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Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

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Page 1: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

Discussion 2

Wednesday 2/6Quiz prep + lecture 4

Page 2: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

• Atmospheric composition• Atmospheric evolution – deep time, recent

CO2, CH4, CFCs• Carbon and hydrological cycles• Aerosols• Air pressure – Torciello, changes with height,

ideal gas law• Layers of the atmosphere• Temperature, heat transfer, radiation

Quiz Topics

Page 3: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

N2

O2

Ar

O3

Inert gasesCO2

H2

←SO2, NO2,CFC’s, etc

PM

COCH4

N2O

Composition of the Earth’s Troposphere

Page 4: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

Fig. 1-4, p. 7

Page 5: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

Fig. 1-7, p. 9

Page 6: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

Fig. 1-3, p. 6

Carbon Cycle

Page 7: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

Fig. 1-5, p. 8

Hydrologic Cycle

Page 8: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

Fig. 1-5, p. 8

Hydrologic Cycle

Page 9: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

Fig. 1-13, p. 15

Page 10: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

Fig. 1-14, p. 17

Page 11: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4
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Fig. 2-7, p. 34

ELECTROMAGNETIC SPECTRUM

Page 14: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

Insolation

• Earth’s tilt & the seasons• Angle of incidence & solar zenith angle• Earth’s energy budget– Insolation and re-radiation– Latitudinal heat balance– The greenhouse effect

Page 15: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

Fig. 2-12, p. 42

HEATING OF THE EARTH’S SURFACE DEPENDS ON THE AMOUNT OF SOLAR RADIATION PER UNIT AREA.

SAME AMOUNT OF RADIATION IS DISTRIBUTED OVER A LARGER AREA IN A THAN IN B.

RADIATION PER UNIT AREA IS LESS IN A THAN IN B. LESS HEATING IN A THAN IN B.

Page 16: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4
Page 17: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4
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Latitudinal Heat Balance

Page 19: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

20 )1( eA RQE

Simple Greenhouse Model

24 4 eeR RTE

4

)1( 04

Q

Te

But this doesn’t factor in the atmosphere! 254K vs 288K

Page 20: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

Project 1 – Hurricane Sandy

Page 21: Discussion 2 Wednesday 2/6 Quiz prep + lecture 4

Project 1 – Hurricane Sandy