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Chapter 22.1 Characteristics of the Atmosphere What is the Atmosphere? Atmosphere – the layer of gases that surrounds the Earth. The Two Functions of Our Atmosphere: 1. To protect the Earth’s surface from the Sun’s radiation. 2. To regulate the temperature of the Earth’s surface. Chemical Composition of the Atmosphere Abundant Elements Nitrogen Oxygen Argon Abundant Compounds (More than one element) Carbon dioxide (CO2) Water Vapor (H2O) Other Components Dust Pollen Nitrogen in the Atmosphere Nitrogen leaves the atmosphere and enters the soil where it is “fixed” into usable compounds by nitrogen fixing bacteria in the soil and on the roots of plants called legumes (ex. soybeans and peanuts). Nitrogen compounds are returned to the soil through animal waste and the decay of dead organisms. Nitrogen is released back into the atmosphere by the decay of dead organisms. Nitrogen makes up 78% of the Earth’s atmosphere. Oxygen in the Atmosphere Oxygen makes up 21% of the Earth’s atmosphere. Ways That Oxygen is Taken Out of the Air: 1. The “life processes” of animals, bacteria, and plants (i.e. 3. Respiration) 2. Burning (ex. forest fires, fossil fuels) The weathering of certain kinds of rock (and soil … especially those rich in iron i.e. Oxidation) Processes That Put Oxygen Into the Air: 1. Photosynthesis Respiration Photosynthesis Photosynthesis and Respiration: In Simple Terms It should be noted that almost all living things, including plants, undergo aerobic respiration. Respiration – the process whereby oxygen (O2) is used to release the energy stored in food, producing carbon dioxide (CO2) and water vapor (H2O). Photosynthesis – the process whereby green plants, algae, and certain protests use sunlight, carbon dioxide (CO2), and water vapor (H2O) to produce food and oxygen (O2). Photosynthesis and Respiration: Inside the Cell The Oxygen-Carbon Dioxide Cycle Part 1 The Oxygen-Carbon Dioxide Cycle Part 2 Water Vapor in the Atmosphere The Two Process That Put Water Vapor Into Air Are: 1. Evaporation 2. Transpiration (from plants) The Two Process That Take Water Vapor Out of Air Are: 1. Condensation 2. Precipitation Based on the time of day, location, and season, water vapor in the atmosphere can vary from as low as 1% to as much as 4%. Ozone: Important Substance in the Atmosphere Ozone (O3) is a form of oxygen found in the stratosphere. Before Earth had an ozone layer, all life lived under the oceans … NONE could live above them! Ozone absorbs harmful ultraviolet radiation (UV rays) coming from the sun. Ultraviolet radiation can cause severe burns, cancers, mutations, and even death!). Ozone can be destroyed by: CFC propellants in old aerosol spray cans, Freon coolant from refrigerants in old refrigerators and air conditioners, and nitrogen oxide exhaust gases from burning supersonic aircraft fuel. Ozone: a Little Chemistry Ozone is created when ultraviolet radiation (UV rays) from the Sun strikes and splits oxygen molecules (O2) to atomic oxygen (O). The atomic oxygen (O) quickly combines with further oxygen molecules to form ozone (O3): O2 + light -> O + O2 -> O + O (1) O3 (2) It should be noted that ground level ozone, which is produced by hydrocarbons that react with sunlight, is a pollutant itself. Ground level ozone causes SERIOUS lung irritation!!! Dust In The Wind… Particulates – tiny solid particles in the air. Sources of Atmospheric Particulates: Dust from volcanic eruptions Ash from fires Microscopic organisms Minerals lifted from soil by winds Pollen from plants Particles from meteorite impacts Salt from sea spray The tinier the particle, the longer it can stay suspended in the air. What is Atmospheric Pressure? Atmospheric pressure – the force per unit area that is exerted on a surface by the weight of the atmosphere. 99% of the mass of the atmosphere is located within 32 km (20 miles) of the Earth’s surface. The general trend between atmospheric pressure and altitude is that, the higher up in the atmosphere one goes, the less atmospheric pressure there will be. altitude pressure A you go up in the atmosphere, the air gets thinner and therefore there is less pressure. That is why ears pop when ascending and descending in an airplane! Measuring Atmospheric Pressure Measuring atmospheric pressure: Barometer – a device used to measure atmospheric pressure. There are two types of barometers: Mercury Barometer – a barometer that works when air pushes down on a pan of mercury forcing the mercury to rise up a calibrated, inverted tube. Aneroid Barometer – a barometer that works when air pressure squeezes on the sides of a can moving an attached pointer. Standard air pressure at sea level can be expressed as one atmosphere, 760 mm of mercury, or 1000 mb. Since air pressure decreases with increasing altitude, an aneroid barometer can be calibrated to read altitude. However, to function accurately, altimeters must be kept calibrated for local weather conditions. Layers of the Atmosphere 1 Did you know… Mount Everest, the highest elevation above sea level, is only about 8.8 km high, keeping it in the bottom layer of the atmosphere. The Earth's atmosphere is composed of several layers: We live in the Troposphere where almost all weather occurs (ex. wind, clouds, fog, rain, hail, sleet, snow and storms). Above the Troposphere is the Stratosphere, which contains the Ozone Layer, which blocks out harmful UV rays. Commercial airliners (ex. a 747) usually fly in the troposphere, whereas supersonic jet airliners (ex. the Concorde) fly in the lower stratosphere. Layers of the Atmosphere 2 Thermosphere Lower region called ionosphere. Upper region called exosphere. Nitrogen and oxygen atoms absorb deadly gamma and X rays here, explaining the unexpected increase in temperature. Mesosphere Coldest layer of the atmosphere. Temperature within this layer decreases as altitude increases. Stratosphere The Ozone Layer absorbs harmful UV Rays here, explaining the unexpected increase in temperature. Troposphere All weather change occurs here. Temperature within this layer decreases as altitude increases because there is an increase in distance from the warming effect of sunlight absorbed by the Earth’s surface. Air Pollution … aka Smog The greatest source of air pollution today is from the burning of fossil fuels which releases pollutants such as sulfur dioxide gas (SO2), hydrocarbons, nitrogen oxides (NO), carbon monoxide (CO), and lead (Pb) into the air. Temperature inversion – a condition in which a layer of colder, polluted air is trapped below warm air and when then cannot disperse causing smog to form. Rain Gone Bad … Acid Rain!!! All rain is somewhat naturally acidic!! But when chemicals from car and factory exhaust (CO, CO2, NO, NO2, SO, SO2) combine with rainwater, they can produce HIGHLY acidic rains that damage buildings and monuments and kill plants and fish. Who is a Meteorologist? A meteorologist studies all characteristics of the atmosphere, weather, and climate. Meteorologists can specialize in areas such as agriculture, aviation, forestry, or health. http://www.nws.noaa.gov/ http://66.208.12.20/amsedu/dstreme/ http://www.weather.com/index.html http://www.wqad.com/ http://www.kwqc.com/ Weather vs. Climate Weather – the general condition of the atmosphere at a particular time and place (i.e. temperature, air movements, and air moisture). Climate – general weather conditions over many years. The End!... Up Next … Light and the Electromagnetic Spectrum …