When there is too much water vapor in the air, it can lead to increased humidity levels, which can make the environment feel warmer and more uncomfortable. High humidity can also contribute to the formation of clouds and precipitation, potentially resulting in heavy rainfall or storms. Additionally, excess moisture can promote the growth of mold and mildew, affecting indoor air quality and health.
Water does NOT condense into the air. Water EVAPORATES into the air. When air cools sufficiently, then water vapour will condense out of the air as, mist, fog, rain, hail, snow. etc.,
Water vapour is a constituents in air because water vapour rises in the atmosphere & is always present in the atmospere in some or the other quantity.Also 0.0001% of air consist water vapour
hurrycan
Hot air full of water vapour.
Water that evaporates will rise and form clouds of water vapour.
it becomes water vapour in the air
Water does NOT condense into the air. Water EVAPORATES into the air. When air cools sufficiently, then water vapour will condense out of the air as, mist, fog, rain, hail, snow. etc.,
Relative humidity compares the amount of water vapour present in the air with the amount of water vapour that would be present in the same air at saturation. Specific humidity is the mass of water vapour present per kg of total air.
Air has only a limited capacity to carry water vapour, this capacity diminishes as the air gets colder. When this happens, the water vapour will condense out, at first as a fine mist.
It is because water vapour is air so it can't be seen but when we breath out in the mirror,water vapour is found.
It cools and consequently can hold less water vapour. The vapour condenses and it rains. This is convection rainfall.
It cools and consequently can hold less water vapour. The vapour condenses and it rains. This is convection rainfall.
Water vapour evaporates due to heat and goes into the clouds. Then when the clouds cool the water vapour condenses and falls as rain <== I think :S
Relative Humidity is the measure of water vapour in air. It is the ratio of the actual water vapour in air divided by the maximum amount the water the air can hold at the existing temperature and pressure. It tells how fast or slow the water on the body or in clothes will evaporate or in otherwords is the air dry or humid. Absolute measure of water vapour in air is called specific humidity. It can be measured as ratio of mass of water and mass of dry air.
both are measures of how much water vapour is in the air
When you breath out, you breath out some water vapour. This is normally invisible, but cold air cannot hold as much water vapour compared with warm. This causes some of the water vapour to condense in mid air in front of you, forming 'the cloud'!
The air that you exhale contains water vapour. When you exhale during a cold day, the relative humidity increases. Relative humidity is actually the percentage of the amount of water vapour in the air.(the maximum amount of water vapour that the air can hold at that temperature) The colder the air, the less water vapour it can carry. When exhaled, air mixes with cold air, the temperature of the exhaled air drops, but there is more water vapour. When the air becomes saturated, (relative humidity is 100%), the extra water vapour will condense, allowing you to see your breathe on cold days.