Family Homecoming Special Event "Can Climate Engineering Serve as a Complementary Step to Aggressive Mitigation?" - PowerPoint PPT Presentation

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Title: Family Homecoming Special Event "Can Climate Engineering Serve as a Complementary Step to Aggressive Mitigation?"


1
Family Homecoming Special Event"Can Climate
Engineering Serve as a Complementary Step to
Aggressive Mitigation?"
  • Dr. Michael MacCracken, The Climate Institute,
    Washington, DC
  • Friday, Sept. 25 at 400 pm in Olin 1, with
    cookies

2
Hydrologic Cycle
3
Annual Precipitation, Washington State
4
The Atmospheres Energy
  • Read Anthes chapter 3

5
Energy is the ability to do work
  • Units are mass x distance2 / time2
  • Potential energy E mgh
  • Kinetic energy E 1/2 mv2
  • Heat energy sensible and latent
  • Radiant energy visible and infrared

6
Laws of Thermodynamics
  • 1. Conservation of energy Energy is neither
    created nor destroyed it is transformed.
  • you can't take out of a system more than you put
    in.
  • you can't win
  • 2. The entropy of the universe is continually
    increasing.
  • perpetual motion and a heat engine with 100
    efficiency are both impossible.
  • you can't break even
  • 3. It is impossible to attain absolute zero or
    absolute 0 entropy.
  • you can't even get out of the game

7
Energy transformation exampleHydroelectric
power plant
8
More complete picture
9
  • Solar power (drives hydrologic cycle)
  • Potential energy (water stored in reservoir)
  • Kinetic energy (spillway)
  • Mechanical energy (spinning turbines)
  • Electrical energy (transmitted over wires)
  • Lightbulbs (converts energy to light)
  • Waste heat (IR) is lost to space

10
Transfer of Energy
  • Conduction -- Molecular motion
  • Convection -- Mass transfer vertical
  • Advection -- Mass transfer horizontal
  • Latent heat -- Ice and liquid phases
  • Radiation -- SW and LW photons

11
Conduction (molecular motion)
  • Thermal conductivity is the ability of a
    substance to transfer heat via molecular motion.
  • Measured in units of cal/sec/cm/oC
  • Conductivity of solids gt liquids gt gases.
  • Silver (good conductor) 1.0
  • Water (1000 times worse) 1.4 x 10-3
  • Ice 5.3 x 10-3
  • Air (good insulator) 6.1 x 10-5

12
Convection and Advection (mass transfer)
  • Rising air currents (thermals) carry sensible
    heat and latent heat from the surface into the
    upper air.
  • Winds (advection) carry sensible heat and latent
    heat (moisture) into northern latitudes.
  • Ocean currents transfer warmer waters to northern
    latitudes and vice-versa.

13
The Electromagnetic Radiation
  • Every object in the universe emits radiation.
  • From 1012 cm radio waves to 10-12 cm gamma rays

14
Stefan-Boltzmann Law
  • Hotter bodies emit more total energy than colder
    bodies.
  • The total energy of a blackbody is proportional
    to the fourth power of temperature.
  • Etot ?T4

15
  • Compare energy emitted by Sun? and Earth?
  • Energy emitted per unit of surface area
  • E? / E? ?T4? / ?T4? (6000 / 300)4 204 1.6
    x 105
  • Energy emitted by the entire surface
  • Multiply by R2?/ R2? (100/1)2 104
  • So Sun emits 1.6 x 109 more energy than Earth

16
Power in watts
  • Sun 3.6 1026
  • Total human consumption, global 1.3 1013
  • Total human consumption, US 3.2 1012
  • Large commercial power plant 109 to 1010
  • human, daily average from diet 100 (one light
    bulb)
  • per capita world 2 x 103 (20 lightbulbs)
  • per capita US 104 (100 lightbulbs)

17
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18
Planck energy distribution curve (energy
density per unit time per unit wavelength)
19
Weins Law
  • The wavelength of maximum emission depends
    inversely on a bodys Kelvin temperature.
  • ?max 2897/T (microns)
  • Emission from hotter bodies peaks at shorter
    wavelengths.
  • What is ?max for the Sun?
  • ?max? C/T 2897/ 6000 0.48 microns yellow
    visible light
  • What is ?max for the Earth?
  • ?max? C/T 2897/ 300 10,1 microns infrared

20
Trace gases absorb radiation at selected
wavelenghts.Atmosphere is transparent to
sunlight at 0.5mm and to IR at 10mm
21
Net result
22
Make a heat budget at the top and bottom of the
atmosphere
23
\
  • Top of atmosphere Gains Losses 100 SW -
    31.3 SW - 68.7 LW 0

Surface 7.6 SW 43.2 SW 98 LW - 7.6 SW - 4.4
C - 22.8 E - 114 LW 0 This is the average
balance sheet -- Dynamic balance is never
achieved!
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