Water vapor in the air is visible in the form of mist, fog, and clouds.
At the Chemical Convention known as STP, or Standard Temperature and Pressure, 20 kg of Air contains more water vapor.
This could be steam if you are heating water. Or fog when warm air crosses cooler ground or cool air crosses warmer ground.steam
The process is known as evaporation, where water becomes a vapor and rises into the sky.
This is known as the "humidity" of the air. Warmer air can hold more water than colder air.The percentage of water vapor in the air, compared to the maximum amount possible at that temperature, is called the relative humidity.Air that contains 100% of the possible water vapor is said to be saturated. In some cases, more water is added to the air, causing it to become supersaturated (relative humidity over 100%).
it vapor when the weather is wet and if your driving you can see it on your windshield
humidity
Water vapor in the air is water in the form of a gas.
At the Chemical Convention known as STP, or Standard Temperature and Pressure, 20 kg of Air contains more water vapor.
This could be steam if you are heating water. Or fog when warm air crosses cooler ground or cool air crosses warmer ground.steam
The process is known as evaporation, where water becomes a vapor and rises into the sky.
Water vapor enters the air as water at the surface evaporates or as plants transpire water vapor from their leaves.
Clouds form when the invisible water vapor in the air condenses into visible water droplets or ice crystals. There is water around us all the time in the form of tiny gas particles, also known as water vapor. There are also tiny particles floating around in the air - such as salt and dust - these are called aerosols.
Condensation nucleus is also known as an aerosol. Basically, condensation nucleus is a form of pollution that is essential to creating clouds. As water vapor goes up into the air, the condensation nucleus becomes the support for the water vapor to condense on.
This is known as the "humidity" of the air. Warmer air can hold more water than colder air.The percentage of water vapor in the air, compared to the maximum amount possible at that temperature, is called the relative humidity.Air that contains 100% of the possible water vapor is said to be saturated. In some cases, more water is added to the air, causing it to become supersaturated (relative humidity over 100%).
This is called the absolute humidity, usually expressed in grams of water vapor per kilogram of air, but also by water vapor per unit volume of air (e.g. grams per cubic meter).
it vapor when the weather is wet and if your driving you can see it on your windshield
The warmer the temperature, the more water vapor in the air. The colder the temperature, the less water vapor in the air.