Temperature, pressure, and water availability. For example, if you decrease temperature, the air cannot hold as much water vapor, this is the main cause of dew in the morning. If you add a large supply of water, like a lake, into a desert region the air can act like a sponge.
The amount of water vapor in the atmosphere varies from place to place. Humidity is the term used to describe the amount of water vapor in the atmosphere.
Relative humidity the exact amount of water vapor in the atmosphere (specific humidity)
Humidity
Geathen rocks
The amount of water vapor per cubic meter in the atmosphere as sea level is 30g/m3.
the shape and height causes it to vary with temperature,pressure,and the amount of water vapor in the atmosphere
The amount of water vapor in the atmosphere varies from place to place. Humidity is the term used to describe the amount of water vapor in the atmosphere.
Relative humidity the exact amount of water vapor in the atmosphere (specific humidity)
Geathen rocks
Humidity
Water vapors makes up only a few percent of the mass of the atmosphere. However, this small amount of water vapor has in oceans and water bodies changes to a gas, water vapor. The mount of water vapor in the air is called humidity
The amount of water vapor per cubic meter in the atmosphere as sea level is 30g/m3.
No, global warming results from humans increasing the amounts of carbon dioxide in the atmosphere. There is a certain amount of water vapor in the atmosphere that remains fairly constant and is part of the natural water cycle. In other words, human actions can not increase the water vapor in the atmosphere.
The cool atmosphere condenses the rising water vapor and causes it to fall back to Earth
barometer/hygrometer/thermometer
The main processes that return water vapor to the atmosphere are evaporation and transpiration. Evaporation occurs when liquid water changes into water vapor from sources such as oceans, lakes, and rivers. Transpiration is the process through which plants release water vapor from their leaves into the atmosphere. Both of these processes contribute to the water cycle by replenishing the atmosphere with water vapor.
water vapor