posted by nissa on .
assume that a parcel of air is forced to rise up and over a 6000 foot high mountain. The intial temperature of the parcel at sea level is 76.5 F, and the lifting condensation level (lvl) of the parcel is 3000 feet. The DAR is 5.5 F/1000 and the SAR is 3.3 F/1000. Assume that conscends. Indicate calculated temperatures to one decimal place.
1. Calculate the temperature of the parcel at the following elevations as it rises up the windward side of the mountain:
(a)1000__________F (b)3000_____F (c) 6000 F___________
2. After the parcel of air has descended down the lee side of the mountain to sea level, what is the temperature of the parcel?
Why is the parcel now warmer than it was at sea level on the windward side (what is the source of the heat energy)?
On the windward side of the mountain, is the relative humidity of the parcel increasing or decreasing as it rises from sea level to 3000 feet?
On the lee side of the mountain, is the relative humidity of the parcel increasing or decreasing as it descends from 6000 feet to sea level?