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The Atmosphere Chapter 15 Page 392 – 419 Page 394 Characteristics of the Atmosphere Atmosphere = a mixture of gases that surrounds the Earth. • It protects us from the sun’s harmful rays. • It is always changing. Every breathe we take, every tree we plant, and every motor vehicle we ride in affects the composition of the atmosphere Pages 394 – 395 Composition of the Atmosphere ≈ 78% of the gases in the atmosphere. It is released by volcanic eruptions & when dead plants & animals decay. Nitrogen ≈ 21% of the gases in the atmosphere. It is produced mainly by plants. Oxygen The remaining 1% of the atmosphere is made up of argon, carbon dioxide, water vapor, & other gases. Besides gases in the atmosphere there are also small amounts of solids & liquids. Pages 395 – 396 Atmospheric Pressure & Temperature Air pressure = the measure of the force with which the air molecules push on a surface. Air pressure, temperature, & the kinds of gases present change through out the atmosphere. Pressure Altitude = the height of an object above the Earth’s surface. As altitude increases, air pressure decreases. Air Temperature Air temperature varies depending on the way solar energy is absorbed as it moves downward through the atmosphere. Page 396 Layers of the Atmosphere Based on temperature the Earth’s atmosphere is divided into four layers: • Troposphere • Stratosphere • Mesosphere • Thermosphere Each layer has unique characteristics Page 397 Troposphere = lowest densest part of the Earth’s atmosphere in which most weather changes occur; temperature generally decreases rapidly with altitude & it extends from the Earth’s surface to the bottom of the stratosphere. Stratosphere Stratosphere = air is thin & contains little moisture; temperature is cold (-60oC) but rises with altitude Ozone = O3 molecule; Almost all ozone in the atmosphere is contained the ozone layer. This layer absorbs solar energy in the form of ultraviolet radiation which protects life on Earth. Troposphere Pages 398 – 399 Mesosphere Mesosphere = coldest layer; temperature drops as altitude increases (as low as -93oC). Scientists recently discovered wind storms in the mesosphere. Thermosphere Thermosphere (ionosphere) = uppermost layer; temperature increases with altitude (as high as 1,700oC); nitrogen & oxygen absorb harmful solar radiation which causes them to become ionic in nature & reflect light & radio waves (Northern lights). There is no definite boundary between the atmosphere and space. In the upper thermosphere, the air becomes thinner & thinner, eventually blending into space. Pages 400 – 401 Heating of the Atmosphere The Earth’s atmosphere is heated by transfer of energy from the sun. Energy in the Atmosphere The Earth receives energy from the sun in the form of radiation. Primary types of radiation reaching the Earth’s surface from the sun are known as visible light. When radiation is absorbed, its energy is changed into heat. The Earth’s surface is heated as it absorbs energy from the sun. The Earth transfers energy to the lower atmosphere, heating it, & causing convection. Page 401 Moving the Energy Around Most heat in the atmosphere moves by convection, but it is only one of many processes responsible for redistributing energy on the Earth. Once incoming solar radiation passes through the atmosphere & is absorbed by the Earth’s surface the energy is transferred to the atmosphere by: • Evaporation of surface water & its condensation in the atmosphere • Emission of infrared waves, which are then absorbed by atmospheric gases • Conduction as cool air comes in contact with warm surfaces. Pages 402 – 403 The Greenhouse Effect Greenhouse effect = process in which the gases in the atmosphere trap thermal energy Global Warming Global warming = rise in the average global temperatures Keeping the Earth Livable radiation balance – the amount of solar energy received & the amount of thermal radiation returned to space. Some scientists argue that humans are responsible for the increased temperatures on Earth today Others argue that it has gone through warm periods before people ever walked the Earth. Pages 404 – 405 Atmospheric Pressure & Winds Wind = moving air Why Air Moves Wind is created by differences in pressure. These differences in air pressure are caused by the unequal heating of the Earth. • Colder, more dense air is heavier & sinks = high pressure. • Air moves from high pressure to low pressure The speed of the wind is determined by the pressure difference between the area of high pressure & the area of low pressure. Page 405 The Pressure Belts uneven heating of the Earth produces pressure belts. These belts occur at about every 30o of latitude. Coriolis Effect The movement of wind is affected by the rotation of the Earth so winds don’t blow directly north or south. Northern Hemisphere they curve to the right Southern Hemisphere they curve to the left Page 406 Types of Winds winds – generally move short distances & can move in any direction. Local winds –These travel longer distances than local winds & travel in a specific direction because they are part of a pattern of air circulation that moves across the Earth. Global Lets take a look at some global winds before we look at local winds Pages 406 – 407 Trade Trade Winds winds = in both hemispheres, the winds that blow from 30o latitude to the equator • Northern Hemisphere they blow from the northeast to the southwest • Southern Hemisphere they blow from the southeast to the northwest. Early traders used these winds to sail from Europe to the Americas. Page 407 Westerlies Westerlies = wind belts found in both the Northern & Southern Hemispheres between 30o & 60o latitude. These winds flow toward the poles in opposite directions form the trade winds. • Northern Hemisphere they blow from the southwest to the northeast • Southern Hemisphere they blow from the northwest to the southeast. These winds helped sailors return to Europe. Page 407 Polar Easterlies Polar Easterlies = wind belts that extend from the poles to 60o latitude in both hemispheres. These are formed from cold, sinking are moving from the poles toward 60o N & 60o S latitude. • Northern Hemisphere they blow from the northeast to the southwest • Southern Hemisphere they blow from the southeast to the northwest. Page 408 Jet Jet Stream stream = narrow belts of high-speed winds that blow in the upper troposphere & lower stratosphere over both the Northern & Southern Hemispheres. These winds often change their speed & can reach a maximum speed of 500km/h. Unlike other winds these don’t follow regular paths around the Earth but change both their latitude & altitude. Pages 408 – 409 These • • Local Winds are influenced by the geography of an area. Mountains or shorelines → cause temperature changes that cause land & sea breezes. Mountains or shorelines → during the day a gentle breeze to flow up the slope & at night cold air flows downslope & settles in the valley. Page 410 The Air We Breathe Cities produce pollution. Even as far back as the Roman Empire cities were producing large amounts of pollution. Air Quality Natural air pollutants include dust, sea salt, volcanic gas & ash, smoke from forest fires, pollen, swamp gas, & many other matters Human-caused air pollutants are most concentrated in cities. The more people the more pollution there is. Page 411 Types of Air Pollution Primary pollutants = pollutants that are put directly into the air by human or natural activity. • Exhaust from vehicles, ash from volcanic eruptions, & soot from smoke Secondary pollutants = pollutants that form from chemical reactions that occur when primary pollutants come in contact with other primary pollutants or with naturally occurring substances such as water vapor. • Automobile exhaust & ozone react in sunlight & become smog Page 412 Sources of Human-Caused Air Pollution source is transportation – cars contribute ≈ 60% of the human-caused air pollution in the US. Industrial Air Pollution ≈ 96% of the sulfur oxides released into the air is given off by industrial plants & electric power plants. The chemicals used by oil refineries, chemical manufacturing plants, dry-cleaning businesses, furniture refinishers, & automobile shops all add poisonous fumes to the air. Major Page 412 Indoor Air Pollution Air pollution is not limited to outdoors. Our homes, schools, & buildings have air pollution too. Sometimes the air inside a building is even worse than the air outside. What contributes to air pollution inside: • Household cleaners, air fresher's, smoke from cooking, & industrial compounds found in carpets, paints, building materials, & furniture Page 413 The Air Pollution Problem Pollution is both a local & global problem because winds can move pollutants from one place to another. Acid precipitation = precipitation, such as rain, sleet, or snow, that contains acids from air pollution. The Ozone Hole In the 1970s scientist determined that some chemicals being released were reacting with the ozone in the ozone layer & creating a hole. Page 414 Effects on Human Health Daily exposure to even small amounts of air pollution can cause serious health problems. Children, elderly people, & people with allergies, lung problems & heart problems are especially vulnerable to the effects of pollution. It can cause: • Dizziness, headaches, runny nose, sore throat, burning, itching eyes, coughing & trouble breathing, lung cancer & other lung diseases, chest pains, increased colds, & allergies. Page 414 Cleaning Up Our Act 1970 Clean Air Act gives the EPA authority to control the amount of air pollutants that can be released from any one source. It checks the air quality & if it worsens then the EPA can set stricter guidelines. Page 415 Controlling Air Pollution from Vehicles EPA requires certain standards from car manufactures. • New cars now have device on the tail pipe that removes most of the pollutants before exhaust is released. • Cars are also moving away from gasoline as a fuel source. Controlling Air Pollution from Industry Clean Air Act requires the Industry to use scrubbers. Scrubber = a device that attaches to smokestacks to remove some of the more harmful pollutants before they are released into the air.