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EXERCISE 16 PROBLEMS-PART IV (English Units) Answer the following questions after completing the problems in Part III. You will also need to refer to the table of Saturation Mixing Ratios in Figure 15-1; interpolate from the chart as needed. Assume that condensation begins at 100% relative humidity and that no evaporation takes place as the parcel descends. 5. 6. 7. 8. (a) (b) Section As the air rises up the windward side of the mountain (a) (b) What is the capacity (saturation mixing ratio) of the rising air at 3000 feet? What is the capacity of the air at 6000 feet? What is the capacity of the air after it has descended back down to sea level on the leeward side of the mountain? (a) On the windward side of the mountain, should the relative humidity of the parcel change as it rises from 3000 feet to 6000 feet? Why? (b) Assuming that no water vapor is added as the parcel descends down the leeward side of the mountain to sea level, is the water vapor content (the mixing ratio) of the parcel higher or lower than before it began to rise over the mountain? Why? g/kg g/kg g/kg

EXERCISE 16 PROBLEMS-PART IV (English Units) Answer the following questions after completing the problems in Part III. You will also need to refer to the table of Saturation Mixing Ratios in Figure 15-1; interpolate from the chart as needed. Assume that condensation begins at 100% relative humidity and that no evaporation takes place as the parcel descends. 5. 6. 7. 8. (a) (b) Section As the air rises up the windward side of the mountain (a) (b) What is the capacity (saturation mixing ratio) of the rising air at 3000 feet? What is the capacity of the air at 6000 feet? What is the capacity of the air after it has descended back down to sea level on the leeward side of the mountain? (a) On the windward side of the mountain, should the relative humidity of the parcel change as it rises from 3000 feet to 6000 feet? Why? (b) Assuming that no water vapor is added as the parcel descends down the leeward side of the mountain to sea level, is the water vapor content (the mixing ratio) of the parcel higher or lower than before it began to rise over the mountain? Why? g/kg g/kg g/kg

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
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ro Physical Geography Laboratory Manual Name EXERCISE 16 PROBLEMS-PART IV (English Units) at pa Answer the following questions after completing the problems in Part III. You will also need to refer to the table of Saturation Mixing Ratios in Figure 15-1; interpolate from the chart as needed. Assume that condensation begins at 100% relative humidity and that no evaporation takes place as the parcel descends. 5. 6. 7. (a) (b) (b) 1000S As the air rises up the windward side of the mountain (a) Section On the windward side of the mountain, should the relative humidity of the parcel change as it rises from 3000 feet to 6000 feet? Why? (b) (c) What is the capacity (saturation mixing ratio) of the rising air at 3000 feet? 31 es 2noltsvolo 2016 What is the capacity of the air at 6000 feet? What is the capacity of the air after it has descended back down to sea level on the leeward side of the mountain? 8. (a) Assuming that no water vapor is added as the parcel descends shle bas down the leeward side of the mountain to sea level, is the water vapor content (the mixing ratio) of the parcel higher or lower than before it began to rise over the mountain? Why? mun svibalo ada nist What is the lifting condensation level of this parcel now, after descending to sea level on the leeward side of the mountain? 98 Copyright © 2022 Pearson Education, Inc. g/kg .g/kg g/kg feet
Transcribed Image Text:ro Physical Geography Laboratory Manual Name EXERCISE 16 PROBLEMS-PART IV (English Units) at pa Answer the following questions after completing the problems in Part III. You will also need to refer to the table of Saturation Mixing Ratios in Figure 15-1; interpolate from the chart as needed. Assume that condensation begins at 100% relative humidity and that no evaporation takes place as the parcel descends. 5. 6. 7. (a) (b) (b) 1000S As the air rises up the windward side of the mountain (a) Section On the windward side of the mountain, should the relative humidity of the parcel change as it rises from 3000 feet to 6000 feet? Why? (b) (c) What is the capacity (saturation mixing ratio) of the rising air at 3000 feet? 31 es 2noltsvolo 2016 What is the capacity of the air at 6000 feet? What is the capacity of the air after it has descended back down to sea level on the leeward side of the mountain? 8. (a) Assuming that no water vapor is added as the parcel descends shle bas down the leeward side of the mountain to sea level, is the water vapor content (the mixing ratio) of the parcel higher or lower than before it began to rise over the mountain? Why? mun svibalo ada nist What is the lifting condensation level of this parcel now, after descending to sea level on the leeward side of the mountain? 98 Copyright © 2022 Pearson Education, Inc. g/kg .g/kg g/kg feet
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