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Atmosphere in Motion Chapter 12 By Amy Johnson Atmosphere  gases surrounding the Earth – necessary for supporting life – protects against harmful UV and X-ray radiation – absorbs and distributes warmth Galileo Galilei  proved air must have weight and contain matter – Weighed flask, injected air, and reweighed to find flask with injected air weighed more  Air stores and releases heat, holds moisture, and can exert pressure Composition of Atmosphere  subject to the pull of gravity – exerts pressure in all directions, therefore cannot be felt – weight is equal to water over 10 m deep  mixture of gases, liquid water, and microscopic particles of solids and other liquids Gases of the Atmosphere Nitrogen – most abundant (78%)  Oxygen – necessary for human life (21%)  Variety of other gases in trace amounts  – water vapor is critical to weather (up to 4%) » Responsible for clouds and precipitation – carbon dioxide allows plants to make food (.03%) » Absorbs heat and emits it back to warm Earth Aerosols in the Atmosphere  solids, such as dust, salt, and pollens and tiny droplets of acid – dust comes from volcanoes and wind blowing across the soil – salt results from wind blowing over the ocean – pollen is released by plants – burning coal in power plants also creates aerosols Layers of the Atmosphere based on temperature changes that occur with altitude  Lower Layers – Troposphere – Stratosphere  Upper Layers – Mesosphere » Ionosphere – Thermosphere – Exosphere Troposphere closest to the Earth (about 10 km)  contains about ¾ of Earth’s entire atmosphere including clouds and weather  about 50% of Sun’s energy passes through  Earth’s surface heats by conduction  – the farther from the surface you get, the cooler it becomes Stratosphere above troposphere (10 km – 50 km)  contains most of the ozone  – Absorbs ultraviolet radiation to warm area » As you go up, you get warmer – without ozone, the UV radiation would reach Earth and cause health problems Mesosphere Extends 50km – 85km above surface  Contains very little ozone so temperature drops to the lowest in atmosphere  Ionosphere part of mesosphere and thermosphere  due to intense interaction with the sun’s radiation  reflects AM radio waves allowing longdistance communications possible  – static results when interaction between this layer and radiation is too active Thermosphere reaches 85km – 500km  temperatures increase rapidly  filters out harmful X-rays and gamma rays from the Sun  Exosphere outermost layer  extends outward to where space begins  – no clear boundary to space GREENHOUSE EFFECT Earth’s Water 70% of Earth’s surface is water  Stored throughout the land-oceanatmosphere system in three different states  – Solid – snow, ice, glaciers – Liquid – oceans, lakes, rivers – Gas – water vapor  Water Cycle