more air
When the air is saturated, it means it is holding the maximum amount of water vapor it can at a given temperature. Further evaporation or addition of water vapor will lead to condensation or precipitation.
Air can hold a certain amount of moisture (water vapor) in the mixture of nitrogen, oxygen and other gases. The amount goes up with the temperature. If air is holding as much moisture as possible at a given temperature, it is said to be saturated, and it probably will start precipitating if the temperature drops at all. it is kind of like a saturated solution in which the excess solute will precipitate as solid particles when the solution is cooled. So to dumb it down, it means that no more water can be evaporated in to the air.
The air is saturated, and has reached its dew point temperature.The dew point.
Air that has reached its water vapor capacity is considered saturated. This means that the air cannot hold any more water vapor at its current temperature and pressure, leading to condensation or precipitation.
Warm saturated air can lead to the formation of clouds and precipitation, which can result in rainy or stormy weather patterns. This is because warm air can hold more moisture, and when it becomes saturated, the excess moisture condenses to form clouds and eventually precipitation.
more air
Saturated air is air that has all the water vapor that it can hold.
when it holds all the water vapor it can hold
8c because the warmer the air, the more water it can hold
SATURATED
When the air is saturated, it means it is holding the maximum amount of water vapor it can at a given temperature. Further evaporation or addition of water vapor will lead to condensation or precipitation.
… any more water vapour.
Air can hold a certain amount of moisture (water vapor) in the mixture of nitrogen, oxygen and other gases. The amount goes up with the temperature. If air is holding as much moisture as possible at a given temperature, it is said to be saturated, and it probably will start precipitating if the temperature drops at all. it is kind of like a saturated solution in which the excess solute will precipitate as solid particles when the solution is cooled. So to dumb it down, it means that no more water can be evaporated in to the air.
The air is saturated, and has reached its dew point temperature.The dew point.
A comparison between the actual amount of water vapor in the air and the amount it could hold if saturated is called relative humidity. It is expressed as a percentage, indicating how close the air is to being fully saturated with moisture. For example, a relative humidity of 50% means the air contains half the amount of water vapor it can hold at that temperature.
The temperature at which air becomes saturated is called the dew point. At the dew point, the air can no longer hold all of its moisture in vapor form and begins to condense into liquid water.
If the air is already saturated with water vapor and the temperature increases, the air can hold more moisture. This may result in the relative humidity decreasing because the air is not as saturated as before. If the temperature increase continues, the air may eventually reach a new saturation point at the higher temperature.