Temperature is the main variant of air's ability to hold moisture. The warmer the air the more water it can hold without condensation.
Temperature
As the air gets warmer, it's ability to hold water vapor increases.
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 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 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.
Air is the mixture of different gases (like oxigen, nitrogen, co2 e.t.c.) & water vapour. Gases are only gases, here is no water vapour. And water vapour is form after the vapourization of water at high temperature.
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 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.
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.
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.