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Table 4.1 saturation Mixing Ratio (at Sea-Level Pressure) Temperature, °C (°F) Saturation Mixing Ratio, g/kg -40 (-40) 0.1 -30 (-22) 0.3 -20 (-4) 0.75 -10 (14) 2 O (32) 3.5 5 (41) 10 (50) 7 15 (59) 10 20 (68) 14 25 (77) 20 30 (86) 26.5 35 (95) 35 40 (104) 47

Table 4.1 saturation Mixing Ratio (at Sea-Level Pressure) Temperature, °C (°F) Saturation Mixing Ratio, g/kg -40 (-40) 0.1 -30 (-22) 0.3 -20 (-4) 0.75 -10 (14) 2 O (32) 3.5 5 (41) 10 (50) 7 15 (59) 10 20 (68) 14 25 (77) 20 30 (86) 26.5 35 (95) 35 40 (104) 47

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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Suppose the air temperature is 20°C (68°F), and the relative
humidity is 50 percent at 6:00 P.M. Also suppose that during the
evening, the air temperature drops, but its water vapor content
does not change. If the air temperature drops 1°C (1.8°F) every 2
hours, will fog occur by sunrise (6:00 A.M.) the next morning?
Explain your answer. (Hint: The data you need are found in Table
4.1 .) 

Table 4.1 saturation Mixing Ratio (at Sea-Level Pressure) Temperature, °C (°F) Saturation Mixing Ratio, g/kg -40 (-40) 0.1 -30 (-22) 0.3 -20 (-4) 0.75 -10 (14) 2 O (32) 3.5 5 (41) 10 (50) 7 15 (59) 10 20 (68) 14 25 (77) 20 30 (86) 26.5 35 (95) 35 40 (104) 47
Transcribed Image Text:Table 4.1 saturation Mixing Ratio (at Sea-Level Pressure) Temperature, °C (°F) Saturation Mixing Ratio, g/kg -40 (-40) 0.1 -30 (-22) 0.3 -20 (-4) 0.75 -10 (14) 2 O (32) 3.5 5 (41) 10 (50) 7 15 (59) 10 20 (68) 14 25 (77) 20 30 (86) 26.5 35 (95) 35 40 (104) 47
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