Answer:
The most extreme measure of water vapor that can be noticeable all around relies upon the air temperature. Hotter air has more water vapor inside it. That is the reason the muggiest days, for the most part; occur at the tallness of summer heat. Yet, as the temperature goes down, the air holds less vapors, and some changes into liquid.
The measure of water vapor noticeable all around is called outright mugginess. The measure of water vapor noticeable all around as contrasted and the measure of water that the air could hold is called relative moistness.
