Global Climate Patterns

Introduction

Climate refers to the average weather that occurs across the surface of the earth. Climates vary dramatically from one region of the earth to the next, ranging from the warm, humid conditions found along the equator, to the hot deserts and cold polar regions. Climates influence the growth of vegetation, the productivity of agriculture and the distribution of the human population. An understanding of global climate patterns provides a fundamental basis for studying world geography.

Learning Objectives

This activity is designed to help you learn the following:

Setup

In your browser, open the mapping program URL: http://geogserver1.fullerton.edu/webmaps/climatejava_2/climate.html
If the map fails to appear, try the alternate site http://geography.fullerton.edu/webmaps/climatejava_1/climate.html
When the map appears, resize the browser window to make the scroll bars disappear. Note: your browser must be Java-enabled for the program to work properly.

Overview of Global Climate Patterns

To begin your exploration of climate and geographic regions, bring up a map of the world’s major climate zones.

Geographers distinguish six general climate types:

When all six are viewed together on one map, the general geographic patterns can be difficult to discern. Instead, let’s look at maps of the individual types.

Humid Equatorial Climate Zones

Humid equatorial climates are marked by two dominant features:

There is little change in temperature from one season to the next, though there may be distinct wet and dry seasons.

Note the two large areas of Humid Equatorial Climates in South America and Africa. Let’s look first at Africa.

Information about the location you clicked on should appear in the lower right of the screen. You probably clicked on the country known until recently as Zaire – now known as the Democratic Republic of Congo. Much of the humid equatorial climate occurs in the Congo River Basin of the DR of Congo. Use the Scantron form to answer the numbered questions below:

    a. North Africa and Southwest Asia

b. South America

    c. Subsaharan Africa

d. South Asia

Nearly all the major geographic regions are associated with more than one climate type. Let’s overlay a map of the Subsaharan Africa region to see how well it matches the boundaries of the humid equatorial climate zone.

The northern boundary of the Subsaharan Africa region closely matches the northern boundary of the equatorial climate zone, but the southern boundary of the region does not. Restore a view of all climate zones to see which ones are found in southern Africa.

    a. Dry & Highland Climate

b. Humid Temperate & Dry

    c. Humid Temperate & Humid Cold

d. Humid Cold & Cold Polar Climate

    a. Northeast

b. Southeast

c. Southwest

    a. Brazil

b. Columbia

    c. Chile

d. Argentina

    a. Humid Temperate & Dry

b. Humid Cold & Dry

    c. Humid Temperate & Humid Cold

d. Humid Cold & Cold Polar

    a. Yes, the pattern is similar

    b. No, the pattern is very different

Dry Climate Zones

Dry climates are characterized by two fundamental features:

Let’s take a look at the geographic distribution of dry climates:

The map shows a large region of dry climates extending across northern Africa into southwest and central Asia. It also shows significant areas of dry climate conditions in North America, South America and Australia. Only Europe shows a lack of areas of dry climate. Let’s look first at northern Africa:

    a. Subsaharan Africa

    b. North Africa/Southwest Asia

    c. South Asia

Now add the boundaries of that region to your map:

The boundary between the Humid Equatorial climate of Subsaharan Africa with its abundant rainfall and the dry climate of North Africa with its low rainfall is a rather abrupt geographic boundary. This boundary is also reflected in the peoples and cultures of the region. These climatic and cultural differences are the main reasons why Africa has been separated into the two regions of North Africa/Southwest Asia and Subsaharan Africa.

Now add all the regions to the map to see if other regions are dominated by dry climates.

    a. Europe

b. North America

    c. Russia

d. Australia

    a. East Asia

b. South Asia

c. North America

Humid Temperate Climate Zones

The humid temperate climates can be characterized by their relative lack of extremes:

Let’s look at the map:

The pattern shows numerous areas of humid temperate climate scattered across each of the continents. Now add the regions to your map.

    a. North America

b. South America

    c. Europe

d. East Asia

    a. Southeast

b. Southwest

    c. Northeast

d. Northwest

    a. Canada & Korea

b. Canada & China

    c. US & China

d. Canada & Japan

Humid Cold Climate Zones

The humid cold climates are characterized by:

Take a look at the map:

Humid cold climates stretch across vast areas of northern North America, Europe and Asia. There are no areas of humid cold climates in the southern hemisphere because none of the three southern continents – South America, Africa, and Australia – extend far enough to the south.

In the northern hemisphere, the warmer southern margins of the humid cold climate zone support agriculture, but farther north the growing season is too short for farming.

Most of the area of humid cold climate occurs in two geographic regions. Add the regions to your map to see which ones these are:

    a. Russia

b. North America

    c. Europe

d. North Africa/Southwest Asia

    a. Europe & Russia

b. North America & Russia

    c. East Asia & Russia

d. South Asia & Russia

Cold Polar Climate Zones

The cold polar climate zones are characterized by one dominant feature:

Look briefly at the map:

One large area of blue stands out in the center of your map.

    a. Canada

b. Greenland

    c. Europe

d. Russia

You should have clicked on the island (inappropriately) named Greenland, a large area covered by glacial ice. Although it is close to North America, it is usually included in the Europe region because it is historically linked to the European country of Denmark.

Our world map doesn’t include the large continent of Antarctica that encircles the south pole. If it did, it would show an area of Cold Polar climate covered by glacial ice that is much larger than Greenland.

Highland Climate Zones

There is no one type of highland climate. Rather, highland climates represent the distortion of other climates due to elevation. Highland climates are generally cooler and wetter than the climates that occur in neighboring lowland regions.

Climate Controls

To complete our discussion of global climates, we need to consider some of the major earth processes that shape our long-term weather patterns. Although an in-depth explanation of climate processes lies outside the scope of an introductory course in world regional geography, there are two major principles you will need to know:

To illustrate the first point, we’ll take a brief look at climate zones which are strongly linked to latitude. To illustrate the second, we’ll consider examples of two additional influences: wind patterns and ocean currents. Our discussion of wind patterns will look at the summer monsoon of Asia. Our example of ocean currents will look at the North Atlantic Drift that flows across the Atlantic Ocean toward Europe.

 The Importance of Latitude

Latitude directly influences the amount of solar energy reaching any point on the earth’s surface over the course of the year. Let’s look at the map:

Note the four latitude zones in each hemisphere:

How do climate zones relate to these latitude bands?

On the map and you’ll see three climate zones that are have a strong west-to-east pattern.

    a. Humid Equatorial

b. Dry

    c. Humid Temperate

d. Highland

    a. Humid Temperate

b. Humid Cold

c. Cold Polar

    a. Humid Temperate

b. Humid Cold

c. Cold Polar

The Summer Monsoon of Asia

Some climates are not as closely linked to latitude. Lets look first at south and southeast Asia.

Now look at the northern portion of the tropical zone of Africa and Asia.

    a. Dry

b. Humid Equatorial

c. Humid Temperate

    a. Dry

b. Humid Equatorial

c. Humid Temperate

How do we explain this?

The blue arrows show how the atmospheric circulation over Asia in the summer draws a warm, humid, rain-producing Monsoon circulation into India and the other countries of South and Southeast Asia. Those wind patterns are absent over North Africa and Southwest Asia, resulting in extremely dry climates.

 The North Atlantic Drift

Now let’s look at the northern portion of the midlatitudes in the northern hemisphere.

    a. Humid Temperate

b. Humid Cold

    a. Humid Temperate

b. Humid Cold

How do we explain this difference?

The red arrows show the movement of a large warm water current from the tropical Atlantic and Gulf of Mexico northeastward to the shores of Europe. Winds moving across this warm current bring milder winter temperatures to Europe. As a result, the climate of western and central Europe is much milder than that found at the same latitude on the east coast of North America.

The summer monsoon of Asia and the North Atlantic Drift represent two of the many factors that influence the earth's climates. For a fuller discussion of climate, you would need to take a course in Physical Geography.

Review Questions Try to answer the following review questions without looking back at your answers or at the computer. If you don't remember, then look back to find the answers.

Exit the GIS Program

When you are finished:

Be sure to put you name on the completed Scantron form and hand it in to the lab instructor. Keep the activity questions.