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An air parcel at 28 degrees Celsius at sea level with a lifting condensation level of 1500m calculate its temperature at 1000m use a DAR of 10 degrees Celsius per 1000m and a WAR of 5 degrees Celsius per 1000m

Sagot :

Final temeprature at 1000m is  18  °C.

According to the dry adiabatic lapse rate of 9.8°C/km t,he air parcel would cool by 4.9°C to about 15° C. However, the temperature at 1 km is not 15°C but 10°C.

Air parcel at sea level =  28 degrees Celsius.

Lifting condensation level of 1500m

1000m use a DAR of 10 degrees

WAR of 5 degrees Celsius per 1000m

Fall in temperature at 1500 °C = 15 °C

Rise in tempereture = 5  °C

Overall 10  °C fall

Final temperature = 28  °C - 10  °C

                               = 18  °C answers.

For this precise scenario, 2000 meters is the altitude at which condensation takes area. that is called the lifting condensation stage. Please notice the difference between the dew factor and lifting condensation degree. Dew factor is a temperature and is given in degrees C or F, at the same time as the lifting condensation stage is an altitude and is given in meters or toes.

The temperature could be sixteen stages C. The air rose up a thousand meters, so it cooled off by 10 levels C. in case you said that the air temperature could be 36 stages C, you made a common mistake.

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