which half of the brains controls the left side of the body
Saturation causes Dew Point
The temperature to which air must be cooled to reach saturation is called the dew point.
The dew point is a saturation point, but a saturation point may not be a dew point. That is, a saturation point has a broader definition -- more general application. Sometimes you can interchange the terms without confusing the reader. =================================
it doesn't depend on the temperature but depends on how much water was evaporated
Yes, at saturation.
That's an approximate definition of saturation. And the temperature at which the current amount of water vapor in the air would be the saturation point is called the dew point. The dew point is a measure of absolute humidity.
It is the Dew point.
The Dew Point.
Intersection of SHR line and saturation line on the Psych Chart
Dew points are related to storms because the higher the dew point, the more likely it is that storms will develop. Dew points 70 and over indicate a better chance for storms.
Dew Point and Temperature 1) The air needs to be cooled to its dew point. 2) The air needs to have reached saturation, which can be achieved through many ways.
Condensation occurs in the atmosphere as part of the phases in rain cycle. During the condensation phase, water vapor transforms into liquid form. When warm air rises into the atmosphere, it cools down and loses its ability to hold water vapor resulting to the condensation of water forming cloud droplets.
The dew point is the temperature at which a given parcel of humid air must be cooled, at constant barometric pressure, for water vapor to condense into water. The condensed water is called dew. The dew point is a saturation temperature.The dew point is associated with relative humidity. A high relative-humidity indicates that the dew point is closer to the current air temperature. Relative humidity of 100% indicates the dew point is equal to the current temperature and the air is maximally saturated with water. When the dew point remains constant and temperature increases, relative humidity will decreaseTherefore, by the above stated reasons (of humidity and barometric pressure and saturation based on temperature) are all reasons the point at wick dew forms is not the same because the regions them selves vary and thus these relative factors maybe dissimilar.