when the temperature reaches the dew point.
when the temperature reaches the dew point.
When the tempreture reaches the dew point.
when the temperature reaches the dew point.
The water vapor will condense and with sufficient particle matter it will form clouds and possibly precipitation.
A cold front occurs when a cool air mass pushes into a warmer one. Since cool air is denser than warm air, the warm air mass gets forced up and over the cooler one. As the air rises it cools, causing moisture in it to condense into clouds and rain.
Warm air is less dense than cool air. The moisture has an interesting role to play. As a mass of air rises, it cools, but the surrounding air generally cools with altitude as well. When the rising air is moist, the moisture can eventually condense to form clouds. The condensation releases heat, which slows the rate at which the air cools. If there is enough moisture present and the surrounding air cools quickly enough, this extra heat allows the rising air mass to remain warmer than its surroundings and continue to rise. It is through this process that the towering clouds of thunderstorms form.
What happens is similar to when a warm air mass meets a cold air mass: the Cold Air Mass is forced to Subside beneath the Warm Air Mass. Thusly the warm air is uplifted, it cools and Rain is formed. When a Warm Air Mass meets a Cold Air Mass, the warm air is [again] forced to Rise above the Cold Air Mass, it cools and Rain is formed.
when the temperature reaches the dew point.
when the temperature reaches the dew point.
Water does NOT condense into the air. Water EVAPORATES into the air. When air cools sufficiently, then water vapour will condense out of the air as, mist, fog, rain, hail, snow. etc.,
The water vapor will condense and with sufficient particle matter it will form clouds and possibly precipitation.
because water molecules attach to dust particle. when tiny mass of water has formed on a dust particle, other molecules will join the liquid mass.
When AIR RISE THERE IS DECREASE IN PRESSURE WITH ELEVATION AT TEMPRATURE REMAIN SAME OF ATMOSPHERE UPTO 11 KM AND THE PARCEL OF AIR IS EXPAND AND IN TURN THE AIR CONDENSE TO FORM PRECIPITATION.
It condenses and it becomes liquid
water vapor
When a mass of warm saturated air cools down the water vapor in the air is precipitated out causing either rain, snow or maybe fog
When air rises it decompresses and cools. The cooling can cause moisture in the air to condense.
It cools, and may loose its water content.
Typically, yes. As air rises it cools, which can cause moisture in it to condense.