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global wind systems answers 1. What wind systems move air from about 30° north or south latitude toward the equator? The northeast trade winds in the northern hemisphere and the southeast trade winds in the southern hemisphere. 2. Describe the movement of air in the huge convection current between 30° north latitude and the equator.
Using the image of the globe below, label the following wind patterns: 0°, 30°, 60°, 90° Latitude. Hadley cells. Ferrell cells. Polar cells. Northern trade winds. Southern trade winds.
Complete the following activities to identify patterns made by global winds. Activity 1 – Global Wind Cells Over the major parts of the Earth's surface there are large-scale wind circulations present. The global circulation can be described as the world-wide system of winds by which the necessary transport (movement) of heat from tropical to ...
Global Winds and Local Winds. BEFORE YOU READ. After you read this section, you should be able to answer these questions: • What causes wind? • What is the Coriolis effect? • What are the major global wind systems on Earth? What Causes Wind? Wind is moving air caused by differences in air pres-sure.
The low pressure wind belt located in equatorial regions is called the At 300 south of the equator, the pressure belt called the Air masses at the equator have pressure. pressure; air masses at the poles have About 190 north of the equator, the wind belt called Name the wind belt that would affect each of the following locations. a. Nome ...
This resource contains 1 worksheet for students to label the common/major parts of Global Wind Patterns and 1 worksheet to match Global Wind Pattern terms with their definitions. Answer key included. This resource can be used as an introduction to new material or a study guide for a quiz.
Lab Activity on Global Wind Patterns. 2002 Ann Bykerk-Kauffman, Dept. of Geological and Environmental Sciences, California State University, Chico * Objectives. When you have completed this lab you should be able to... 1. explain how convection redistributes atmospheric heat energy from the equator to the poles,
