MOHAMMAD Assignment1
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Queens University *
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Course
102
Subject
Geography
Date
Apr 3, 2024
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docx
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6
Uploaded by MajorDinosaur4175
GEOGRAPHY 102 Winter 2024
Assignment #1
Weather and Climate
EXERCISE 1: WEATHER MAP INTERPRESTATION
Questions: 1.
Compare Maps 1 through 3. Describe changes to the weather of The Pas, Manitoba over this time period. What caused these changes? (3 marks)
The weather underwent some significant changes between maps 1 and 3. Wind speed, cloud coverage and air pressure all increased, while the temperature dropped. Additionally, there was a shift from occlusion to a cold front. Overnight, the wind speed decreased, but picked up again during the day and night. This can be observed by the changes in the isobar proximity. As the night transitioned to day and back to night, the isobars became closer, indicating higher wind speeds. Cloud coverage increased slightly from 0 to 1/8. Air pressure increased significantly from around 1009.0 mb to 1023.0 mb, which means the wind will slow down from earlier. The temperature decreased notably between weather maps 1 and 3
due to the change from occlusion to a cold front. 2.
Based on the information in Map 3, complete the table below to compare the weather recorded at Edmonton, Alberta; Trout Lake, Ontario; and Charlottetown, Prince Edward Island. Be sure to include proper units. (5 marks)
Edmonton, Alberta
Trout Lake, Ontario
Charlottetown, PEI
Air Temperature
6
°
C
0
°
C
9
°
C
Dew Point
-2
°
C -3
°
C
1
°
C
Sky Cover
1/8
6/8
2/8
Air Pressure
1022.7 kPa
1012.7 kPa
1023.1 kPa
Wind Speed
5-13 km/hr
14-22 km/hr
14-22 km/hr
Wind Direction*
NE
NW
NW
*Approximate your value as one of N, NE, E, SE, S, SW, W, NW
3.
Refer to Map 4 for the below two-part question:
a.
Examine that air temperature and dew point of the air for stations falling within the shaded areas that indicate precipitation. What can you say about the relationship of air temperature? (2 marks)
The first area of precipitation appeared in Northern Alberta’s air temperature is at approximately 3
°
C; and dew point is between 2
°
C and 3
°
C. In Northeastern United States,
which is the second area of precipitation, the air temperature is between 9
°
C and 12
°
C; and the
dew point is between 6
°
C and 12
°
C differing between states. The first area of precipitation in Quebec has air temperature between 1
°
C and 2
°
C; and the dew point presents between -1
°
C and 1
°
C. Through observing the relationship between the air temperature and dew point at these specific areas of precipitation it is evident that the cooler the air temperatures that have higher dew points increases the chances of precipitation. b.
Contrast these differences between air temperature and air’s dew point temperature
to those in the southwestern United States. What is the relationship between air temperature and dew-point difference, and the potential for precipitation? (2 marks)
The area of precipitation in the Southwestern United States has higher air temperatures and a higher dew point. This depicts that the air has less moisture, meaning the chances for rainfall are lower.
4.
Refer to Map 5. Identify the area with the greatest pressure gradient. Calculate the pressure gradient (mb/km) across at least 5 isobars. Note that a degree of latitude equals approximately 100 km. although there are no weather stations in the areas of the
steepest gradients, speculate as to what the wind speeds could potentially reach in this region. (4 marks)
1008 -984 = 24
24 mb/500 km
0.048 mb/km
The nearest weather station had predicted a wind speed of a minimum of 50 km/hr. As the isobars continue to migrate closer to each other, we can predict that the wind speed will be between 60 and 69 km/h. EXERCISE 2: WORKING WITH CLIMATE DATA – PART 1
Questions:
5.
Examine the weather data for Kingston, ON (Latitude 44
°
15’ N; Longitude 76
°
30’ W; Elevation 104m), in July 1900 and July 2020 that are contained in the attached data sheets. Fill in the summary columns for each year. (4 marks)
JULY – Normal*
JULY 1900
JULY 2020
Temperature
Mean Daily Average (
°
C)
21.5
19.79
°C
23.10°C
Mean Daily Maximum (
°
C)
25.9
24.37
°C
27.80°C
Mean Daily Minimum (
°
C)
17.1
15.18
°C
18.40°C
Precipitation
Total Precipitation (mm)
64.3
56.2mm
102.3mm
*Normals derived from 1981-2010 [you should be able to find and confirm these values from the National Climate Date and Information Archive; the website provided]
6.
Provide a general comparison of the weather in July 1900 with that in July 2020. Highlight the most significant differences between the two years. (2 marks)
The daily average, maximum, and minimum temperatures have shown a significant increase between July 1900 and July 2020. This could be attributed to the impact of global warming, which has increased over time and is a significant contributor to temperature changes. The two most notable differences between these two years are the amount of precipitation and the mean daily average temperature. In July 1900, the total precipitation was 56.2mm, which was below average. However, in July 2020, the precipitation almost doubled to 102.3mm, which was
way above normal. The mean daily average temperature in July 1900 was around 19.79°C, which was below normal, while in July 2020, the mean daily average temperature was 23.10°C, which was above normal.
7.
Compare the data you have entered into the table with the July climate normals that are
entered in the first column. In meteorological terminology ‘normals’ are averages and from a long time period (typically 30 years). In this instance, the normal for Kingston are based on data collected from 1981 to 2010. Based on these data, answer the following questions:
a)
What generalizations can you make about Kingston weather in July 1900 and 2020 in comparison to the long-term average (i.e., 1981-2010 average)? Was the weather in July 1900 and July 2020 normal or abnormal? Explain. (3 marks)
b)
Can these observations be used to support or contradict the argument for global climate
change? Why or why not? (3 marks)
The recorded data and observations of temperature and precipitation levels in July 1900 and July 2020 can be used to support or contradict the theory of global warming. The temperature recorded in July 2020 was noticeably higher than the average, and the amount of precipitation was almost double the average. This suggests that as the temperature rises, more evaporation takes place, leading to an increase in precipitation. Therefore, the surge in temperature and precipitation levels is evidence of a warmer climate.
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