response - aspen global change instituteand global warming potential (gwp) will also change. non-co...

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Role of Other Greenhouse Gases - Role of Other Greenhouse Gases - Response Response Atul K. Jain Atul K. Jain Department of Atmospheric Sciences Department of Atmospheric Sciences University of Illinois, Urbana, IL University of Illinois, Urbana, IL email: [email protected] email: [email protected]

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Page 1: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

Role of Other Greenhouse Gases -Role of Other Greenhouse Gases -ResponseResponse

Atul K. JainAtul K. JainDepartment of Atmospheric SciencesDepartment of Atmospheric Sciences

University of Illinois, Urbana, IL University of Illinois, Urbana, ILemail: [email protected]: [email protected]

Page 2: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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Main ConclusionMain Conclusion

CO2 will be the maincontributor to the future totalradiative forcing andtemperature change.

Page 3: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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Increase in Radiative Forcing from pre-Increase in Radiative Forcing from pre-industrial timesindustrial times

Based on Jain et al.2000

CO2

59%CH4

21%

N2O6%

CFCs and HCFCs

13%

SF6, PFCsHFCs

1%

CO2

69%

CH4

18%

N2O7%

CFCs,HCFCs

1%SF6, PFCs

1%

HFCs4%

(1765-2000) = 2.45 Wm-2 (1765-2100) = 5.05-8.31 Wm-2

Page 4: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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What Other Greenhouse Agents are Forcing Climate?

Page 5: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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Page 6: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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Non-CONon-CO22 Greenhouse Gases Greenhouse Gases(GHGs) & Climate Change(GHGs) & Climate Change

Non-CO2 Greenhouse Gases include the gases listedunder the Kyoto Protocol (CH4, N2O, HFCs, PFCs,and SF6), as well as other fluorinated compoundsalready listed under Montreal Protocol and itsAmendments.

Why is it so important to study thecontribution of non-CO2 GHGs to climatechange and mitigation?

Page 7: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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Why are Non-COWhy are Non-CO22 Gases Important ? Gases Important ?Non-CO2 GHGs are major Contributors to increase in

radiative forcings on climate since 1750.

Non-CO2 GHGs effect the lifetimes of many greenhousegases. As a GHG’s lifetime changes, its climate forcingand Global Warming Potential (GWP) will also change.

Non-CO2 GHGs, since they arise from a variety ofsources, offer the potential to increase flexibility andlower the cost of meeting emission targets relative toCO2 abatement alone

Page 8: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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Anthropogenic Control of the Major GHGases

CH4 emissions (600 Tg-CH4/yr)fossil fuels 17%biomass burning 5%landfills 7%ruminants 14%rice 9%pollution (lifetime) ??%

N2O emissions (16 Tg-N/yr)industrial processes 7%biomass burning 3%agriculture 24%cattle/feedlots 12%

CFC & HCFC emissions (<< 1 Tg/yr)refrigeration, foam, propellant, cleaningphased out under Montreal Protocol

Page 9: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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Anthropogenic Control of the Other GHGases

PFCs = CF4 + ... (13 Gg/yr ++)anthropogenic*** 100%aluminum, industrial

SF6 emissions (6 Gg/yr ++)anthropogenic 100%insulation, electrical switches

HFC emissions (100 Gg/yr ++)anthropogenic 100%CFC partial replacements

Page 10: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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Anthropogenic Control of the Pollution gases

CO emissions (2800 Tg-CO/yr)fossil & domestic fuel 32%biomass burning 25%

NOX emissions (52 Tg-N/yr)fossil fuels 65%biomass burning 14%agriculture/soils 12%

VOC emissions (600 Tg-C/yr)fossil fuel 28%biomass burning 6%

Page 11: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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CH4

CO is an indirect greenhouse gas

CO emissions are effectivelyequivalent to CH4 emissions:

100 Tg-CO = 5 Tg-CH4(IPCC, TAR)

OHCO O3

Page 12: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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Anthropogenic Impact through Reactive Pollutants1750 - 2000

18002000 O3 OH

CH4 +4.6 DU - 30 %NOX +4.1 + 14CO +1.2 - 11VOC +0.5 - 5sum +10 DU - 32 %

“observed” +9 (±4) ??

Page 13: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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Effective Reactive Pollutant Contribution to CH4

CH4 320 Tg(CH4)/y = direct emission

NOx 40 Tg(N)/y - 80 Tg(CH4)/y

CO 1000 Tg/y + 50 Tg(CH4)/y

VOC 250 Tg/y + 30 Tg(CH4)/y

(IPCC TAR)

Page 14: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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What is the impact of including non-CO2What is the impact of including non-CO2 GHGs GHGs??Example: CH4 mitigation in the U.S.Example: CH4 mitigation in the U.S.

Science ArticleScience Article((29 October 1999, Vol 286, pp. 905-906)29 October 1999, Vol 286, pp. 905-906)

HayhoeHayhoe et al. et al.

A significant amount of CH4 emissions for the UnitedStates can be reduced with economically justified optionswith no reduction costs. Based on the latest abatementcosts, we estimate that for short-term targets, CH4 canoffset CO2 reductions and reduce U.S. costs by more than25% relative to strategies involving CO2 alone.

Page 15: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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COCO22 and CH and CH44 Marginal Abatement Cost Curves Marginal Abatement Cost Curves

$0

$100

$200

$300

$400

$500

0 100 200 300 400 500 600 700 800Emission Reduction (MtC eq)

Mar

gina

l Aba

tem

ent C

ost (

1992

$/tC

eq)

CO2 abatement 2000CH4 abatement 2000CO2 abatement 2010CH4 abatement 2010

$0

$50

$100

$150

$200

30 40 50 60 70 80

Abatement costs for CH4 increase gradually up to 75 MtCeq, or 40%of projected CH4 emissions

In contrast to CH4 costs, the carbon permit fees needed to providean economic incentive for CO2 reduction increase gradually

Page 16: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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Comparison of Emission Reduction CostsComparison of Emission Reduction Costs(Year 2010)(Year 2010)

0

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0 100 200 300 400 500 600 700 800

Emission Reduction (MtCeq)

Ratio

of C

O2+

CH4

Cost

s to

CO

2-on

ly

0

0.2

0.4

0.6

0.8

1

1.2

1.4

Tota

l Cos

t (%

of p

roje

cted

GDP

)

CH4+CO2 CO2-only

ratio = cost of in 2010

Case 1 - CO2 reduction onlyCase 2 - CH4 + CO2 reduction

Page 17: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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Illustrative emission pathwayIllustrative emission pathway

0

100

200

300

400

500

600

700

2000 2002 2004 2006 2008 2010

Year

Tota

l Cos

t (%

of p

roje

cted

GD

P)

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Cost of Illustrative Emission ScenarioCost of Illustrative Emission Scenariowith CHwith CH4 4 (green) vs. without CH(green) vs. without CH4 4 (red)(red)

0

0.2

0.4

0.6

0.8

1

1.2

2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010

Year

Tota

l Cos

t (%

of p

roje

cted

GD

P)

Page 19: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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Contribution of CHContribution of CH44 to Total CO to Total CO22-Equivalent-EquivalentReductionsReductions

0

10

20

30

40

50

60

70

80

90

100

0 0.2 0.4 0.6 0.8 1

CO2-equivalent emission reductions (GtCeq)

Cont

ribut

ion

of C

H4 (%

)

GWP = 5GWP = 24GWP = 65

Page 20: response - Aspen Global Change Instituteand Global Warming Potential (GWP) will also change. Non-CO 2 GHGs, since they arise from a variety of sources, offer the potential to increase

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ConclusionsConclusions Including non-CO2 GHGs in emission reduction

schemes has the potential to greatly reduceCO2 controls and total costs, particularly in theshort term

CH4 alone can reduce costs by over 25%relative to CO2-only

The contribution of CH4 and other non-CO2GHGs to multi-gas reduction targets dependsstrongly on how the gases are weightedrelative to CO2.

Due to the strong impact of atmosphericchemistry on CH4 concentrations, emissionsof CO, NOx and NMHCs are likely to affect thecontribution of CH4 to a multi-gas reductionscheme.