relative Humidity (RH) can hold 500% more water than air at 50o F (10o C) & 90% RH.
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