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Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)
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Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Dec 25, 2015

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Noah Jennings
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Page 1: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Global Greenhouse Effect (steady-state)

vs. Global Warming

(disturbed steady-state)

Page 2: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Earth’s Energy Balance

Page 3: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Earth’s Energy Balance

• Visible and UV light from sun through atmosphere to earth

• Energy absorbed by earth

• Infrared light radiated from earth

• 84% of radiated IR light absorbed by “Greenhouse Gases”

• Energy in = Energy out

Page 4: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Disturbed Energy Balance

• Additional carbon dioxide in atmosphere

• >84% of radiated IR light absorbed by “Greenhouse Gases”

• Energy out<Energy inEnhanced greenhouse effect

Page 5: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Matter/Radiation Interaction

Page 6: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

What’s a Greenhouse Gas??

•CH4 (methane), H2O (water), CO2 (carbon dioxide)

•NOT N2 (nitrogen), O2 (oxygen)

A greenhouse gas absorbs IR radiation

Page 7: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Specific Bending and Stretching, CO2

•Figure 3.6

Page 8: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)
Page 9: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Greenhouse Gases absorb radiation in the

IR region•For an absorption to occur, the

overall charge distribution in the molecule must change.

You must be able to make he molecule non-symmetric

Page 10: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Molecular “SHAPE”From 2D Lewis Structures to 3D

shapes

“ Electron groups around an atom will orient themselves as far

apart as possible”

Page 11: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)
Page 12: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Fig. p.115

Page 13: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Figure 3.10

CO2 Human

Contribution

Page 14: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

How much carbon dioxide do you

generate when you have an outdoor

barbecue?

Page 15: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Two ways to quantify

•How many?–Particles–Moles of particles

•What mass?–Atomic weight (isotope average)

–Molar mass

Page 16: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Enhanced Global Warming?

Page 17: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Fig. 3.6

Page 18: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)
Page 19: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Relation between CO2 and Temperature

Page 20: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Fig. 3.2

Page 21: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

True, False or Maybe?1. Carbon dioxide contributes to

an elevated global temperature.2. The concentration of CO2 in the

atmosphere has been increasing.

3. The increase in CO2 is due to human activity.

Page 22: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

True, False or Maybe? Cont.

4. There has been an increase in average global temperature during the past century?

5. The greenhouse gases generated by human activity are responsible for the temperature increase.

Page 23: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

True, False or Maybe? Cont.

6. The average global temperature will continue to increase as human emissions of greenhouse gases increase.

Page 24: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

Climate Modeling

MANY variablesdifficult to identifydifficult to measureinteractions

Page 25: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

3.9 Consider This: The CO2 Emissions-Implications for

Policy(page 109)

Page 26: Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)

HomeworkRead distributed article and

identify two questions you would like to have answers to before you

could decide to endorse or not endorse the Bush administration’s

policy.(TYPED for FRIDAY)