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Water vapor in the cool air condenses in to tiny droplets of water, forming clouds.
When the water vapour condenses and turns into a liquid.
It rises into the air and condenses to become clouds.
Cooler. The cloud forms because the water vapor condenses by cooling down. Thunderstorms occur because a warm, moist air mass is cooled by an incoming cold air mass. When the moist air gets chilled, the water vapor condenses to form clouds, resulting in rain.
It rains, or maybe hail storm or a snowstorm.
the dew point
Water vapor in the cool air condenses in to tiny droplets of water, forming clouds.
Condensation commonly occurs when a vapor is cooled. Water vapor from air which naturally condenses on cold surfaces into liquid water is called dew. Water vapor will only condense onto another surface when that surface is cooler than the temperature of the water vapor, or when the water vapor equilibrium in air, i. e. saturation humidity, has been exceeded. When water vapor condenses onto a surface, a net warming occurs on that surface.
The moisture comes from the water vapor in the air. As the temperature drops to near the dew point, the water vapor condenses on cold surfaces in the desert.
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.
Water can't condense. Condensation is about something turning from a gas to a liquid. Once it has become a liquid it can't be come liquid-er.
Water vapor and air. Water vapor condenses to produce clouds. Even if air has no visible clouds it still has water vapor.
It condenses
evaporation
it condenses
In nature, air is known to contain water vapor in itself. When the water vapor condenses, or turns into liquid water, there is a very high chance of precipitation. The dew point temperature is the temperature at which the water vapor in air condenses into a liquid. When air is at the dew point temperature, a cloud begins to form. Relative humidity is a long term that simply means is how full of water is air. Air can only hold so much water vapor, and when air is full of it, it is "saturated." When there is no water vapor in the air, there is 0% humidity. When air is full of water vapor and can't hold anymore, there is 100% humidity.
It condenses and becomes liquid water.