The amount of water vapor in the air varies considerably depending on climate and weather. In a desert water vapor may account for a tiny fraction of a percent of the air. In a tropical rainforest during a storm water vapor may account for as much as 4% of the air.
All clouds have the potential to be rain clouds. It just depends on how much water vapor is in them. Once the water vapor in a cloud cools or becomes too heavy, it rains. Clouds with lots of water are generally dark gray as opposed to white clouds with less water.
Thermosphere contain the same gases as troposphere but in very low concentrations: oxygen, nitrogen argon.
When you see a list of the components of air, they refer to DRY air, because the amount of water vapor varies. If the relative humidity is 100% and the temperature is 104F, water vapor would make up 7% of that air. I doubt the dew point has ever hit 104F, so almost certainly it's never been that high and is usually a good bit less. When temperatures drop well into the double digits below 0, there is only a barely-detectable amount of water vapor. So those component lists floating around describes dry air, or the make-up of the air that isn't water vapor. Those numbers are fairly constant whereas if you tried to include water vapor, you couldn't come up with hard numbers because they are all displaced by any water vapor in proportion to how much of the dry air they make up.
Mist comprises airborne droplets of water. Dew comprises droplets of water attached to some solid structure (eg a blade of grass or a spider's web). The source of water in both circumstances is water vapour contained in the air which comes out of the air when it cools past its 'dew point'.
The warmer the temperature, the more water vapor in the air. The colder the temperature, the less water vapor in the air.
If air is holding as much moisture as it can, colder air holds less than warmer.
Warmer air has higher saturation mixing ratios then cold air does. So therefore because of this 100% humidity in cold air is not 100% humidity in warmer air. The warmer the temperature, the more water vapor in the air. The colder the temperature, the less water vapor in the air.
colder air doesn't collect as much water vapor
no, warm air holds more water vapour than cold air
The warmer the water the less oxygen it holds.
warm air hold more water vapor...unless it doesnt like sandwiches between its toes at 5 o'clock in the after noon
As the air cools, it can contain less and less water vapor as a gas. So the vapor condenses and creates visible mist called fog, clouds, drizzle, and rain depending on where the water vapor condenses and how much of it condenses. The rain and drizzle forms as the mist groups together and creates the droplets and drops.
Because the water molecules which are far inside the liquid experience an outward force, and has no maximum potential energy.
No, cold air can't hold as much as warm air, that's why clouds are up in the sky.
When the temperature drops the less water vapor in the air
When the temperature drops the less water vapor in the air