As the temperature of the air increases, water gets evaporated and hence the water content (humidity) decreases.
As temperature reduces the temperature of the water vapour also reduces and it cannot maintain it's gaseous form so undergoes a phase transition to a liquid, or even straight to ice, which happens more readily at cold surfaces ('frost). The temperature is called the 'dew point'.
At a microscopic level the process is rather more complex than that, quite interesting and counter intuitive.
As the air gets warmer, it's ability to hold water vapor increases.
The capacity of air to hold water vapor increases with a temperature increase of the air.
no, air doesn't have a water holding capacity. A common belief is that it is temperature dependent, however temperature only changes the speed at which water evaporates/condensates.
Increasing the temperature the evaporation is more important.
The humidity decreases. Plain and simple!
increase
Temperature
As the air gets warmer, it's ability to hold water vapor increases.
Temperature is the main variant of air's ability to hold moisture. The warmer the air the more water it can hold without condensation.
Air can hold a certain amount of water vapour. The amount it can hold depends on the air temperature - the hotter it is, the more water it can hold. A way to think of it is that water Can dissolve in air, just like some gases and solids can dissolve in water.
As air temperature drops, it is able to hold less water. If the air temperature continues to drop after the relative humidity reaches 100%, dew forms (or frost, if it's cold enough).
Temperature
As the air gets warmer, it's ability to hold water vapor increases.
As the air gets warmer, it's ability to hold water vapor increases.
As the air gets warmer, it's ability to hold water vapor increases.
Temperature is the main variant of air's ability to hold moisture. The warmer the air the more water it can hold without condensation.
Heat. Hot air holds more vapor than cold air. This is why we get rain when hot air rises, cools down, and the water vapor condenses out to form rain drops. It's also why we get clouds, the vapor condenses when the air gets cold at altitude but not enough to form droplets and fall from the sky.
This is called the Airs "Relative" humidity. The more water vapor in the atmosphere the higher the relative humidity will be.
Air can hold a certain amount of water vapour. The amount it can hold depends on the air temperature - the hotter it is, the more water it can hold. A way to think of it is that water Can dissolve in air, just like some gases and solids can dissolve in water.
because they float and airs lighter because they float and airs lighter
As air temperature drops, it is able to hold less water. If the air temperature continues to drop after the relative humidity reaches 100%, dew forms (or frost, if it's cold enough).
The Airs of Palestine was created in 1816.
Country Airs was created in 1986.