There are a few factors that increase the ability to hold water vapor or in other words evaporation. If there is a increased amount of clouds in the air that means the air is collecting more water vapor and the water vapor forms around aerosols which are tiny dust particles that water forms around, eventually it condenses and falls back down to earth as rain or some sort of precipitation according to the atmospheric conditions.
Higher air pressure, and higher temperature will both increase the ability of the air to absorb water vapour.
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Air's ability to hold water vapor increases as temperature increases. Warmer air can hold more water vapor compared to cooler air.
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.
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.
The ratio of air's water vapor content to its capacity to hold water vapor at the same temperature is known as the relative humidity. It is expressed as a percentage and indicates how close the air is to being fully saturated with water vapor at that temperature. A relative humidity of 100% means the air is holding the maximum amount of water vapor it can at that temperature.
When the air is holding a small amount of water, it is likely to have low humidity. Low humidity means that the air has less water vapor present compared to its maximum capacity at that temperature.
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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).