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Clouds form as air cools to its dew point, condensation nuclei like pollen and dust play a vital role. Learn about factors influencing cloud formation, from dry adiabatic lapse rate to dew point lapse rate. Discover different cloud types and their characteristics.
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How do Clouds Form? • They form when air above the ground cools to its dew point. • There must be condensation nuclei present. • Examples of Nuclei: Pollen, Dust, Smoke, Volcanic Ash, Salt
Cloud Formation… • As the air rises due to convection, it cools at a rate of 10 degree Celsius for every 1 km in elevation. This rate of cooling is called the dry adiabatic lapse rate. • The cooling is caused only by the air expanding. • When the temperature of the rising air reaches the dew point, the humidity is then 100%, and condensation begins onto a nuclei.
Dew Point Lapse Rate • As the air rises the dew point also decreases but at a rate of 2 degrees Celsius per 1 km. This rate is called the Dew Point Lapse Rate. • Once the Dry Adiabatic Lapse rate and Dew Point Lapse rate are the same, condensation occurs. • Condensation needs a surface to stick to.
Cloud Formation… • As the water condenses onto nuclei, it releases heat (exothermic), and the lapse rate changes to 6 degrees Celsius per 1 Km. • The is called the moist-adiabatic lapse rate • The base of the cloud is known as the condensation level (temp. = dew point).
Types of Cloud… • The type of cloud depends on how the air is moving. • If the air is moving horizontal, the clouds form in layers called stratiform clouds. • If the air movement is vertical, the clouds grow upwards, called cumuliform clouds.
Cirrus Clouds • Cirrus clouds are thin, feathery, and are made of ice crystals. • Average cloud height is 7000-13000 m.
Stratus Clouds • Stratus clouds are very low in altitude. • Alto status = 2,000 – 7,000 m • Stratus = 500 – 2,000 m
Cumulus Clouds • Cumulus clouds are formed by vertically rising air currents. They are thick, puffy, and massive.