Pearson eText for Exercises for Weather & Climate -- Instant Access (Pearson+)
9th Edition
ISBN: 9780137612949
Author: Greg Carbone
Publisher: PEARSON+
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Chapter 10, Problem 1E
To determine
Labelling the air masses in the maps in Figure 10-2.
Expert Solution & Answer
Answer to Problem 1E
The following picture shows the air mass on Monday.
The following picture shows the air mass on Tuesday.
The following picture shows the air mass on Wednesday.
Explanation of Solution
According to Norwegian polar front theory, the mid latitude cyclones are occurring in northern hemisphere along a stationary front, when two different temperature of air masses flowing in opposite direction in the same front.
A separating barrier is formed between these two air masses and wave like a surface flow is developed, such as warm air conveyer belt.
When cold air overtakes the warm air and it is separated from the center of the low-pressure occluded front is formed and pave the way for steepest pressure gradient.
The surface flow forms an isobar with the low pressure at the center of the wave and at final stage, the flow is inward and counterclockwise. Finally, air mass will start to weaken, and then storm will start to disintegrate.
Always mid latitude cyclones require two different extreme temperature air masses. In summer, the different in temperature is less compared to that of in winter and spring. Hence, mid latitude cyclones are occurring in less over United States in hot season compared to that of in winter and spring.
Always moisture characteristics are represented by small letter and temperature characteristics are represented as capital letter. The following are the examples of different air mass representation.
- maritime equatorial – mE
- maritime tropical –mT
- maritime polar –mP
- continental tropical –cT
- continental polar – cP
- continental arctic–cA
Below the warm front, air mass categorized as mT and it is warm. This air mass contains moisture in general. Above the cold front, the air mass categorized as cP and it is generally cold and dry.
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Chapter 10 Solutions
Pearson eText for Exercises for Weather & Climate -- Instant Access (Pearson+)
Ch. 10 - Prob. 1ECh. 10 - On all three maps and at each station (AD), use...Ch. 10 - The conditions at each station (A, B, C, and D)...Ch. 10 - How much did the pressure drop in the storms...Ch. 10 - How did the surface pressure gradient in the Great...Ch. 10 - How do the cloud and precipitation patterns match...Ch. 10 - What was the range of temperature and dew-point...Ch. 10 - What was the predominant wind direction in the...Ch. 10 - How much lower were temperatures and dew-point...Ch. 10 - Describe the differences in wind speed and...
Ch. 10 - Which station experiences the lowest surface...Ch. 10 - From 9/0300 to 10/0900 by how much did the dew...Ch. 10 - When did the cold front pass Indianapolis?Ch. 10 - Describe how the winds in Indianapolis shifted...Ch. 10 - When did the cold front pass Oklahoma City? How...Ch. 10 - When did the cold front pass Birmingham? Was there...Ch. 10 - Surface pressure typically drops as a front...Ch. 10 - Circle and label areas of warm-air and cold-air...Ch. 10 - Air should rise in areas of warm-air advection and...Ch. 10 - How does the area of warm-air advection and upward...Ch. 10 - Highlight the 0 isotherm. Does it conform to the...Ch. 10 - Identify an area of directional divergence...Ch. 10 - Prob. 23ECh. 10 - Prob. 24ECh. 10 - Prob. 25ECh. 10 - Prob. 26ECh. 10 - a. Summarize what caused the spatial pattern of...Ch. 10 - Prob. 1RQCh. 10 - Prob. 2RQCh. 10 - Prob. 3RQ
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