
Introduction to Station Models
Presentation
•
Science
•
8th - 10th Grade
•
Hard
Joseph Anderson
FREE Resource
6 Slides • 22 Questions
1
Weather Maps, Station Models, and Air Masses
​
2
Multiple Choice
3
Multiple Choice
4
Multiple Choice
5
Multiple Choice
Warm air is ______ dense than cool air. Warm air rises and cool air sinks.
less
more
6
Multiple Choice
7
Multiple Choice
8
Multiple Choice
9
Multiple Choice
10
Draw
Draw an arrow to identify the direction of the weather pattern approaching Virginia. Then indicate what type of weather is moving towards Virginia.
11
12
Draw
Answer the following: Identify which part tells you wind speed. What direction is the wind blowing? What is the current sky conditions? Is there precipitation and, if so, how much?
13
Multiple Choice
What is the temperature for the following station model?
4 ºF
76 ºF
80 ºF
129 ºF
14
Multiple Choice
What is the dewpoint for the following station model?
10 ºF
23 ºF
65 ºF
75 ºF
15
Multiple Choice
What is the present weather for the following station model?
rain
thunderstorms
drizzle
fog
16
Multiple Choice
What is the amount of precipitation for the following station model?
.15 in
1/4 in
6 in
46 in
17
Multiple Choice
What is the wind direction for the following station model?
north
east
northwest
northeast
18
Multiple Choice
What is the wind speed at this location?
5 knots
10 knots
15 knots
20 knots
19
What is an Air Mass?
An air mass is a large volume of air in the atmosphere that is mostly uniform in temperature and moisture. Air masses can extend thousands of kilometers across the surface of the Earth, and can reach from ground level to the stratosphere—16 kilometers (10 miles) into the atmosphere.
20
Where do Air Masses Form?
Air masses form over large surfaces with uniform temperatures and humidity, called source regions. Low wind speeds let air remain stationary long enough to take on the features of the source region, such as heat or cold. When winds move air masses, they carry their weather conditions (heat or cold, dry or moist) from the source region to a new region. When the air mass reaches a new region, it might clash with another air mass that has a different temperature and humidity. This can create a severe storm.
21
Types of Air Masses
Meteorologists identify air masses according to where they form over the Earth. There are two main categories for air masses: tropical and polar.
Polar air masses form in the arctic region and are very cold. Tropical air masses form in low-latitude areas and are moderately warm.
Air masses are also identified based on whether they form over land or over water. Maritime air masses form over water and are humid. Continental air masses form over land and are dry.
22
Air Masses
Air masses are classified on weather maps using two or three letters.
A lowercase letter describes the amount of moisture in the air mass (m for maritime and c for continental).
An uppercase letter describes the heat of the air mass: T for tropical and P for polar.
There are 4 air mass abbreviations, which can be seen in the diagram to the right.
23
Multiple Choice
24
Multiple Choice
25
Multiple Choice
26
Multiple Choice
27
Multiple Choice
28
Multiple Choice
Weather Maps, Station Models, and Air Masses
​
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