If its over 50 u have reached dewpoint.
it doesn't depend on the temperature but depends on how much water was evaporated
dew point
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.
When air cools to a temperature where it can no longer hold all of its water vapor, the air has reached its dew point. This is when condensation occurs, forming clouds or fog.
The temperature at which moist air becomes saturated and forms dew is called the dew point temperature.
The dew point is reached when the air temperature cools down to the point where it can no longer hold all of its moisture, causing condensation to form. This can be observed by the formation of dew on surfaces like grass or the temperature reaching the dew point value reported by weather forecasts.
The dew point is reached when the temperature falls to the point where air becomes saturated with water vapor and can no longer hold it, causing condensation to form. At this point, the air is said to be at 100% relative humidity.
it doesn't depend on the temperature but depends on how much water was evaporated
When a parcel of air is cooled to the temperature at which it is saturated, it has reached its dew point temperature. At the dew point temperature, the air is holding the maximum amount of moisture it can hold, and any further cooling will result in the formation of water droplets or condensation.
dew point
Yes, when the dew point temperature and the air temperature coincide, the air is saturated. This is because the air has reached its maximum humidity at that temperature, leading to condensation or dew forming.
The hypothesis for a dew point experiment could be that as air temperature decreases, the dew point temperature will be reached, causing water vapor in the air to condense into liquid water droplets, forming dew.
Dew point. At this point, the air can no longer hold all of the water vapor it contains, leading to condensation and potential formation of clouds or fog.
The dew point controlled the temperature of the air.
The temperature to which air must be cooled to reach saturation is called the dew point.
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.
Dew point is the temperature at which air becomes saturated.