Unsaturated air rises at dry adiabatic lapse rate which is
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The lapsi rate is the rate at which an atmospheric variable, normally temperature in Earth's atmosphere, change with altitude.
Explanation:
Lapse rate arises from the world lapse ,in the sense of a gradual change. It corresponds to the vertical component of the spatial gradient of temperature.
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Answer:
When the air contains little water, this lapse rate is known as the dry adiabatic lapse rate: the rate of temperature decrease is 9.8 °C/km (5.38 °F per 1,000 ft) (3.0 °C/1,000 ft). The reverse occurs for a sinking parcel of air.
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