Vaporisation, or evaporation.
Water vapor rises because it is less dense than the surrounding air. When water evaporates, it turns into vapor and, being lighter, it ascends into the atmosphere. Additionally, warm air tends to rise, carrying the water vapor with it as it expands. This process is a key component of the water cycle and contributes to weather patterns.
Water vapor enters the air as water at the surface evaporates or as plants transpire water vapor from their leaves.
Water vapor does not rise into the stratosphere primarily due to the temperature inversion that occurs at the boundary between the troposphere and stratosphere. In the troposphere, temperature decreases with altitude, allowing rising air to cool and condense, forming clouds. However, in the stratosphere, temperatures increase with altitude, creating a stable layer that inhibits the vertical movement of air and water vapor. Additionally, most water vapor condenses and precipitates out in the troposphere before it can reach the stratosphere.
The process by which oceans contribute to cloud formation occurs through evaporation. The sun heats up the surface of the ocean, causing water molecules to break free and rise into the atmosphere as water vapor. As the water vapor ascends, it cools and condenses into tiny water droplets, forming clouds.
Dew is the water that has condensed on a cool surface overnight from water vapor in the air.
bob the builder
It is called water vapor :)
Heat energy makes water evaporate and rise into the air as water vapor.
it is condensation
it's called humidity
Rain.
Condensation
The comparison of the actual amount of water vapor in the air to the amount of water vapor in the air if it were saturated is called relative humidity. It is expressed as a percentage and indicates how close the air is to being saturated with moisture.
The amount of water vapor in the air varies considerably depending on climate and weather. In a desert water vapor may account for a tiny fraction of a percent of the air. In a tropical rainforest during a storm water vapor may account for as much as 4% of the air.
Increasing the temperature of the air increases its capacity to hold water vapor because warmer air can accommodate more water molecules. Additionally, increasing the surface area of water exposed to air or reducing the air pressure can also enhance the air's capacity to hold water vapor.
Water vapor in the air is water in the form of a gas.
water rises into the atmosphere in the process of evaporation