Condensation And Precipitation-Precipitation

Condensation is the way of transforming water vapor into liquid water, with the clearest illustration being those big, fluffy skies floating above your head. The method by which water evaporates is known as evaporation. Water vapor is water in the form of a gas. Condensation is the formation of clouds from water vapor. Precipitation is the rain that falls when a cloud is full. Condensation occurs next, which is the procedure by which water vapor is converted back into liquid water. The water then turns into precipitation, which is water that falls from the clouds as rain,snow, sleet, snow, or hail.

Condensation

When droplets in clouds merge, they become bulky enough to form raindrops that fall on your head. Even if you can’t see it, the air is full of water. Hidden water condenses into tiny liquid water droplets-clouds-higher in the sky, where it is chillier than on the ground. Whenever the cloud droplets merge to create heavier cloud drops that can no longer “float” in the surrounding atmosphere, it can begin to rain, winter, and hail. All these forms of precipitation, with the superhighway transporting water from the sky to the Earth’s surface.

Condensation is the transformation of a gas, such as water vapor, into liquid water. When humidity cools and attains saturation point, tiny droplets condensate into bigger drops of water.

Condensation Forms:

Dew: Relatively small drops of moisture are developed as a result of condensation.  Water vapor can be found at or near the ground surface.

Frost: Frost is a cooled condensation that happens when air is at a certain temperature.  The ground level is super-cooled to well below freezing temperatures.

Fog: Fog is a cloud of relatively small droplets of water that shape when water evaporates.  The vapor condenses on a core close to the earth’s crust.

Clouds: A cloud is a concentration of relatively small droplets of water that occurs as the result of condensation up in the atmosphere.

Adiabatic Cooling: When pressure moves, it moves from an area of dense air on the ground to regions of the less dense surrounding air, which is known as adiabatic cooling. As a result, the rising air has less mass above it, and the decrease in pressure enables the air to broaden and cool. Adiabatic Cooling refers to the reduction in air temperature affected by increased air expansion.

Adiabatic Warming: The temperature rise of air is induced by the compression process as it falls out of the sky to the earth’s crust. When the air begins to fall from an elevated level to the atmosphere, it falls into a province of higher density air near the earth’s crust. The compressed air is warmed as a result of the process.

Precipitation:

Precipitation is defined as rain, sleet, snow, or the sudden onset of activity. Rain is an exemplification of precipitation. Any or all of the aspects of water particles that fall from the atmosphere, whether liquid or solid (e.g., rain, hail, snow, or sleet) are precipitation exemplifications.

Precipitation Forms:

1. a) Snow: Snow is formed when water vapor is defrosted straight into a solid before even forming a liquid.
2. b) Sleet: a defrosted rain that shapes when rain droplets make contact with cooler air and defrost into ice before falling out of the sky.
3. c) Hail: Round ice lumps fall from the sky.
4. d) Rain: Droplets of water that fall from the sky. 

   Conclusion 

   We discussed Condensation and Precipitation and forms of Condensation and Precipitation and other related topics through the study material notes on Condensation and Precipitation-

    Condensation is the transformation from the vapor to the liquid phase. Precipitation is the accumulation of liquid droplets of water and ice particles that shape in the atmosphere and develop to a huge enough size to be gravitational forces settled to the Earth’s surface.