A rise in temperature allows the air to absorb more water vapour.
it occurs as rain,fog,or mist
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.
The maximum amount of water vapor that can exist in the air largely depends on temperature. Hotter days mean an increased ability to hold water vapor while colder days have decreased humidity. When relative humidity is at 100%, fog generally forms.
Water vapor in the air compared to the amount of water vapor that air could hold at a given temperature.
Relative humidity
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.
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.
decrease in the temperatue
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.
it rains.
Temperature is the main variant of air's ability to hold moisture. The warmer the air the more water it can hold without condensation.
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.
No. It increases. Warmer air can hold more water than colder air.