ESCI110-20224-LEC
Clouds and Moisture Laboratory Assignment
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Clouds and Moisture Laboratory Assignment

  • Due Nov 28, 2021 by 11:59pm
  • Points 15
  • Submitting a text entry box or a file upload

Introduction

             Weather and climate are of vital interest to people in many of their daily activities.  There are a few key elements to weather and climate, one of which is moisture content. In this lab we will examine the changes of state of water, how water vapor content of the air is measured, and the events that lead to cloud formation.

Objectives

Upon completion of this exercise, you should be able to:

  • Explain adiabatic heating and cooling and be able to calculate temperature changes associated with changing altitudes
  • Describe the change of temperature associated with normal lapse rates and calculate temperature changes associated with normal lapse rates

Water Vapor Capacity and Relative Humidity

Use the table below to answer the following question.

Table 1.

Water Vapor capacity of a Kilogram of air

(at average sea level pressure

      Temperature      Grams of water vapor

(ºC)           (ºF)              per kg of air (g/kg)

-40

-40

0.1

-30

-22

0.3

-20

-4

0.75

-10

14

2

0

32

3.5

5

41

5

10

50

7

15

59

10

20

68

14

25

77

20

30

86

26.5

35

95

35

40

104

47

From Tarbuck, Lutgens, Pinzke  
Applications and Investigations in Earth Science.
3rd Edition, Prentice Hall, 2000

 

1. What is the water vapor capacity for a kilogram of air at each of the following temperatures?

-10ºC: ­­­­­­­­­­­__________ g/kg                                

35ºC: ­­­­­­­­­­­__________ g/kg

41ºF: ­­­­­­­­­­­__________ g/kg                                 

77ºF: ­­­­­­­­­­­__________ g/kg

2. Raising the temperature of a kilogram of air from 20ºC to 25ºC increases or decreases its water vapor capacity and by how much?

3. Decreasing the temperature of a kilogram of air from 95ºF to 86ºF increases or decreases its water vapor capacity and by how much.

 

 Relative Humidity = Water Vapor Content   X     100
                                               Water Vapor Capacity 

4.                    Air Temp.            Water Vapor                   Relative
                          Content               Capacity                           Humidity

20ºC                   2g/kg            ________g/kg                         ________%

20ºC                   7g/kg            ________g/kg                         ________%

20ºC                   10g/kg          ________g/kg                         ________%

5.                    Air Temp.           Water Vapor                       Relative
                        Content                  Capacity                            Humidity

15ºC                   2g/kg            ________g/kg                         ________%

20ºC                   2g/kg            ________g/kg                         ________%

25ºC                   2g/kg            ________g/kg                         ________%

6. How does the relative humidity vary if the temperature is constant but the water vapor content increases?

7. How does the relative humidity vary if the water vapor content is constant but the temperature increases?

8. What do you think would happen to the relative humidity if the water vapor content remains the same but the temperature decreases?

9. If you turn on the heat in your house, how does that affect the relative humidity?

10. Refer back to the table, What is the dew point temperature of a kilogram of air that contains 10g of water vapor?

Temp. ____________ºC

11. What is the relative humidity and dew point temperature of a kilogram of air that is 15ºC and contains 2 grams of water vapor?

Relative humidity _______________%

Dew-point temperature _______________ºC

 

Adiabatic Processes.

12. Adiabatic heating and cooling is a temperature change caused by a change in ___? 

13. As air is forced to rise, pressure (increase, decreases) and air temperature (increases,  decreases).  

The Dry Adiabatic Rate vs. the Saturated or Wet Adiabatic Rate (when do you use one or the other to calculate the change in temperature).

The dry adiabatic rate is about  5.4 °F for 1,000 feet of elevation change.

The wet adiabatic rate is about 2.7°F for 1,000 feet of elevation change.

 

14. Air is moving across a mountain front in Figure 1. Calculate the temperature of air at the points labeled B, C, D and E in Figure 1.  Values are in feet and °F.

Assume that the Dew point is reached at 6,000 feet.  Once Point D is reached, the air has become unsaturated. Show your calculations to the right of each answer.

B  __________

C  __________

D  __________

E  __________

 

Air moving over a ridge.

Figure 1.  Cross Section Showing Air(Arrow) Rising over Mountain

15.  At what elevation could precipitation begin?  What type of precipitation would this be?

 

1638172799 11/28/2021 11:59pm
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Video Lecture: Relative Humidity Video Lecture: Fog and Cloud Formation