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Temperature
As the air gets warmer, it's ability to hold water vapor increases.
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.
When temperature is increased the amount of molecules evaporated is increasef and as a consequence condensation is also increased so vapour pressure increases.
Yes, vapor water does contribute to the global increase in temperature. Water vapor is a greenhouse gas, meaning it can trap heat in the Earth's atmosphere. As the Earth's temperature rises, more water evaporates and enters the atmosphere, creating a positive feedback loop that amplifies the warming effect.
Temperature
INCREASES the solubility of SOLIDS and LIQUIDS... and DECREASES the solubility of GASES.
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.
Vapor pressure increases as temperatures increase because water will evaporate in hot weather. This evaporation rises increasing the vapor pressure. This is why many areas have high humidity in the summer.
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.
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.
A rise in temperature allows the air to absorb more water vapour.
By carrying away moisture the wind allows air with a greater ability to absorb evaporation and so increased evaporation will occur (until equilibrium in vapor pressure is reached).