Our Early Atmosphere

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Our Early Atmosphere The Earth’s physical features are what affect our daily lives and how we live them. But it’s what people don’t see that affects them the most, the atmosphere. This is the gaseous mass or envelope surrounding a celestial body, and retained by the celestial body's gravitational field. It’s an invisible shield that protects us from many harmful things and keeps our planet in balance. Our atmosphere is about 300 miles thick and is made up of many gaseous chemicals: 78% nitrogen, 21% oxygen, 0.9% argon, 0.03% carbon dioxide, and trace amounts of other gases. There is no actual place where the atmosphere ends in space, it just slowly gets thinner the farther you travel away from Earth. As you move closer to Earth the air gets thicker thus the air pressure rises. At sea level, the air pressure is about 14.7 pounds per square inch. Depending where you are and what altitude you are at greatly varies in the atmosphere so it is divided into five layers: the Troposphere, Stratosphere, Mesosphere, Thermosphere, and the Exosphere. The Troposphere is the lowest layer, it extends from the ground to around 12 miles up. Also, it is the warmest being closest to the surface where air is the most dense. All weather happens in this layer because evaporated water only reaches to about 50,000 feet above sea level. At 31 miles you run into the Stratosphere. The height of this layer relies on the latitude and the seasons. Our main protector, the Ozone layer is in the Stratosphere. Contrary to what people think the temperature actually goes up as you ascend. This is because of the Ozone layer which is heated when it absorbs the Ultraviolet Radiation of the Sun. Chemicals can stay in this layer for a long period of time due to vertical convection. This is the main problem for the depletion of the Ozone layer. The next layer is the Mesosphere.
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