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(Solved): An air parcel with a surface temperature of 16C (@ 0 m) is forced to rise to over a 3800-m mo ...







  1. An air parcel with a surface temperature of 16°C (@ 0 m) is forced to rise to over a 3800-m mountain. The LCL is located at 1800 m. Given the DALR of 10°C/1000m and a MALR of 6.4°C/1000m, calculate the dew point temperature and the air parcel’s temperature at the peak.
  2. If all condensed moisture fell out as precipitation on the windward side of the mountain, what is the temperature be at 0 m on the lee side?
7) An air parcel with a surface temperature of 16°C (@0 m) is forced to rise to over a 3800-m mountain. The
LCL is located at
7) An air parcel with a surface temperature of 16°C (@0 m) is forced to rise to over a 3800-m mountain. The LCL is located at 1800 m. Given the DALR of 10°C/1000m and a MALR of 6.4°C/1000m, calculate the dew point temperature and the air parcel's temperature at the peak. If all condensed moisture fell out as precipitationon the windward side of the mountain, what is the temperature be at 0 m on the lee side? Show answers to 1 dp. Show all your work and units. NOTE: It may be useful to draw a diagram of the mountain and label it with the details to help visualize the question. [3] Dew point temperature_ Temperature at peak Lee-side temperature at 0 m Why is the parcel warmer on the lee side at Om than on the windward? [1]


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Given data: Temperature of air parcel at surface(@ 0m) = 16°C LCL(lifting condensation level) is located at = 1800 m DALR = 10°C/1000m MALR = 6.4°C/1000m ***** Dew point temperature = Initial temperature - (
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