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8/10/2019 4.3 Greenhouse Effect - The Context
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Greenhouse Effect: the context
The three planets
Energy balance
Albedo
Introduction
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Four billion years ago Earth, Venus and Mars
had similar CO2atmospheres
Mars Thin atmosphereAlmost all CO2in ground Increase in temperature: +6C
Earth0.03% CO2in atmosphereIncrease in temperature: +31C
Venus Thick atmosphere 96% CO2Increase in temperature: +510C
Temperature increase due to Greenhouse effect
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Tenuous gases of the atmosphere
Steam emissions from coal burning electric power stations
Hydrocarbon powered aircraft engine
Snowy mountains
Image from aircraft over Victoria, Australia, Credit: David Jamieson
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Energy must balance
Energy input = energy reflected + energy absorbed& re-radiated
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Albedo determines how much energy is reflected
Albedo
Cloud up to 0.7
Snow 0.8-0.9Water 0.2 to 1
(depends on angle)Bare Ground 0.17
Road 0.04
Charcoal (soot) 0.04
Earth Average
0.31
Black Body 0
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white
light yellow
lemon
orange
dark orange
salmon
bright cherry
cherry
mediumcherrydark cherry
blood red
faint red
1205C (2200F)
1080C (1975F)
990C (1830F)
940C (1725F)
915C (1680F)
845C (1550F)
790C (1450F)
745C (1375F)
690C (1275F)
635C (1175F)
580C (1075F)
500C (930F)
Emission of energy: colour depends on temperatureThese are the colours of an ideal black body
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The Stefan Bolzmann Law
SUN T= 5780 K
E*= 6.34#
107
Wm-2
EARTHT= 290 K
E*= 400 Wm-2
Total black body irradiance:
where = 5.67#10-8W m-2K-4
(temperature T is measured in Kelvin)
E* =
T
4
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a simple approximation to get started.
Sun Power Input = Earth Heat output
(1 A) S(rE)2=(TE)
44(rE)2
A=Earth Albedo, S=Sun input rate on Earth (W/m2), rE=Earth Radius, TE=Earth surface temperature
Gives TE= 255 K or 18oC
But the average temperature is actually +15o
C
Clearly we are missing something!
It is the Greenhouse effect!
Let us apply black body physics to the Earth
Moon seen through the atmosphere, Credit: NASA;
(1 0.31) 1,370 = 5.67#108(TE)44
1,370 W/m2
at 12 noon
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Greenhouse Effect: the context
Summary
Mars and Venus can teach us about planetary energetics
Energy in must balance Energy out
Albedo affects reflected energy
Simple physics tells us how much a body radiates
The surface of the Earth is warmed by the Sun AND the atmosphere (the
Greenhouse effect)
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Image Credits
Slide
Details
2 Mars (http://hubblesite.org/newscenter/archive/releases/2005/34/image/h/) by NASA $(http://www.nasa.gov/),ESA $(http://www.spacetelescope.org/), and The Hubble Heritage $
Team (http://heritage.stsci.edu/) (STScI /AURA ) (http://www.stsci.edu/|http://www.aura-astronomy.org/)
The Blue Marble : Western Hempishpere(http://eoimages.gsfc.nasa.gov/images/imagerecords/57000/57723/globe_west_2048.jpg) byNASA [Public Domain]
Venus Cloud Tops (http://hubblesite.org/gallery/album/solar_system/venus/pr1995016g) by L. Esposito (University of Colorado,
Boulder), and NASA $(http://www.nasa.gov/)
3 David Jamieson
4
Swirling Maelstrom (http://sdo.gsfc.nasa.gov/assets/gallery/preview/Swirling_304_Sept2010.jpg) by NASA [Public Domain]$Full Earth (http://www.nasa.gov/images/content/115334main_image_feature_329_ys_full.jpg) by NASA/Apollo 17 [Public Domain]
5 South Pole frame (SouthPole_1920x108060fps.0001.tif ) from Pulse of Snow and Sea Ice(SVS Animation 3944 http://svs.gsfc.nasa.gov/goto?3944) by NASA/Goddard Space FlightCenter Scientific Visualization Studio
6 (partial) Swirling Maelstrom (http://sdo.gsfc.nasa.gov/assets/gallery/preview/Swirling_304_Sept2010.jpg) by NASA [Public Domain]pt2010.jpg
Adaptation: David Jamieson
7 Swirling Maelstrom (http://sdo.gsfc.nasa.gov/assets/gallery/preview/Swirling_304_Sept2010.jpg) by NASA [Public Domain]Full Earth (http://www.nasa.gov/images/content/115334main_image_feature_329_ys_full.jpg) by NASA/Apollo 17 [Public Domain]
8 (partial) Swirling Maelstrom (http://sdo.gsfc.nasa.gov/assets/gallery/preview/Swirling_304_Sept2010.jpg) by NASA [Public Domain]$View of the crescent moon through the top of the earth's atmosphere (
http://commons.wikimedia.org/wiki/File:Top_of_Atmosphere.jpg) By NASA Earth Observatory [Public domain], via WikimediaCommons