Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out...
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![Page 1: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/1.jpg)
Radiation Balance of the Earth-Atmosphere System
In Balance:
Energy flow in = Energy flow out
PowerPoint 97
To download: Shift LeftClick
Please respect copyright on this material
![Page 2: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/2.jpg)
Reaction Topic
What would be the impacts on life in Wisconsin if the climate were 10oF warmer year round?
![Page 3: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/3.jpg)
Key Points Climate depends on radiation from sun
– Sun higher above horizon in summer => more radiation per unit area of earth surface
– Atmosphere mostly transparent to solar
– Surface heating reduced by clouds & snow Because CO2 acts like a blanket, surface and lower
atmosphere cool by infrared radiation to space from upper troposphere (ERL= effective radiating level)
Increased atmospheric CO2 raises ERL, reducing outgoing IR, until troposphere has warmed to compensate
Ocean heat storage in ocean takes decades to come to new balance
For given CO2 low clouds cool , high clouds warm
![Page 4: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/4.jpg)
The Seasons
Equinox Summer
Madison
![Page 5: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/5.jpg)
The effect of distance from the sun
Assumed mathematics– Sphere of radius r
Surface area = 4 r2
– Disc of radius r One sided area = r2
Intensity = Power received by object divided by the area of object = Energy flow / unit surface area
![Page 6: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/6.jpg)
Radiation from the Sun
rR
S
Earth
Sphere
Sun
Intensity over Earth = 1368 r2 / (4 r2) = 342 W m-2
(averages time of day & latitude)
Intensity direct from sun = S / (4 R2) = 1368 W m-2
(the inverse square law)
![Page 7: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/7.jpg)
How Strong is the Sun at Mars?
S = total power emitted by Sun – output of nuclear furnace deep inside
R = distance of Earth from Sun Distance of Mars from Sun = 1.4 R Direct Intensity = S / {4 (1.4 R)2}
= 1368 / (1.4)2 W m-2 = 698 W m-2
Sunlight is half as strong on Mars
![Page 8: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/8.jpg)
Electromagnetic Spectrum
.1 .5 1 5 10
Vis
ible
Nea
r In
frar
ed
Infr
ared
10,000
Mic
row
ave
X-r
ays
Ultr
avio
let
.0001
Wavelength (microns)
![Page 9: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/9.jpg)
Opacity of Atmosphere (no clouds)
Horel & Geisler Chapter 3
Fraction of radiation absorbed by entire atmosphere (mostly in the troposphere)
From Sun From Earth
0 %
50 %
100 %
20151050.70.50.30.10.07
Wavelength (micrometers)
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Key Points Climate depends on radiation from sun Because CO2 acts as a blanket, surface and lower
atmosphere cool by infrared radiation to space from upper troposphere (ERL= effective radiating level)
Increased atmospheric CO2 raises ERL, reducing outgoing IR, until troposphere has warmed to compensate
Because of heat storage in the ocean, the system to takes decades to come to new balance
For given CO2 low clouds cool , high clouds warm
![Page 11: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/11.jpg)
Solar Radiation Budget
100% 342 W/m2
30.7% 105 W/m2
69.3% 237 W/m2
Reflected
Incoming
Absorbed
Earth as a whole
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The Effective Radiating Level
ERL ERL: The lowest level in the atmosphere from
which infra red radiation is able, on average, to escape upwards to outer space without being reabsorbed
As concentrations of absorbing gases such as CO2 are increased, the ERL rises, decreasing the total mass of air above and keeping the opacity of that air constant.
The intensity of the radiation emitted to space increases with the temperature at the ERL
![Page 13: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/13.jpg)
Temperature and Altitude
Adapted from H & W Figure
Stratosphere
Troposphere
5% mass
20% mass
75% mass
Tropopause10 km
20 km
30 km
40 km
200 K 250 K 300 K
Convection & clouds
Little Mass to Absorb RadiationSlow Overturning (years)
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Key Points Climate depends on radiation from sun Surface and lower atmosphere cool by infrared
radiation to space from upper troposphere (ERL= effective radiating level, such that total CO2 above is fixed)
Increased concentration of atmospheric CO2 raises ERL, reducing outgoing IR, until troposphere has warmed to compensate
Ocean heat storage in ocean takes decades to come to new balance
For given CO2 concentration, low clouds cool , high clouds warm
![Page 15: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/15.jpg)
Absorbent Atmosphere
Temperature
ERL
InfraredSolar
ERL =Effective Radiating Level
Solar in = IR out
H2O, CO2, ...
Tropopause
![Page 16: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/16.jpg)
Key Points Climate depends on radiation from sun Surface and lower atmosphere cool by infrared
radiation to space from upper troposphere (ERL= effective radiating level, such that total CO2 above is fixed)
Increased concentration of atmospheric CO2 raises ERL, reducing outgoing IR, until troposphere has warmed to compensate
Ocean heat storage in ocean takes decades to come to new balance
For given CO2 concentration, low clouds cool , high clouds warm
![Page 17: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/17.jpg)
Greenhouse Warming: a simple model
Hold absorption of incoming solar radiation radiation fixed
Infrared radiation leaves earth for space from upper troposphere (ERL). Amount increases with temperature at ERL (immediate). Height of ERL is such that total CO2 above it is constant.
Additional carbon dioxide mixes rapidly in troposphere (weeks) – ERL rises to where temperature is lower, less
outgoing radiation., Earth surface+ troposphere warms till outgoing
radiation from ERL balances incoming (years to centuries)
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Effects of Enhanced CO2initial change in radiation
Temperature
ERL
InfraredSolar
ERL =Effective Radiating Level
Solar in = IR out
H2O, CO2, ...
Tropopause
![Page 19: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/19.jpg)
Effects of Enhanced CO2after rebalance
Temperature
ERL
InfraredSolar
ERL =Effective Radiating Level
Solar in = IR out
H2O, CO2, ...
Tropopause
![Page 20: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/20.jpg)
Key Points Climate depends on radiation from sun Surface and lower atmosphere cool by infrared
radiation to space from upper troposphere (ERL= effective radiating level, such that total CO2 above is fixed)
Increased concentration of atmospheric CO2 raises ERL, reducing outgoing IR, until troposphere has warmed to compensate
Because of heat storage in the ocean, it takes decades to come to new balance
For given CO2 concentration, low clouds cool , high clouds warm
![Page 21: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/21.jpg)
How long to achieve balance?
Land surface & atmosphere ~ 1 month
Ocean surface layers ~ decades
Deep ocean ~ millenia
![Page 22: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/22.jpg)
Key Points Climate depends on radiation from sun Surface and lower atmosphere cool by infrared
radiation to space from upper troposphere (ERL= effective radiating level, such that total CO2 above is fixed)
Increased concentration of atmospheric CO2 raises ERL, reducing outgoing IR, until troposphere has warmed to compensate
Heat storage in ocean takes decades to come to new balance
For given CO2 concentration, low clouds cool , high clouds warm
![Page 23: Radiation Balance of the Earth-Atmosphere System In Balance: Energy flow in = Energy flow out PowerPoint 97 To download: Shift LeftClick Please respect.](https://reader030.fdocuments.in/reader030/viewer/2022032516/56649c7c5503460f9493166f/html5/thumbnails/23.jpg)
Effects of Low Clouds
reflect sunlight (to space as well as to your eyes)
reduce absorbed solar radiation little effect on outgoing infrared tend to cool the earth
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Effects of High Clouds
reflect little sunlight (hard to see) are much colder than earth surface absorb and re-emit outgoing infrared like
a greenhouse gas tend to warm the earth
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Earth from
Space
NASA
Which wins?
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Sources of Information
Horel & Geisler Chapter 2