No, it is always less than one hundred percent.
The percent of water vapor saturation of the air is called relative humidity. It measures the current amount of moisture in the air compared to the maximum amount the air can hold at a given temperature. Relative humidity is expressed as a percentage and indicates how close the air is to being fully saturated with water vapor.
Water vapor is water is gas form. Humdity is the amount of water the air can hold. So, they're both water in the air.
Saturated air is more dense.
If the amount of water vapor in the air does not change, the relative humidity will remain at 80% as long as the temperature remains constant at 75°F. If the temperature changes, the relative humidity will change, as it is dependent on both temperature and the amount of water vapor in the air.
Water would not evaporate at 100 percent relative humidity because the air already holds the maximum amount of water vapor it can. This means no additional water can evaporate into the air until the humidity decreases.
If the relative humidity is 50 percent, the air is holding half of the maximum amount of water vapor it can hold at that temperature. This means the air is holding 50 percent of the water vapor it could potentially hold.
yes
A relative humidity of 25% means that the air is holding 25% of the maximum amount of water vapor it can hold at that temperature. It indicates that the air is relatively dry compared to its capacity to hold moisture.
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.
Water vapor in the air is water in the form of a gas.
Water vapors makes up only a few percent of the mass of the atmosphere. However, this small amount of water vapor has in oceans and water bodies changes to a gas, water vapor. The mount of water vapor in the air is called humidity
Water vapor falls into that range depending on weather conditions.
The amount of water vapor in air varies based on the temperature and density of air. The amount of water vapor ranges from a trace amount up to 4%.
Water vapor enters the air as water at the surface evaporates or as plants transpire water vapor from their leaves.
When water vapor is added to the air, the density of the air decreases. This is because water vapor molecules are less dense than dry air molecules.
Over a tropical ocean, yes.
If the relative humidity is at 75%, the air is not holding it's maximuim amount of water vapor. If it was holding its maxumum amount it would be 100%. The formula for that is:Actual water vapor_______________ * 100 Equals the percentTotal water vapor