Metrics and a stabilization of the global average surface

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Chalmers University of Technology

Metrics and stabilization of the global average surface temperature

UNFCCC workshop on common metrics

Bonn, Germany, 2012-04-03

Daniel J.A. Johansson

Division of Physical Resource Theory, Department of Energy and Environment

Chalmers University of Technology

Gothenburg, Sweden.

Chalmers University of Technology

Outline

• Emissions profiles

• Global Cost Potential (GCP)

• Global Temperature change Potential (GTP)

• Cost-Effective Temperature Potential (CETP)

Chalmers University of Technology

Stabilizing below 2 ºC cost-effectively

CO

2 equivalent emissions using GWP-100

GWP was not designed to facilitate the basket approach in a cost effective stabilization regime.

UNEP, 2010, The Emissions Gap Report

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Global Cost Potential (GCP).

• Based on that a climate target should be met at lowest possible abatement cost.

• Based on optimizing Integrated Assessment Models

(IAMs).

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Optimizing Integrated Assessment

Model

Economy & Energy module

Emissions

Climate module:

Calculates concentrations, radiative forcing and subsequent temperature response

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Optimizing Integrated Assessment

Model

Objective:

Minimize total NPV abatement costs to stabilize the temperature at 2°C above the pre-industrial level

Emissions

• Climate module:

• Calculates concentrations, radiative forcing and subsequent temperature response

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Global Cost Potential (GCP)

• Based on that a climate target should be met at lowest possible abatement cost.

• Based on optimizing Integrated Assessment Models

(IAMs).

• The metric is the ratio of the cost-optimal price (tax) on emissions of a gas X to the cost-optimal tax on emissions of CO

2

.

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Global Cost Potential (GCP)

2000

2200 2000

Manne & Richels, 2001, An alternative approach to establishing trade-offs among greenhouse gases, Nature

2100

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GCP - Transparency and numerical models

• Optimizing IAMs are complex and far from transparent for most climate scientist, policy advisors and policy makers.

• Include a range of very uncertain parameters and uncertain structural relationships.

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0,06

0,05

0,04

0,03

0,02

0,01

0

0

Global Temperature change Potential (GTP)

GTP for year t

1 M ton CH4

50 100 150

100 M ton CO2

350 400 450 500

GTP

 

T

X

T

CO

2

( t )

( t )

200 250

Time (Year)

300

GTP initially developed in: Shine K.P., Fuglestvedt J.S., Hailemariam K., Stuber N. , 2005, Alternatives to the Global

Warming Potential for Comparing Climate Impacts of Emissions of Greenhouse Gases, Climatic Change

Chalmers University of Technology

120

Comparison GCP and GTP for CH

4

100

80

60

40

GCP

GTP

20

0

2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100

Time (year)

Results from runs with the MiMiC model (Azar, Johansson & Persson)

Relationship between GTP and GCP originally formulated in : Shine K.P., Berntsen T.K., Fuglestvedt J.S., Bieltvedt

Skeie R., Stuber N., 2007, Comparing the climate effect of emissions of short- and long-lived climate agents,

Philosophical Transactions of The Royal Society A

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Cost-Effective Temperature Potential

(CETP)

An approximation of GCP.

Includes:

-physical information,

-an estimate of stabilisation year,

-discount rate.

Johansson, 2011, Johansson, 2011, Economics- and physical-based metrics for comparing greenhouse gases, Climatic

Change .

Chalmers University of Technology

CETP

0,06

0,05

0,04

0,03

0,02

0,01

0

0

CETP for year t

50

100 M ton CO2

Integrate and discount

1 M ton CH4

100 150 200 250

Time (Year)

300 350 400 450

The time integrated discounted temperature pulse beyond the target time year.

500

CETP

 

 t

 t

T

X

T

CO

2

(

(

) · e

) · e

 r

 r d

 d

 e -rτ = Discount factor r -discount rate

τ -time

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Simple Carbon Cycle and Climate model ACC2

Carbon Cycle Climate

Temperature feedback

Atmosphere Max 2 ºC above pre-industrial level

Minimizing NPV abatement cost

Land

Ocean

Uptake

Uptake

Atmospheric Chemistry

CH

4

& N

2

O

SF

6

& 29 Halocarbons

Tropos-/Stratospheric O

3

Sulfate/Carbonaceous

Aerosols (direct/indirect)

Stratospheric H

2

O

OH, NO x

, CO, VOC

Tanaka et al., 2007, MPI Report ;

Tanaka et al., 2009, GRL

Tanaka et al., 2009, Climatic Change

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CH

4 metric value in 2°C stabilization scenario

140

120

100

80

60

40

20

0

2000 2020 2040 2060 2080 2100

GWP5

GWP20

GWP100

GTP5

GTP20

GTP100

Evaluation of emission metrics under climate stabilization targets, Ongoing work.

Chalmers University of Technology

CH

4 metric value in 2°C stabilization scenario

140

120

100

80

60

40

20

0

2000 2020 2040 2060 2080 2100

GWP5

GWP20

GWP100

GTP5

GTP20

GTP100

CETP

GCP

Evaluation of emission metrics under climate stabilization targets, Ongoing work.

Chalmers University of Technology

CH

4 metric value in 2°C stabilization scenario

140

120

100

80

60

40

20

0

2000 2020 2040 2060 2080 2100

GWP5

GWP20

GWP100

GTP5

GTP20

GTP100

GTPSTB

CETP

GCP

Evaluation of emission metrics under climate stabilization targets, Ongoing work.

Chalmers University of Technology

N

2

O metric value in 2°C stabilization scenario

400

350

300

250

200

GWP5

GWP20

GWP100

GTP5

GTP20

GTP100

GTPSTB

CETP

GCP

150

2000 2020 2040 2060 2080 2100

Year

Tanaka K., Berntsen T.K., Fuglestvedt J.S., Johansson D.J.A., O’Neill B., 2012, [working title:]

Evaluation of emission metrics under climate stabilization targets, Ongoing work.

Chalmers University of Technology

Importance of discount rate

CH

4

Johansson, 2011, Economics- and physical-based metrics for comparing greenhouse gases, Climatic

Change .

Chalmers University of Technology

Importance of discount rate

N

2

O

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Conclusion

• GWP was not constructed to facilitate the implementation of cost-effective climate stabilization regime…

• … although it has enabled the implementation of the basket approach.

• Using cost effective trade-off ratios (Global Cost Potential - GCP) instead of GWP could enhance the cost-effectiveness of a stabilization regime…

• … but one would then depend on complex and uncertain optimizing

IAMs.

• CETP approximate GCP well under a range of assumptions.

• Neither GTP, CETP and GCP take into account climate effects in the short term.

• CETP and GCP do to take into account climate effects in the long-term, beyond stabilization, while GTP does not.

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THANK YOU!

Questions, comments?

Chalmers University of Technology

Additional cost of meeting the 2°C limit when using

GWP-100 as compared to GCP

• The use of GWP-100 would set a too high price on CH

4

(short lived gases) years far from when stabilization occur, while the opposite hold for years close to when stabilization occur.

• The cost of of using GWP-100 is very approximately about

5% of Net Present Value (NPV) abatement cost.

Based on: Johansson, Persson & Azar, 2006, The cost using Global Warming Potentials, Climatic Change

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