solar constant (1370 w/m (5.67x10 t s (1 a)...

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Earths radiative balance or, how I learned to stop worrying and love the greenhouse effect If the Earth had no atmosphere: T 4 = S / 4 (1 A) T = 255 K -18 ˚C 0 ˚F Albedo (reflectivity) Solar constant (1370 W/m 2 ) Stefan-Boltzmann constant (5.67x10 -8 ) reflected Absorbed and re-radiated as heat

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Page 1: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If

Earth’s radiative balance or, how I learned to stop worrying and love the greenhouse effect

If the Earth had no atmosphere:

T4 = S/4(1 — A)

T = 255 K

-18 ˚C

0 ˚F

Albedo (reflectivity)

Solar constant (1370 W/m2) Stefan-Boltzmann constant

(5.67x10-8)

reflected

Absorbed and

re-radiated as heat

Page 2: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 3: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 4: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If

288 - 255 = 33 ˚ of ‘normal’ greenhouse warming

Actual surface

No atmosphere

Sunlight Infra-red radiation

Air

Page 5: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If

0

-0.4

0.4

1900 1940 1980 1860

Te

mp

era

ture

an

om

aly

(˚C

)

Global Temperatures for the last 150 years (5-year running average; as of ~2005)

Civil war

Model T

World War II

Al Gore invents

the internet

Page 6: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If

After Jones and Wigley, 1980

“ . . . a global deterioration of climate, by order of magnitude larger than any hitherto experienced by

civilized mankind, is a very real possibility and indeed may be due very soon.”

Climate change in the age of Disco

Page 7: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If

The last ~10 years: another plateau resembling ~1950

Page 8: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If

Currently favored explanation of the plateaus is that

these are periods when accumulated heat gets

preferentially stored in ocean instead of atmosphere…

Page 9: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If

Warming has a strong geographic bias

(2000-2009 avg. vs. 1950-1980 mean)

±2.5 ˚C scale

Page 10: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If

A long-suspected driving force — rise in CO2

Global average 1700-2000 AD

Mauna Loa 1958-2004 AD

Page 11: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If

The CO2 Greenhouse Effect What should physical principles lead me to expect of global warming?

Complications

• Solar ‘constant’ is a variable

• Water-vapor feedback

• Albedo

• Ice

• Clouds

• Aerosols and dust

• Ground cover

33 ˚ of warming = 20˚ from H2Ov + 10 ˚ from CO2 + 3 ˚ from other things

CO2 has risen 10’s of %, so T should

have risen by a degree or more

Arrhenius, 1896

Doubling CO2 = 5-6 ˚C warming

Page 12: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If

Cylon invasion happens here

Page 13: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 14: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 15: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If

Reid, 1999; by way of www.oar.noaa.gov

Sunspots and early 20th century temperatures

Page 16: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 17: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 18: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 19: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 20: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 21: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 22: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 23: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 24: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 25: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 26: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 27: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If
Page 28: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If

So what factor is to blame for 20th century T rise?

Wrong question — lots of things are to ‘blame’ but some

are more important than others, and at different times

Page 29: Solar constant (1370 W/m (5.67x10 T S (1 A) 4web.gps.caltech.edu/classes/ge11a/Docs_2014/Ge11a.2014.L12.pdf · or, how I learned to stop worrying and love the greenhouse effect If