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1 What Makes Up Earth’s Atmosphere? Study Guide The layer of air that surrounds our planet is called the atmosphere. When compared to the size of Earth, the atmosphere looks like a very thin blanket surrounding the entire planet. So, we say that the atmosphere is a thin blanket of air that surrounds Earth. Our atmosphere formed millions of years ago as gases from erupting volcanoes collected around the planet. Over time, the gas mixture changed slowly to become the atmosphere Earth has now. The atmosphere now is made up of billions and billions of gas particles – nitrogen, oxygen, water vapor and other gases. Plants use carbon dioxide during the process of photosynthesis. Plants give off oxygen as photosynthesis occurs. Carbon dioxide also absorbs heat energy from the sun and from Earth’s surface. This helps keep the planet warm. Water vapor can absorb energy, too. The amount of water vapor in the air varies from place to place. Air over bodies of water usually contains more water vapor than air over land. High in the air, water vapor condenses to form clouds (condensation). All particles of air pressing down on the surface cause air pressure. Air pressure changes as you go higher in the atmosphere. At the surface of Earth, air particles are close together. The higher you go in the atmosphere, the farther apart the air particles are. So the air pressure is less as you go higher in the atmosphere. (more on back) 2 Atmosphere Layers Earth’s atmosphere is divided into four layers: troposphere, stratosphere, mesosphere, and thermosphere. The layer closest to Earth is the troposphere. We live in the troposphere and breathe its air. Almost all bad weather happens in this layer of the atmosphere. In the troposphere, air temperature decreases as you go higher. The second layer from Earth is the stratosphere. Some airplanes that travel long distances fly in the stratosphere to be above most bad weather. The stratosphere contains most of the atmosphere’s ozone, a kind of oxygen. The ozone protects living things from the sun’s harmful rays. Temperatures in the stratosphere increase with height. The third layer from Earth is the mesosphere. In the mesosphere, air temperature decreases with height. In fact, the mesosphere is the coldest layer of the atmosphere. The fourth layer from Earth is the thermosphere. The thermosphere is the hot, outermost layer of air. In the thermosphere, temperature increases quickly with height. Temperatures high in the thermosphere can reach thousands of degrees Celsius. (Harcourt Science D6-8)