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2 The Stratosphere and the Figure 1 Variation of temperature bottomaxis and ozone top axis with altitude fromthe surface of the Earth In the tropospheretemperature decreases with altitude In. Students m ust read the background material plot data points and determine where layers begin and end from their comprehension of the reading material Grade Level 10 Time Required 35 45 minutes Materials No additional materials are needed Backgroun Controlled atmosphere storage refers to the constant monitoring an d adjustment of the CO and O levels within gas tight stores or containers The gas mixture will constantly change due to metabolic activity of the respiring fruits and vegetables in t characters or a "This can be a rare, yet costly problem and you want to know, Then click on the fly drop down window.below.If there is a “” next to the word “Ligatures” then you ne Key Terms. Atmosphere. – a thin envelope of gases that encircles the earth and other particles (aerosols). Weather. – the state of the atmosphere at a specific place and time. Meteorology. – the study of the atmosphere and the processes that cause weather. Atmospheres. Atmospheric compositions. Venus – . CO. 2. (96.5%), . N. 2. (3.5%), SO. 2. (0.015%). Mars -- . CO. 2. (95.3%), . N. 2. (2.7%), Argon (1.6%), O. 2. (0.13%). Earth – N. 2. (78.1%), O. Lesson Objectives. Describe how the temperature of the atmosphere changes with altitude.. Outline the properties of the troposphere.. Explain the role of the ozone layer in the stratosphere.. Describe conditions in the mesosphere.. Definition of the Atmosphere. . The layer of gases surrounding Earth; composed mainly of 78% nitrogen and 21% oxygen, and other gases (water vapor, dust, pollutants, etc.). Brainpop: . Earth’s atmosphere. Earth’s . protective bubble. NASA accessed via Wikipedia . compared to the size of the Earth (10. 4. km), the atmosphere is a thin shell (120 km).. . Earth’s Atmosphere. http://www.gsfc.nasa.gov/gsfc/earth/pinatuboimages.htm. II 2017. a. aron.hill@ttu.edu. Weather Is Everywhere. University Studies/Global Studies. Climate change protocols. Fossil fuel consumption/climate change. R. enewable energy reliance. Business/Finance/Marketing/Commerce. GLY 4241 - Lecture 6 . Fall, . 2016. 2. Earth. Even in a high resolution image from space, the atmosphere is not visible. 3. Radiation. NASA graphic. 4. Chinese Smog. Haze over China. Increased desertification has added dust to China’s atmosphere. La gamme de thé MORPHEE vise toute générations recherchant le sommeil paisible tant désiré et non procuré par tout types de médicaments. Essentiellement composé de feuille de morphine, ce thé vous assurera d’un rétablissement digne d’un voyage sur . Section 11.2 – Properties of the Atmosphere 8 th Grade Earth and Space Science Class Notes Temperature Temperature – measure of the average kinetic energy of the particles in a material Higher the temperature = faster particle movement ATMOSPHERE Composition of the Atmosphere The atmosphere is comprised of a variety of gases: Major Constituents (99%): Nitrogen (N): 78% Oxygen (O 2 ): 21% Trace Constituents: Other: 1% In fact, the atmosphere receives very low amount of heat energy from the sun as it receives most of its energy from the long wave terrestrial radiation.. Atmosphere receive energy from the sun and the earth in different ways. .