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See more ideas about architecture presentation, architecture drawing, diagram architecture. The pre-designed Global Circulation PPT template is 100% customizable. This means you can mold every slide to showcase what you want in front of your audience. With just a few clicks, you'll be able to ensure this set matches your style.
When the air reaches the equator, it is lifted vertically by the processes of convection and convergence . Even with disruptions like weather fronts and storms, there is a consistent pattern to how air moves around our planet’s atmosphere. This pattern, called atmospheric circulation, is caused because the Sun heats the Earth more at the equator than at the poles. A recurring theme within the #geographyteacher community on Twitter is about how to teach the global atmospheric circulation model.
The page references refer to the Oxford textbook. Designed for the AQA 9-1 Syllabus. Editable word document and PDF version included.
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For one, it is vital to the transport of heat around the globe, bringing warm water towards the poles, and cold water to the tropics, stabilizing temperature in both environments. Global Wind Patterns wind belts of the general circulation The global wind pattern is also known as the "general circulation" and the surface winds of each hemisphere are divided into three wind belts: Polar Easterlies: From 60-90 degrees latitude. Prevailing Westerlies: From 30-60 degrees latitude (aka Westerlies). Designed to help summarise the key features of the global circulation model.
Circulation Atmosphere Global Circulation Patterns
The accompanying diagram (Figure 1) will show how variations in temperature cause updrafts, downdrafts, surface winds and upper air winds. It is important to know that some additional factors are critical in understanding the circulation of air in our atmosphere. They will be covered in this chapter as well. 2017-01-20 · During the first half of the lesson students were asked to annotate a diagram of global atmospheric circulation, which I had introduced them to step by step on the whiteboard (available below). The labels students used to annotate the diagram included key characteristics such as convection cells, trade winds, precipitation as well as areas of low and high pressure.
Match The Lettered Zones (A, B, C, And D) In The Global Circulation Diagram ( above) To The Correct Pressure Belt (listed Below).
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As described in the diagram above, surface air flow is from the poles to the equator. When the air reaches the equator, it is lifted vertically by the processes of convection and convergence .
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Global Atmospheric Circulation Labelled Diagram - Märkt
When it reaches the top of the troposphere, it begins to flow once again horizontally. The global circulation. 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 of heat from tropical to polar latitudes is accomplished. The accompanying diagram (Figure 1) will show how variations in temperature cause updrafts, downdrafts, surface winds and upper air winds. It is important to know that some additional factors are critical in understanding the circulation of air in our atmosphere.