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Arizona State University *
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Course
112
Subject
Geography
Date
Apr 3, 2024
Type
Pages
7
Uploaded by DoctorPartridge4095
3/31/24, 11
:
17 PM
Lightning in the Peaks: Northern Arizona Climate and Lightning Strikes: GPH 112: Intro to Phys Geography Lab (2024 Spring)
Page 1 of 7
https://canvas.asu.edu/courses/178831/quizzes/1343074
?
module_item_id=12797102
Lightning in the Peaks: Northern Arizona Climate and Lightning
Strikes Due Feb 14 at 11:59pm
Points 5
Questions 3
Available after Jan 21 at 12am
Time Limit None
Instructions
For the following questions, investigate the monthly changes in lightning strike, temperature, dew point, and
precipitation data for Flagstaff, Arizona. Remember, dew point simply is the temperature that the air would have to cool to in order for moisture in the air to
condense into water droplets (forming dew or clouds). Humidity on the other hand is the ratio of moisture in the air
compared to how much it can hold. This is dependent on temperature, so we'll stick with dew point as it easier to see
a seasonal shift. In essence, the higher the dew point, the more moisture that exists within the atmosphere - however,
dew point
cannot exceed air temperature and is dependent on air temperature. Colder air simply cannot hold as much moisture,
so there is less available to condense and form clouds (think of polar deserts like Antarctica!).
When you hear of dry heat, that often is associated with warm, dry air, meaning a large difference between
temperature and dew point. When that begins to change, and dew point increases, it feels humid and uncomfortable,
and you are more likely to have rain and storms. Changes in dew point are one of the driving features for the change in precipitation and lightning strikes across the
southwestern United States during the summer, as the North American Monsoon becomes more prominent.
Monthly climate data for Flagstaff, Arizona can be found below. Monthly Air Temperature
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
C
1.7
2.8
4.4
7.2
11.6
18.3
19.4
16.6
15.0
10.0
3.9
0.6
F
35.1
37.0
39.9
45.0
52.9
64.9
66.9
61.9
59.0
50.0
39.0
33.1
Monthly Dew Point Temperature
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
C
-9.4
-5.0
-6.1
-5.6
-3.9
-3.9
10.6
11.1
10.0
2.8
-5.6
-3.9
F
15.0
23.0
21.0
22.0
25.0
25.0
51.0
52.0
50.0
37.0
22.0
25.0
Monthly Precipitation
o
o
o
o
3/31/24, 11
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Lightning in the Peaks: Northern Arizona Climate and Lightning Strikes: GPH 112: Intro to Phys Geography Lab (2024 Spring)
Page 2 of 7
https://canvas.asu.edu/courses/178831/quizzes/1343074
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module_item_id=12797102
Attempt History
Attempt
Time
Score
LATEST
Attempt 1
2 minutes
5 out of 5
Score for this quiz: 5 out of 5
Submitted Feb 14 at 8:02pm
This attempt took 2 minutes.
Question 1
2 / 2 pts
Answer 1:
.06%
Correct!
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
mm
50.0
54.0
50.0
34.0
35.0
12.0
121.0
132.0
67.0
35.0
33.0
45.0
in
2.0
2.1
2.0
1.3
1.4
0.5
4.8
5.2
2.6
1.4
1.3
1.8
Study Area Lightning Strikes
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Count
0
0
10
25
25
10
3200
3500
500
10
0
0
First, let's understand why we are using lightning strikes in August, and not in May or June. It has to do with the
change of moisture in the atmosphere, brought by the North American Monsoon. To prove this, answer the following
questions using the data table above:
Monthly Percentage = ((Sum of May, June OR July, August) / Total Precipitation)*100
Calculate the percentage of annual precipitation that falls in May and June: 7.8%
Calculate the percentage of annual precipitation that falls in July and August: [ Select ]
Which month of the year had the greatest difference between temperature and dew point:
[ Select ]
Which two months had the highest number of lightning strikes: [ Select ]
Recall your knowledge from the lecture on the North American Monsoon.
Why does the precipitation and lightning strike count change so dramatically throughout the summer?
[ Select ]
3/31/24, 11
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Lightning in the Peaks: Northern Arizona Climate and Lightning Strikes: GPH 112: Intro to Phys Geography Lab (2024 Spring)
Page 3 of 7
https://canvas.asu.edu/courses/178831/quizzes/1343074
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module_item_id=12797102
7.8%
12%
2.5%
Answer 2:
10%
12.5%
8.2%
Correct!
38%
Answer 3:
December
April
Correct!
June
July
Answer 4:
May and June
October and November
Correct!
July and August
June and September
Answer 5:
The dew point drops with the increasing temperature, so precipitation also increases.
Temperatures drop, so the precipitation increases since it is closer to forming snow.
Correct!
Shifting monsoon winds bring moisture-laden air to the region , increasing dew point.
The lakes around Arizona fill up, increasing humidity across the region.
May and June are extremely dry months in the Flagstaff area. Winter storms (wave cyclones) have moved north
along with the jet stream (storm rack), and the summer monsoon has not yet started. In contrast, after the monsoon
gets going around July 4th or so, about a quarter of the annual rainfall takes place in July and August. The dramatic
change from June to July is the monsoon. Notice the SINGULAR use of the word monsoon. Monsoon is a wind shift.
Lots of people call storms “monsoons”, but that is ignorance. It is the shifting wind pattern that brings the tropical
moist air into the Flagstaff area, and this increases the dew points.
Question 2
1 / 1 pts
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3/31/24, 11
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Lightning in the Peaks: Northern Arizona Climate and Lightning Strikes: GPH 112: Intro to Phys Geography Lab (2024 Spring)
Page 4 of 7
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module_item_id=12797102
The greatest clusters of lightning occurs primarily on the middle-slopes on cool north and west facing sides of the peaks and hills.
Correct!
The greatest clusters of lightning occurs primarily on the middle-slopes on warm south and east facing sides of the peaks and hills.
The greatest clusters of lightning occurs primarily along the high ridgeline and mountain tops of the San Francisco Peaks.
The greatest clusters of lightning occurs primarily in the low, flat regions near Flagstaff and west of the San Francisco peaks.
You should have seen the slopes, especially over Shultz Pass and the eastern slopes of the San Francisco Peaks (in
the image below), absolutely covered in lightning strikes, while the cooler mountain slopes on the western and north
side were much quieter.
Question 3
Fast travel to the eastern edge of Flagstaff at these coordinates: 35.2191 N , -111.5863 W. Change the geovisualization layer to display air temperature. Use the helicopter fast travel mode to go from your current location to 35.4023N, -111.7008 W, a transect taking you
up and over the San Francisco Peaks to the northwest. While you travel, closely look at the lightning strike distribution. What lightning strike pattern do you observe while
moving up and over the San Francisco Peaks in this transect? HINT: You can see where lightning strikes are happening by observing the small circles on the ground. Those are
where lightning will randomly strike, and if you waited (or flew) and watched, would see this clustering.
3/31/24, 11
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Lightning in the Peaks: Northern Arizona Climate and Lightning Strikes: GPH 112: Intro to Phys Geography Lab (2024 Spring)
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https://canvas.asu.edu/courses/178831/quizzes/1343074
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module_item_id=12797102
2 / 2 pts
Of course, lightning strikes in other places as well, not just in one area. Often though, the first thunderstorms of the
day will begin over the higher terrain around Flagstaff, and more generally over the higher terrain across Arizona. You might be familiar with radar on a weather app. It's a bunch of colors meaning rain is nearby or heading your way. We're going to take a look at a radar loop in northern Arizona to help us begin to understand the distribution of
lightning we see within the lightning game. But first, we need to briefly look at what radar is and how to interpret it. Radar dishes send out a pulse of energy that bounces
off objects in the air like dust, rain, hail, or even bats and
bugs. The data collected by this return signal can tell us
the size, speed, and direction of the objects the radar
pulse bounces off of. You are likely most familiar with
radar reflectivity, or the strength of the return signal
related to size of the features. This value is in dBZ or
decibels. A value of 20 dBZ is typically the point at which light rain
begins. A value around 40-45 dBZ indicates heavy rain.
The values of 60 to 65 dBZ is about the level where 1"
(2.5 cm) diameter hail can occur. You can see the scale
an an image of a strong thunderstorm with heavy rain
and possible hail in the picture to the right. Radar can get a little bit more complicated due to how it
is measured, and you can even start to discern features
within a storm system, like rotation or debris lofted by
tornadoes. But that's beyond this 100 level class, if you
are interested in learning more how to interpret radar,
ASU has meteorology courses that dive a bit deeper. In
the meantime, if you want to learn to interpret the
greater details of radar yourself, check out this National
Weather Service website:
https://www.weather.gov/jetstream/doppler_intro
(https://www.weather.gov/jetstream/doppler_intro) Below is a 2 hour base reflectivity loop centered over northern Arizona. You can see Flagstaff located just below the
middle of the map, and the San Francisco Peaks north of the city. Interstate 40 cuts through the lower third of the
map from west to east and Interstate 17 extends south of Flagstaff towards Phoenix. If you look closely, you can see
some major feature labels like Flagstaff, the San Francisco Peaks, Upper Lake Mary, and Sitgreaves Mountain.
3/31/24, 11
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Lightning in the Peaks: Northern Arizona Climate and Lightning Strikes: GPH 112: Intro to Phys Geography Lab (2024 Spring)
Page 6 of 7
https://canvas.asu.edu/courses/178831/quizzes/1343074
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module_item_id=12797102
Answer 1:
above Flagstaff Pulliam Airport
Correct!
above Humphreys Peak
above Sitgreaves Mountain
above Upper Lake Mary
Answer 2:
roughly 35 dBZ above Sitgreaves Mountain
roughly 40dBZ above Upper Lake Mary
Correct!
roughly 50dBZ on the southern side of the San Francisco Peaks and in the volcanic field east of Highway 89
roughly 70dBZ directly over downtown Flagstaff
Answer 3:
north of the San Francisco Peaks
to the northwest, towards the Grand Canyon
Correct!
south of Interstate 40
west of Sitgreaves Mountain
Flagstaff Radar
QUESTION: Using the reflectivity scale discussed above, fill in the following statements. Thunderstorms first begin to form [ Select ]
. From there, the strongest reflectivity value (dBZ) is
observed at roughly 50dBZ on the southern side of the San Francisco Peaks and in the volcanic field east of Highway
89 . By the end of the radar loop, the majority of storms can be located [ Select ]
.
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Lightning in the Peaks: Northern Arizona Climate and Lightning Strikes: GPH 112: Intro to Phys Geography Lab (2024 Spring)
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Quiz Score: 5 out of 5
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