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2. Consider the same air mass in question 1 and the following additional conditions including a saturated adiabatic lapse (SALR) rate of 6°C/1000m and a specific humidity of 7.6g/kg for rising air parcel on the windward side. 5000 4000 3000 bimu 2000 1000 30°C Sea level With the given specific humidity for the air parcel, what would be the dew point temperature of this air parcel? i. Complete the following table by determining the temperature on the windward and leeward sides of the above mountain range. Remember that if the air mass reaches dew- point at some altitude, adiabatic cooling rate will switch to SALR. ii. Altitude (Windward Side) (m) Temperature (°C) Altitude (Windward Side) (m) Temperature (°C) 1000 4000 2000 3000 2000 3000 1000 4000 0 (sea level) Elevation (m)

2. Consider the same air mass in question 1 and the following additional conditions including a saturated adiabatic lapse (SALR) rate of 6°C/1000m and a specific humidity of 7.6g/kg for rising air parcel on the windward side. 5000 4000 3000 bimu 2000 1000 30°C Sea level With the given specific humidity for the air parcel, what would be the dew point temperature of this air parcel? i. Complete the following table by determining the temperature on the windward and leeward sides of the above mountain range. Remember that if the air mass reaches dew- point at some altitude, adiabatic cooling rate will switch to SALR. ii. Altitude (Windward Side) (m) Temperature (°C) Altitude (Windward Side) (m) Temperature (°C) 1000 4000 2000 3000 2000 3000 1000 4000 0 (sea level) Elevation (m)

Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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ESC205: Principles of Meteorology gofoosMto Spring 2021 50 45 40 35 30 Irin 25 20 15 10 talomoA 0. 40 60 us80A GO 100 s 120 Temperature (°F) Saturation specifichumidity (g/kg) 5. water capacity 20
Transcribed Image Text:ESC205: Principles of Meteorology gofoosMto Spring 2021 50 45 40 35 30 Irin 25 20 15 10 talomoA 0. 40 60 us80A GO 100 s 120 Temperature (°F) Saturation specifichumidity (g/kg) 5. water capacity 20
ESC205: Principles of Meteorology 2. Consider the same air mass in question 1 and the following additional conditions including a saturated adiabatic lapse (SALR) rate of 6°C/1000m and a specific humidity of 7.6g/kg for rising air parcel on the windward side. 5000 4000 smut svitetsn o vo 3000 b diblmu 2000 30°C 1000 Sea level i. With the given specific humidity for the air parcel, what would be the dew point temperature of this air parcel? Complete the following table by determining the temperature on the windward and leeward sides of the above mountain range. Remember that if the air mass reaches dew- point at some altitude, adiabatic cooling rate will switch to SALR. i. Altitude (Windward Side) (m) Temperature (°C) Altitude (Windward Side) (m) Temperature (°C) 1000 4000 2000 3000 2000 3000 1000 4000 0 (sea level) Elevation (m)
Transcribed Image Text:ESC205: Principles of Meteorology 2. Consider the same air mass in question 1 and the following additional conditions including a saturated adiabatic lapse (SALR) rate of 6°C/1000m and a specific humidity of 7.6g/kg for rising air parcel on the windward side. 5000 4000 smut svitetsn o vo 3000 b diblmu 2000 30°C 1000 Sea level i. With the given specific humidity for the air parcel, what would be the dew point temperature of this air parcel? Complete the following table by determining the temperature on the windward and leeward sides of the above mountain range. Remember that if the air mass reaches dew- point at some altitude, adiabatic cooling rate will switch to SALR. i. Altitude (Windward Side) (m) Temperature (°C) Altitude (Windward Side) (m) Temperature (°C) 1000 4000 2000 3000 2000 3000 1000 4000 0 (sea level) Elevation (m)
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