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Chapter 15

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Chapter 15 The Atmosphere Atmosphere A mixture of gases composed of 78% nitrogen and 21% oxygen. Gravity holds the gases close to the Earth making it thicker ... – PowerPoint PPT presentation

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Title: Chapter 15


1
Chapter 15 The Atmosphere
  • Atmosphere A mixture of gases composed of 78
    nitrogen and 21 oxygen.
  • Gravity holds the gases close to the Earth making
    it thicker with higher pressure near the surface
    and thinner with lower pressure at higher
    altitudes.
  • The Layers of the Atmosphere
  • Troposphere the lowest, densest and closest
    layer to the surface of the Earth containing 90
    of the mass of the atmosphere.
  • Stratosphere the gases in this layer are thin
    and do not mix. Thin with very little moisture.
  • Mesosphere the coldest layer characterized with
    a decrease of temperature with increasing
    altitude (inverse relationship). This is the
    middle layer but also is one of the highest
    layers.
  • Thermosphere one of the highest layers
    containing too few air molecules to successfully
    transfer any thermal energy. Temperatures may
    reach 1000C.
  • Ionosphere composed of the upper mesosphere and
    lower thermosphere where nitrogen oxygen atoms
    absorb harmful solar radiation. These gas
    particles become electrically charged (ionized)
    and form the auroras when energized by solar
    particles. This layer also reflects radio waves
    back to the surface.

2
  • Atmospheric Heating
  • Energy from the sun reaches the Earths surface
    in the form of electromagnetic waves called
    radiation. Only about two billionths
    (2/1,000,000,000,000) of the suns energy ever
    reaches the Earths surface and half of that get
    absorbed by the water and land (50).
  • Thermal Conduction The transfer thermal energy
    through a conductive material. Similar to
    cooking. Heat is transferred from the flame to
    the pot to the food.
  • Convection The transfer of heat by the
    molecules of a liquid or a gas. The movement
    created when warm air rises and cold air sinks.

3
  • Greenhouse Effect The warming of the surface
    and lower atmosphere caused by water vapor,
    carbon dioxide, sulfur dioxide, nitric oxide
    (greenhouse gases) that absorb radiation and
    transfer the thermal energy to the surroundings.
  • Global Warming The unnatural, gradual average
    global temperature increase due to an increased
    concentration of greenhouse gases.
  • Global Local Winds
  • Wind The movement of air caused by differences
    in air pressure. The greater the pressure
    differential, the stronger the wind. Differences
    in air pressure are caused by the unequal heating
    of the Earths surface with warm air rising at
    the Equator and cooler air sinking at the Poles.
  • Convection (Hadley) Cells Large, circular
    patterns that the air travels in, separated by
    high and low pressure belts located about every
    30 latitude.
  • Coriolis Effect The curving of the Earths
    winds and ocean currents caused by the Earths
    rotation.

4
  • Global Winds
  • Polar Easterlies Winds that blow from the poles
    to 60 latitude.
  • Westerlies The flow of air to the poles from
    the west to the east. This is the opposite of the
    Trade Winds and blow from 30 to 60 latitude.
  • Trade Winds Winds that blow from 30 south
    latitude to 30 south latitude. Named by sailor
    who traveled from Europe to the Americas.
  • Doldrums Located at the Equator where the Trade
    Winds meet and rise creating a very calm center
    of low pressure.
  • Horse Latitudes A region located at 30
    latitude where the air sinks creating a high
    pressure, windless area. Many of the worlds
    deserts are located here.
  • Jet Stream A narrow band of high altitude, high
    speed winds that blow up to 400 km./hr. (240
    m.p.h.) in the upper troposphere and lower
    stratosphere.

5
  • Local Winds Winds that move air short distances
    and can blow from any direction. Can be created
    by a shoreline, mountain range or even a forest
    fire.
  • Mountain and Valley breezes Caused by
    differences in temperature created by changes in
    elevation. Valley breeze by day, mountain breeze
    by night. Breezes and winds are named by where
    they blow from.
  • Air Pollution The contamination of the air by
    pollutants from human and natural sources. Can
    cause coughing, headaches and lung cancers.
  • Primary Pollutants put directly from their
    source directly into the air. Car exhaust is the
    1 human primary pollutant.
  • Secondary Pollutants A primary pollutant that
    reacts with other pollutants to create a new
    pollutant such as ozone and smog.
  • Indoor air pollution is the result of the use of
    cleaners, heaters, dirty ductwork, chemicals from
    carpet, etc. Can be reduced with a proper
    ventilation system that mixes household air with
    outdoor air.

6
  • Acid Precipitation precipitation that contains
    acids from air pollution.
  • Acidification Acid precipitation changing
    the acidity of the water and soil causing harmful
    effects.
  • Acid Shock A rapid change of the acidity
    of a body of water killing fish and damaging eggs
    of fish and amphibians. Most harmful in our area
    with the spring thaw.
  • Ozone Hole Harmful effects of chemicals called
    CFCs (chlorofluorocarbons) that are breaking
    down the ozone (O3) into oxygen (O2) allowing
    harmful ultraviolet (UV) radiation to reach the
    Earths surface.
  • Cleaning Up Air Pollution
  • Allowance Trading System Limits the amount
    of pollutants that a company can release.
  • Hybrid Cars Uses both gasoline electric
    power.
  • Scrubbers Devices that remove some
    pollutants before they are released into the air.
    Usually mounted on the tops of smokestacks.
  • Cleaner fuels, catalytic converters, more
    efficient auto engines, etc.
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