The Atmosphere: An Introduction to Meteorology (13th Edition) (MasteringMeteorology Series)
The Atmosphere: An Introduction to Meteorology (13th Edition) (MasteringMeteorology Series)
13th Edition
ISBN: 9780321984623
Author: Frederick K. Lutgens, Edward J. Tarbuck, Dennis G. Tasa
Publisher: PEARSON
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Chapter 7, Problem 6GST

(a)

To determine

The explanation for the given statement that states that the only true zonal distribution of pressure exists in the region of the subpolar low in the Southern Hemisphere.

(b)

To determine

The explanation for the given statement that states that the subtropical highs are stronger in the North Atlantic in July than in January.

(c)

To determine

The explanation for the given statement that states that the subpolar lows in the Northern Hemisphere are the result of individual cyclonic storms that are more common in the winter.

(d)

To determine

The explanation for the given statement that states that a strong high-pressure cell develops in the winter over northern Asia.

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Activity 12.3: Wave Refraction Pgs 202-203Figure 12.2 is a map view of a headland along a coastline. The water depths are shown by blue contour lines. As you complete the following questions, assume that waves with a wavelength of  60 feet are approaching the shoreline from the bottom left of the figure. 1. At approximately what water depth-10, 20, 30, or 40 feet-will the approaching waves begin to touch bottom and slow down? (Hint: Recall that this occurs when the water depth is one-half the wavelength.)  2. Using the wave shown in Figure 12.2 as a starting point, sketch a series of lines to illustrate the wave refraction that will occur as the wave approaches the shore by following these steps:Step 1: Mark the position on the 30-foot contour line where the wave front will first touch bottom.Step 2: Knowing that the section of the wave that touches bottom will slow down first, sketch the shape of the wave front when it reaches the 20-foot contour line.Step 3: Using the same…
N Depth of water contour Advancing wave crest Beach HEADLAND -10- -20- -30' Land -40'- 50- 0 Beach Scale 200 feet
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