The Physical Environment
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Weather Systems

Getting Ready for Chapter 8
Weather Systems

Chapters 4 through 7 dealt with elements of weather and climate and set the stage for chapter 8 "Weather Systems". In chapter 8 we'll focus on how these weather elements explain the daily changes in our daily weather. We'll also examine the processes that create, and geographical patterns of, powerful storm systems like tornadoes and hurricanes.

Thunderstorm

Monsoonal thunderstorm over Arizona
Courtesy NOAA (Source)

Weather and climate are elements of physical geography that impact all of our lives. That's why an understanding of the potential effects of climate change is important to all of us. If we stay on our present course, geoscientists predict storm systems in some parts of the world will become more severe. The patterns of both weather systems, and climates could radically shift, causing significant changes in natural habitats, agricultural systems, population distribution, and the economic stability. Geographers will be at the forefront of understanding how these changes will take place, where they will happen, and how we might address them.

What you should already know ...

Weather systems, like any other natural system, are composed of many interacting components. Temperature, moisture, pressure and air circulation combine to create systems that affect our day-to-day weather. We'll focus mostly on the impact of cyclonic systems that form in the mid- to high latitudes in association with jet streams. We'll also look at severe weather systems, thunderstorms, tornadoes, and hurricanes.

The elements of these systems were presented in Chapter 5 "Air Temperature", Chapter 6 "Atmospheric and Oceanic Circulation", and Chapter 7 "Atmospheric Moisture". In particular, you should have a handle on the basic concepts of humidity, precipitation formation, cloud types, air pressure, and wind.

Use the quiz below to assess your understanding of a few key topics from these chapters.

Quiz

1. Which of the following is considered a cold, dry airmass?

mT
mP
cP
cT

2. Wind direction is described as

where the wind comes from.
where the wind is blowing to.

3. Low pressure systems in the Northern Hemisphere exhibit

surface convergence and subsidence
suface convergence and uplift
surface divergence and subsidence
surface divergence and uplift

4. The approximate wind direction and speed (assume north at top of page)

wind speed and direction symbol

SW, 20 knots
NE, 15 knots
SW,15 knots
NE, 20 knots

5. Circulation in a cyclone in the Northern Hemisphere is

clockwise and outward from the center
clockwise and inward toward the center.
counterclockwise and inward toward the center.
counterclockwise and outward from the center

6. ____ uplift occurs when two unlike air masses collide.

Orographic
Convective
Convergent
Frontal

7. A steep pressure gradient would exhibit ___ isobars on a weather map.

closely spaced
widely separated

8. What type of cloud is shown here?

cloud

Cirrus
Stratus
Cumulonimbus
Altostratus

9. If the surface air pressure is 1010 mb it would be considered ______ pressure.

high
low

10. _____ flow occurs when the polar front jet stream and equatorward edge of the circumpolar vortex takes on a curving flow.

zonal
meridonal


 

Score =
Correct answers:

About your score ....

If you scored 80% or above, Great! ... start reading the chapter.

If you scored 70% to 80% you should consider reviewing the previous material.

If you scored less than 70% you should consider reviewing the previous material and seeking help from your instructor.

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For Citation: Ritter, Michael E. The Physical Environment: an Introduction to Physical Geography.
Date visited.  https://www.earthonlinemedia.com/ebooks/tpe_3e/title_page.html

©2003 - 2012 Michael Ritter (tpeauthor@mac.com)
Last revised 6/5/12

 

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