Answer : X = 20°C. Y = 30°C. Z = 40°C.
Explanation : Given : Saturated adiabatic lapse rate = 5°C/km which means for every 1 km of rising or sinking air, the temperature of the parcel falls or rises by 5°C respectively. So as the parcel rises from h = 1 km to h = 2 km, it rises by 1 km and temperature falls by 5°C. So the final temperature of the air parcel at X = 25°C - 5°C = 20°C. Similarly, the dry adiabatic lapse rate is 10°C/km which means that for every 1 km of rising or sinking air, the temperature of the parcel falls or rises by 10°C respectively. So, as the parcel descends from h = 2km to h = 1km, the temperature increases by 10°C and similarly from Y to Z, the temperature increases by another 10°C .
X (h 2 km) Saturated adiabatic Dry adiabatic 25 C (h 1 km) Y (h 1...
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