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Moist air contains large amounts of water vapor. Water vapor carries large amounts of energy. This energy is what powers a thunderstorm that might produce a tornado
Water vapor enters the air as water at the surface evaporates or as plants transpire water vapor from their leaves.
The water vapor in the air. Since the cup is so cold from the ice inside, the vapor in the air when it hits the cup it causes it to make the water on the outsaide of the cup. You'd think it came from the inside, but it doesn't.
As air rises it becomes decompressed, which causes it to cool. This cooling can cause water vapor to condense, forming clouds.
water vapor
Yes. The cool glass causes water vapor in the air to condense.
No, absolute humidity is the exact amount of water vapor in the atmosphere. So, if the water vapor in the air remains unchanged, so does the absolute humidity.
Water vapor in the air....
yes because the more hot air the more water vapor
colder air doesn't collect as much water vapor
the temp changes
There is more water vapor present in the air when it is warmer because it is hotter and it causes more evaporating to occur and the liquid is turning into a gas.
Condensation of water vapor causes dew.
Add water (vapor) ... evaporation. Lower the temperature of the air mass.
Water vapor in the air is water in the form of a gas.
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.
Condensation commonly occurs when a vapor is cooled. Water vapor from air which naturally condenses on cold surfaces into liquid water is called dew. Water vapor will only condense onto another surface when that surface is cooler than the temperature of the water vapor, or when the water vapor equilibrium in air, i. e. saturation humidity, has been exceeded. When water vapor condenses onto a surface, a net warming occurs on that surface.