The dew point is a measure of the amount of water vapor in the atmosphere. As the temperature gets closer to the dew point, the humidity rises. When the temperature finally drops to the dew point (100% humidity), the the atmosphere is completely saturated with water, and it will start to rain (or snow, if the dew point is below freezing). Since the atmosphere is completely saturated when the temperature is at the dew point, it cannot go below the dew point.
No. Because the Dew Point always depends on the temperature. As the temperature changes so does the dew point.
because it goes by the temperature
Dew point is not always the same. It changes throughout the course of the day.
Dew Point: Is the temperature at which gas condenses into a liquid.
Dew point is the temperature at which the water vapor in the air condenses, then evaporates. The barometric or air pressure is independent from the dew point.
Because the other liquids think dew point stinks.
nothing
Dew point is not always the same. It changes throughout the course of the day.
Dew point is not always the same. It changes throughout the course of the day.
No. (It has a very wide range.)
They are the same.
there is no dew point of a hurricane
the realationship between condensation and dew point is that condensation occurs when it reaches the dew point.
The approximate dew point at sea level is dependent on more than just the sea level itself. Calculating dew point requires the air temperature as well as relative humidity. So in a general sense, there is no difference in dew point based on elevation if the temperature is the same.
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.
Dew point is the point when condensation forms
i think dew point.
The temperature to which air must be cooled to reach saturation is called the dew point.
They are the same.