Fog or clouds.
Air is able to hold a certain amount of water vapor in the atmosphere, and the amount is dependent on the temperature and pressure of the air. Higher temperature air can contain more transparent water vapor than colder air can. We calculate the "relative humidity" of the air as the ratio of how much water the air DOES contain divided by the maximum amount of water that the air could contain, for a given temperature.
When air cools, the absolute amount of water contained in the air does not change, but the air's ability to hold it decreases. So as air cools, the "relative humidity" increases. We can also calculate the temperature at which the air is at 100% relative humidity; that is to say, the air can't hold any more water. We call this temperature the "Dew Point".
When the air cools down to the "Dew Point", moisture in the air begins to condense onto cooler surfaces, and we call these droplets of water on the grass and trees "dew". If the water condenses into tiny droplets in the air, it will form fog on the ground, or clouds above the ground surface.
The cooling of water vapor in the atmosphere is known as condensation. It then comes to earth in the form of precipitation.
Gaseous
This phenomenon is called evaporation. Water molecules at the water surface gain sufficient energy to be released in the atmosphere.
water vapor
The water vapour in the atmosphere condense to form clouds. It may precipitates in the form of sleet.
Water vapor
Water is stored in the atmosphere in the form of water vapor.
because water in the atmosphere is in a form of vapor
Water vapor or the heat
Water vapor
Particles are needed because then the water vapor can condense on them
water vapors combine together in the air. They form clouds.
Its Dew Point
Water forms on windows because there is water vapor in the atmosphere, which is water in a gaseous state.
Water existing in gaseous form makes up the water found int the atmosphere and this is called Water-vapor.
condenses
condenses