Exercises for Weather & Climate (9th Edition)
9th Edition
ISBN: 9780134041360
Author: Greg Carbone
Publisher: PEARSON
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Question
Chapter 12, Problem 1E
To determine
The major source of maritime tropical air affecting the United States. Also describe the way in which proximity to this source influence the spatial pattern of thunderstorms.
Expert Solution & Answer
Answer to Problem 1E
The major source is the Gulf of Mexico. A large number of thunderstorms are developed in this area due to the proximity of the southeast and central United States to this moisture source.
Explanation of Solution
The development of thunderstorms and tornadoes occurs following the forced rise of warm, moist air in an unstable atmosphere. Thunderstorms often considered as air mass thunderstorms or severe thunderstorms based on its formation. The development of some occurs within a warm, moist air mass, whereas others require strong vertical wind shear.
Thunderstorms are occurred most frequently in the United States when maritime tropical air is forced aloft through the process of orographic lifting, frontal lifting, intense surface heating, or convergence of surface air flow.
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Students have asked these similar questions
44) In periglacial environments, the layer of ground that thaws every summer and freezes every winter is called
A) frost layer
B) permafrost
C) active layer
D) discontinuous permafrost
Use the attached piezometer map to make your own, clean version of the map, and indicate the elevation of the water table at all piezometer locations.
Draw equipotential lines (lines of equal water table elevation) using regular intervals – creating a contoured map of the water table.
Determine the direction of groundwater flow based on the horizontal gradient. Label the areas of recharge and discharge directly on your map.
Flow lines: Draw flow lines on your water table map. The lines should be at right angles to the equipotential lines and extend from the recharge area to the discharge area.
Hydraulic Gradient, Specific Discharge (Darcy Flux), Average Linear Velocity:
Using your water table map, estimate an average hydraulic gradient between two locations, call them locations A and B, one at the eastern-most and a second at the western-most extent of your dataset (note the north arrow on the map).
Calculate the specific discharge, q, between the two locations. For this calculation…
Calculate all the values of table 1:
Q in (L/day)
Q out (L/day)
Residence time (days)
Please show all steps
Chapter 12 Solutions
Exercises for Weather & Climate (9th Edition)
Ch. 12 - Prob. 1ECh. 12 - What processes over the Florida peninsula force...Ch. 12 - What geographic feature might contribute to the...Ch. 12 - If you see a lightning bolt in the distance and 15...Ch. 12 - Recall that updraft s within the thunderstorm...Ch. 12 - Prob. 6ECh. 12 - Entrained air is drier than the air within a...Ch. 12 - How could updraft s and downdraft s contribute to...Ch. 12 - Explain how downdraft s can trigger the...Ch. 12 - How do air mass conditions ahead of the squall...
Ch. 12 - Label the cP, cT, and mT air masses in the map...Ch. 12 - Prob. 12ECh. 12 - Circle the upper-air inversion layer on the...Ch. 12 - How would you characterize the temperature and...Ch. 12 - How would you characterize the temperature and...Ch. 12 - Using the wind speed and direction symbols in...Ch. 12 - Identify as many of these conditions as you can to...Ch. 12 - Prob. 18ECh. 12 - Prob. 19ECh. 12 - Prob. 20ECh. 12 - Reflecting on the forces producing winds, how does...Ch. 12 - Prob. 22ECh. 12 - Prob. 23ECh. 12 - Prob. 24ECh. 12 - Figures 12-25 through 12-27 show the locations of...Ch. 12 - Prob. 26ECh. 12 - Prob. 1RQCh. 12 - Prob. 2RQCh. 12 - Prob. 3RQ
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