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Energy in Atmosphere

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Title: Energy in Atmosphere


1
Energy in Atmosphere
2
Part 1. Atmosphere Formation
  • Ancient volcanic eruptions released gases into
    atmosphere
  • Ammonia, Nitrogen, CO2, CO, Sulfur, Methane,
    Hydrogen
  • Water was formed (meteorites released water when
    collide w/ Earth)
  • Algae formed in oceans
  • Photosynthesis uses CO2 to make O2
  • O2 diffuses into atmosphere
  • Ozone layer is formed (O3)

3
Part 2 Air Pressure
  • Force exerted by the weight of air
  • Measured with a barometer
  • Air Pressure at sea level
  • 1 atmosphere
  • 15 lbs per sq. inch
  • 30 inches of mercury
  • 760 mm of mercury
  • 1013 millibars (mb)

4
Part 2 Air Pressure
  1. As altitude increases, air pressure decreases
  2. As temperature increases, air pressure decreases

5
Part 3 Composition of Atm
  • Nitrogen 78
  • Oxygen 21
  • Argon .4
  • Greenhouse Gases absorb Infrared (warming)
    radiation
  • CO2
  • Water Vapor
  • Chlorofluorocarbons (CFCs)
  • Methane
  • Ozone filters out UV (skin cancer) radiation

6
Part 4 Energy
  • Energy is transferred from warmer to cooler
    substances
  • Heat Source warmer
  • Heat Sink cooler
  • Temperature
  • Average Kinetic Energy of the particles in a
    substance
  • Higher Temp faster moving particles

7
Part 5 Heat Transfer Methods
  • Conduction
  • Contact between hot substance and cooler
    substance (touching)
  • Curling Iron
  • Convection
  • Heated material rises b/c it has a lower density
  • Happens in liquids and gases

8
Water loses heat to air becoming cooler and more
dense
Heated water rises
Cooler water sinks
Water is heated, becomes less dense
Convection Cell one cycle Convection Current
2 or more cycles
9
Part 5 Heat Transfer Methods
  • Radiation
  • Energy transfer by waves of energy
  • Suns energy to Earth
  • Example
  • Light Bulb
  • Microwave

10
Part 6 Electromagnetic Radiation
  1. Vibrating particles have electrical charges that
    also vibrate forming electromagnetic waves

11
Part 6 Electromagnetic Radiation
  • Frequency
  • Number of crests passing a point in one second
  • Hertz (Hz) is unit for frequency
  • As wavelength gets longer, freq gets smaller

12
Electromagnetic Radiation
13
Part 7 Electromagnetic Spectrum
  1. Each form of energy has a specific frequency and
    wavelength
  2. ALL forms travel at speed of light 186,000
    miles/sec or 3x108 m/s
  3. Visible Light maximum intensity
  4. When waves are absorbed and then re-radiated
    (given off), they have longer wavelengths

14
Part 8. Heating of Land and Water
  • Land absorbs heat energy FASTER and cools FASTER
    than water
  • Reasons for Results
  • Land is darker and rougher, so it is a better
    absorber and radiator of energy
  • Water has a higher specific heat so it heats and
    cools more slowly

15
Heating of Land and Water
  • Effects on Earth due to different heating rates
    of land and water
  • Climate
  • Cooler summers near water
  • Warmer winters near water
  • Water causes areas near water to have small
    seasonal changes and temperature ranges

16
Heating of Land and Water
  • Air above surface
  • Air is mainly heated by energy re-radiated from
    surface (terrestrial radiation) infrared
    radiation longer wavelengths
  • Since land gives off energy faster, air over land
    heats and cools faster than air over water

17
Part 9. World-Wide Air Circulation
  • Coriolis Effect
  • Apparent bending of wind b/c of the rotation of
    the Earth
  • Northern Hemisphere wind curves to RIGHT
  • Southern Hemisphere wind curves to LEFT
  • Coriolis effect influences wind direction.

18
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19
Part 10. Insolation
  • Greenhouse Effect
  • Process to heat the atmosphere
  • Earth absorbs radiation from Sun
  • Energy is re-radiated to the atmosphere with a
    longer wavelength (infrared)
  • Infrared radiation gets absorbed by gases (CO2
    and water vapor) and remains trapped in atmosphere

20
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21
Part 11. Insolation Temperature Lag
  1. Suns energy is first absorbed by Earths
    surface, then given off as infrared radiation
    which warms the air
  2. There is a time difference (lag time) between
    greatest intensity of insolation and the time of
    highest temp
  3. Also true for lowest intensity and temp

22
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23
Part 12. Measuring Temp and Heat
  • Temperature
  • Measures the average Kinetic Energy of molecules
  • Water
  • Celsius 100 º boils, 0 º freezes
  • Fahrenheit 212 º boils, 32 º freezes
  • Kelvin 373 º boils, 273 º freezes, 0 º absolute
    zero
  • Absolute Zero
  • Coldest possible temp, molecules stop moving, no
    KE
  • -273 º C, -459 º F or 0 º K

24
Part 12. Measuring Temp and Heat
  • Heat
  • Measures the TOTAL amount of ALL Kinetic Energy
    in all molecules of substance
  • Measured in joules

25
Part 12. Measuring Temp and Heat
  • Specific Heat
  • Amount of heat needed to raise one gram of a
    substance 1 º C
  • Specific Heat of Water 4.18 joules/gºC
  • Lower the specific heat, the faster something
    will heat up or cool off.

26
Part 13. States of Matter
  • Solids
  • Particles close together, definite shape
  • Liquids
  • Particles more separated, assumes shape of
    container
  • Gases
  • Particles farther apart than liquids

27
Part 14. Changes of State
  • Melting
  • Solid to liquid
  • Needs heat energy that is stored as Potential
    Energy (no temp change)
  • Heat of Fusion heat needed to change 1 gram of
    solid into liquid
  • HF for water 334 Joules/g

28
Part 14. Changes of State
  • Freezing (Fusion)
  • Liquid to solid
  • Heat is removed (given-off)
  • Use Heat of Fusion also

29
Part 14. Changes of State
  • Vaporization (evaporation)
  • Liquid to gas
  • Needs heat energy that is stored as Potential
    Energy (no temp change)
  • Heat of Vaporization heat needed to change 1
    gram of liquid into gas
  • HV for water 2260 Joules/g

30
Part 14. Changes of State
  • Condensation
  • Gas to liquid
  • Heat is removed (given-off)
  • Use Heat of Vaporization also

31
Part 14. Changes of State
  • Problems
  • How much heat is needed to change 20g of ice at 0
    º C into 20g of water at 0 º C?
  • Heat Energy (Q) Mass (m) x HF
  • Q mHF
  • Q 20g x 334 J/g
  • Q 6680 Joules

32
Part 14. Changes of State
  • How much heat must be lost to turn 50 g of water
    at 0 º C into ice at 0 º C ?
  • Q mHF
  • Q 50g x 334 J/g
  • Q 16700 Joules

33
Part 14. Changes of State
  • How much energy is needed to turn 50g of water at
    100 º C into 50g of steam at 100 º C ?
  • Q mHV
  • Q 50g x 2260 J/g
  • Q 113,000 Joules
  • Which takes more energy melting ice or boiling
    water?

34
  1. What temp does this substance melt?
  2. What temp does it boil?
  3. At this rate, how long does it take to turn the
    substance from a solid at 40 º C into gas at 170
    º C ?
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