The warmer the temperature, the more water vapor in the air. The colder the temperature, the less water vapor in the air.
Water vapor accounts for the majority of the "green house effect" for the atmosphere - accounting for about 95% of Earth's greenhouse effect. The impact is probably most notable when comparing daytime and night-time temperatures for desert areas (with low atmospheric water vapor levels) and very humid areas - such as near rivers, lakes and oceans (which have high atmospheric water vapor levels.) In Death Valley night temperatures will be about 20-30 degrees cooler than in the daytime. Monterey, CA, which is about 300 miles due west only has temperature swings half that size. At higher altitudes, the air is less dense and can hold less water vapor. That is one reason higher altitudes tend to be colder and have bigger temperature swings than lower altitudes. There is also the fairly obvious effect that when there is more water vapor, clouds are more likely to form, which keeps things cooler during the day and holds in more warmth at night after the sun goes down.
Water vapor in the air compared to the amount of water vapor that air could hold at a given temperature.
The warmer the temperature, the more water vapor in the air. The colder the temperature, the less water vapor in the air.
Relative humidity is directly related to the amount of water vapor in air, and that's the relationship. The more water vapor that is in the air, the higher the relative humidity at a given temperature.
Relative humidity
Relative humidity.
Relative humidity.
Relative humidity.
The amount of water vapor in the atmosphere affects the formation of clouds in the atmosphere, which affects the precipitation in the atmosphere. The amount of solar heating in the atmosphere affects the temperature of the surface and the amount of water evaporation, and also determines the extent to which the humidity is convected into the atmosphere. Differences in humidity cause drought or precipitation, depending on how it is added or lost. Differences in heating are what drive the major pressure systems, which interact to form winds, clouds, and storms.
The amount of water vapor in air varies based on the temperature and density of air. The amount of water vapor ranges from a trace amount up to 4%.
atmospheric presures
By using the sun rays to calibrate the amount of water if the temperature affects the water cycle then it affects the whole world.
the amount of water vapor depends in volume temperature and pressure.Since you can never keep any of them constant forever, then the amount of water vapor would have to change to "balance" out the system (the conservation of energy or stuff like that). This could be done by precipitation or condensation, both of which help to regulate the right amount of water vapor.