GEG1301_Lab3_Atmosphere and ocean circulation
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Apr 3, 2024
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Student Name:___________________________ Student #:________________
Department of Geography, Environment and
Geomatics
GEG 1301 THE PHYSICAL ENVIRONMENT
Fall 2022
Laboratory #3: The Atmosphere and Ocean
Circulation
Professor: Roxanne Frappier
Due Date
Group A01: November 15
th
Group A02: November 22
nd
Purpose: The purpose of this lab is to provide an introduction to atmospheric
composition and stratification, and
ocean currents and
circulation
. Students
will learn about important atmospheric concepts, such as the role of temperature
in controlling the amount of water vapour contained in an air parcel, and how
atmospheric temperature and pressure change as a function of altitude.
Students will also test their ability to locate and map global surface and deep-
water currents, and examine the effects of salinity, density and temperature on
water circulation.
By completing this lab, students will become familiarized with producing tables
and figures, as well as the creation and placement of appropriate captions.
Critical thinking, simple mathematic skills, observations and descriptions, and
knowledge of table and figure components are basic skills that will be acquired in
this lab, and will be applicable in future geographic studies. Assignment:
Answer the following questions (#1-19) in the spaces provided.
The total points available for this assignment = 82 points
All lab assignments must be completed and handed in individually. Format:
Students will hand in (a) questions with completed answers, (b) 7
completed tables, (c) Figure 1 with an appropriate figure caption, and (d)
completed Figures 3 and 4.
Tables and figures should be produced to the standards of the
Department of Geography, Environment and Geomatics, University
of Ottawa. For guidelines on proper formatting and presentation of
tables and figures, please see the lab manual provided with this
course.
SECTION 1 – COMPOSITION OF THE ATMOSPHERE (23 points)
1.
Complete missing information in table below
. The total mass of the
atmosphere is about 5.15 x 10
16
kg. Create an appropriate caption
for the
table, and select the proper placement (Above? Below? To the right?).
Ensure that your caption begins with “Table 1:”. (2 points)
Atmospheric
gas
% of atmosphere
Total mass (kg) Nitrogen (N
2
)
78.09
Oxygen (O
2
)
Argon (Ar)
0.93
Other
0.03
2.
During the summer months, residents of the Ottawa region often complain
about the humidity. On those humid days the air feels heavier. Is humid air
actually heavier than dry air? The following few steps will help you answer
this question. Table 1 (above) presents gaseous composition of an air parcel
with no water vapour. Table 2 presents the gaseous composition of a
hypothetical air parcel, which contains 4% of water vapour. “Other gases” have been omitted and because values have been rounded
up, the relative change in percentage is only noticeable in the nitrogen
and the oxygen. Since water vapour (H
2
O) makes up 4% of the air parcel,
the relative abundance of other gases diminishes by 4% (Nitrogen 3%
and Oxygen 1%). Why does argon (Ar) remain at 1%
? (3 points)
Table 2. Composition of an air parcel that contains 4% water vapour.
Atmospheric gas
% of atmosphere
Nitrogen (N
2
)
75
Oxygen (O
2
)
20
Argon (Ar)
1
Water vapour
4
3.
Table 3 presents the atomic mass number of the elements that constitute the
atmospheric gases, and also that of hydrogen (one of the “other” gases). Also
found in Table 4 are the gas formula and gas mass. It takes two atoms of the
element nitrogen
to produce nitrogen in its gaseous form (N
2
); therefore the
mass of a molecule of nitrogen is 28 (two atoms of atomic mass number of
14). The same can be said for oxygen and hydrogen. Argon, a noble gas, can
exist in a monoatomic form
, therefore the argon gas mass is of 40. Water
vapour, the gaseous form of water, is composed of H
2
O: two atoms of
hydrogen and one atom of oxygen. Complete Table 3. (3 points)
Table 3. Gas mass of atmospheric gasses.
Element
Atomic mass number
Gas formula
Gas mass
Nitrogen (N)
14
N
2
28
Oxygen (O)
16
O
2
Argon (Ar)
40
Ar
40
Hydrogen
1
H
2
2
-
H
2
O
4.
Remember our question: Is humid air heavier than dry air?
Table 4 will give
you more information to help you answer the question. The data in Table 4 is
based on a hypothetical air parcel, which is composed of 100 molecules of
gas. In the first column data is provided for dry air, which contains 0% water
vapour. In the second column data is provided for humid air, which contains
4% water vapour. Complete the following table and include a caption,
beginning with “Table 4:”
. (10 points)
Dry air parcel of 100
molecules
(H
2
O = 0%)
Humid air parcel of 100
molecules
(H
2
O = 4%)
Number of N
2
molecules
Number of O
2
molecules
20
Number of Ar molecules
1
Number of H
2
O molecules
0
Mass of all N
2
molecules
Mass of all O
2
molecules
672
Mass of all Ar molecules
Mass of all H
2
O molecules
0
Mass of all molecules
5.
Now you can answer the question: Is humid air heavier than dry air?
Answer and provide a short explanation. (5 points)
SECTION 2 – ATMOSPHERE STRATIFICATION, TEMPERATURE, AND PRESSURE (17 points)
6.
In the next few steps, you will be constructing a figure that represents the
location of the atmosphere layers, the changes of atmospheric temperature
and pressure as a function of altitude. Most of the data necessary to the
construction of your figure is presented in Table 5. First, start by
completing Table 5. (2 points)
Table 5. Atmospheric temperature and pressure as a function of altitude above sea level
Elevation ( )
Temperature
( )
Atmospheric pressure ( )
0
15
1013.25
1
8.5
878.36
2
2
761.43
3
-4.5
660.07
4
-11
572.20
5
-17.5
496.02
6
-24
429.99
7
-30.5
372.75
8
-37
323.13
9
-43.5
280.11
10
-50
242.82
20
-56
58.19
30
-46.5
13.94
40
-22.1
3.34
50
-2.5
0.80
60
-27.7
0.2
70
-55.7
0.04
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