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Section 13.4 The Atmosphere On top of the world Summit On top of the world Version 2.0 Felix Baumgartner Properties of the Atmosphere Blanket of air and moisture that surrounds the earth. Extends about 500km above the earth. Most dense at sea level. Density decreases as elevation increases. (Particles become further apart) Layers of the Atmosphere Layers of the Atmosphere The atmospheric layers differ in: altitude (height above sea level) Temperature Composition pressure Layers of the Atmosphere Atmospheric layers are thicker above the equator than at the poles Warm air expands and cool air contracts It is warmer at the equator so it takes up more volume. Layers of the Atmosphere Use your text pages 510-511 and Figure 3 to add details to the Atmosphere Layers handout. Troposphere . 9 Stratosphere 10 Mesosphere 11 Thermosphere 12 Thermosphere 13 Exosphere 14 How does the Atmosphere support life? How does the Atmosphere support life? 1. Provides oxygen and nitrogen required for basic life functions How does the Atmosphere support life? 2. Has carbon dioxide needed by plants in photosynthesis How does the Atmosphere support life? 3. Protects the earth from harmful radiation How does the Atmosphere support life? 4. Regulates temperature by trapping heat and moving it from one place to another. http://earth.nullschool.net/ How does the Atmosphere support life? 5. Involved in the water cycle, and all organisms need water. How does the Atmosphere support life? 6. Burns up asteroids preventing many dangerous collisions. Atmospheric Pressure The force the air exerts on objects as gravity pulls it towards the center of the earth Greatest at sea level since the height, and therefore weight, of the atmosphere is greatest. Atmospheric Pressure As altitude increases (climbing mountain) the weight of the air above is less and pressure is less. Atmospheric Pressure Another factor that affects atmospheric pressure is whether the air is rising or falling. Rising air has less pressure than falling air. Measuring Pressure (Units) Atmospheric pressure (also called barometric pressure) is measured with a barometer. Pressure is most often measured in Kilopascals (kPa) Kilo = 1000 1KPa = 1000 pascals (Pa) 100 KPa = 100 000 Pa You may also hear of pressure in Atmospheres (atm) or millibars (mb) Measuring Pressure (Units) Samples: 1) Convert 54 kPa to Pa. 2) 757840 pascals to kilopascals Answers 1) 54000 Pa 2) 757.840 kPa Measuring Pressure (Units) Standard Atmospheric Pressure is the normal atmospheric pressure at sea-level. It is assigned a value of 101.3kPa. Low Pressure systems have a pressure less than 101.3 kPa High pressure systems have a pressure above 101.3 kPa We will learn shortly how air pressure actually affects weather. It is very important. Pressure Gradient A measure of how the atmospheric pressure changes across the earth's surface This change can be either vertical or horizontal. Vertical is like how it changes with altitude. Horizontal pressure gradients can be shown on a map by joining points of equal atmospheric pressure. They can then be used to predict where high and low pressure areas are and the direction and strength of winds. Wind moves from high pressure to low pressure. C B A Temperature Gradient Clouds