The concentration of water vapor in the atmosphere decreases as altitude increases. Most planes fly near the tropopause since there's less water vapor and, therefore, weather there.
Increases. Warmer air can hold more water vapor before reaching saturation, so as the temperature rises, the air can accommodate a larger amount of water vapor before becoming saturated. This is due to the higher vapor pressure in warmer air.
Increases
Because air is cooler at higher altitudes in the troposphere, water vapor cools as it rises high in the atmosphere and transforms into water droplets by a process called condensation. The water droplets that form make up clouds.
When water vapor rises and cools, it reaches a temperature called the dew point. At this point, the water vapor condenses back into liquid water, forming clouds or fog. If the cooling continues, the condensed water droplets may grow and eventually fall as precipitation.
Yes, at which point it takes the form of precipitation and returns to the earth as rain, snow, sleet, or hail.
it condenses
it will precipitate
It becomes condensation.The water vapor turns into a liquid
It condenses into liquid.
As water vapor cools to the dew point it converts from a gas back to a liquid.
turns into hail or snow.
When the sun rises, the warmth and light cause the dew to evaporate. As the temperature rises, the water droplets in the dew transform into water vapor and are released into the air.
it explodes man
When water vapor is evaporation outside it rises to the sky and goes through the water cycle.
Water vapor
Increases. Warmer air can hold more water vapor before reaching saturation, so as the temperature rises, the air can accommodate a larger amount of water vapor before becoming saturated. This is due to the higher vapor pressure in warmer air.
When water vapor rises, it cools and condenses into liquid water droplets, leading to the formation of clouds. If the cooling continues, the droplets may combine to form larger droplets and eventually fall as precipitation in the form of rain, snow, hail, or sleet.