adiabatic lapse rate sentence in Hindi
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- The moist adiabatic lapse rate varies strongly with temperature.
- Note that adiabatic lapse rate redirects to the lapse rate article you linked.
- Above that altitude, the adiabatic lapse rate decreases to the moist adiabatic lapse rate as the air continues to rise.
- Above that altitude, the adiabatic lapse rate decreases to the moist adiabatic lapse rate as the air continues to rise.
- As the air descends on the leeward side, it is warmed by adiabatic compression at the dry adiabatic lapse rate.
- Instability results from difference between the adiabatic lapse rate of an air mass and the ambient lapse rate in the atmosphere.
- The lapse rate, dry adiabatic lapse rate ( DALR ) and moist adiabatic lapse rate ( MALR ), are obtained.
- The lapse rate, dry adiabatic lapse rate ( DALR ) and moist adiabatic lapse rate ( MALR ), are obtained.
- A rise from sea level into the upper regions of the atmosphere causes the temperature to decrease ( see adiabatic lapse rate ).
- The adiabatic lapse rate is the rate at which a rising or falling air mass lowers or increases per distance of vertical displacement.
- The difference between the dry adiabatic lapse rate and the rate at which the dew point drops is around per 1, 000 m.
- The dry adiabatic lapse rate ( for unsaturated air ) is 3 �C ( 5.4 �F ) per 1, 000 vertical feet.
- Meteorologists use radiosondes to measure the environmental lapse rate and compare it to the predicted adiabatic lapse rate to forecast the likelihood that air will rise.
- The temperature decreases with the dry adiabatic lapse rate, until it hits the dew point, where water vapor in the air begins to condense.
- As a result of the latent heat that is released during water vapor condensation, moist air has a relatively lower adiabatic lapse rate than dry air.
- The moist adiabatic lapse rate varies from 1.1 �C to 2.8 �C ( 2 �F to 5 �F ) per 1, 000 vertical feet.
- From there on, follow the moist adiabatic lapse rate until the temperature of the parcel reaches the air mass temperature, at the equilibrium level ( EL ).
- This decrease is constant for Earth's atmosphere, and is approximately per kilometer ( 0.62 miles ); this is known as the dry adiabatic lapse rate.
- If the environmental lapse rate is less than the moist adiabatic lapse rate, the air is absolutely stable rising air will cool faster than the surrounding air and lose buoyancy.
- The difference in moist adiabatic lapse rate and the dry rate is the cause of foehn wind phenomenon ( also known as " Chinook winds " in parts of North America ).
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