Climate%20Uncertainty%20and%20the%20Necessity%20to%20Transform%20Global%20Energy%20Supply%20%20Bob%20van%20der%20Zwaan%20(ECN%20and%20Harvard%20University)%20and%20Reyer%20Gerlagh%20(IVM,%20Vrije%20Universiteit%20Amsterdam) - PowerPoint PPT Presentation

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Climate%20Uncertainty%20and%20the%20Necessity%20to%20Transform%20Global%20Energy%20Supply%20%20Bob%20van%20der%20Zwaan%20(ECN%20and%20Harvard%20University)%20and%20Reyer%20Gerlagh%20(IVM,%20Vrije%20Universiteit%20Amsterdam)

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Title: Climate%20Uncertainty%20and%20the%20Necessity%20to%20Transform%20Global%20Energy%20Supply%20%20Bob%20van%20der%20Zwaan%20(ECN%20and%20Harvard%20University)%20and%20Reyer%20Gerlagh%20(IVM,%20Vrije%20Universiteit%20Amsterdam)


1
Climate Uncertainty and the Necessity to
Transform Global Energy SupplyBob van der
Zwaan (ECN and Harvard University)andReyer
Gerlagh (IVM, Vrije Universiteit Amsterdam)
  • International Energy Workshop
  • (EMF/IEA(ETSAP)/IIASA)
  • International Energy Agency
  • Paris
  • 22-24 June 2004

2
Outline
  • I. Introduction
  • II. Climate sensitivity
  • III. Model
  • IV. Results
  • V. Conclusions

The EU-funded NEMESIS/ETC project (European
Commission contract No. ENG2-CT-2001-00538) is
greatly acknowledged.
3
I. Introduction
  • The sensitivity of the global mean temperature on
    Earth to the increasing concentration of
    atmospheric CO2 is currently known to about only
    a factor of three.
  • Uncertainty in the climate sensitivity has a
    larger effect than the uncertainty in our
    understanding of the carbon cycle (Caldeira,
    2003).
  • This presentation / paper explores the
    relationship between the climate sensitivity
    uncertainty and the claimed necessity to
    transform world energy supply.

4
II. Climate sensitivity
  • Mankind is already halfway towards an equivalent
    doubling of the atmospheric CO2 concentration,
    from the pre-industrial level of 280 ppmv to 420
    ppmv today.
  • A doubling corresponds, via the enhanced
    greenhouse effect, to a global average surface
    air temperature increase, ?T(2X), of 1.5
    4.5 ºC (IPCC, 2001).
  • The stabilisation CO2 concentration, P, and
    stabilisation temperature increase, ?T, are
    related through

5
III. Model
DEMETER DEcarbonisation Model with Endogenous
Technologies for Emission Reductions
  • There are two competing generic energy sources,
    one fossil-based (F), the other one with zero CO2
    emissions (N).
  • Old capital is distinguished from new capital, in
    a so-called vintage approach.
  • Technological change is modelled endogenously
    through learning curves.
  • A substitution elasticity is included between F
    and N, such that the new technology (N) can
    spread before it reaches maturity.

6
III. Publications
  • van der Zwaan, B.C.C., R. Gerlagh, G. Klaassen,
    and L. Schrattenholzer (2002), Endogenous
    technological change in climate change
    modelling, Energy Economics 24, 1.
  • Gerlagh, R. and B.C.C. van der Zwaan (2003),
    Gross World Product and Consumption in a Global
    Warming Model with Endogenous Technological
    Change, Resource and Energy Economics 25, 35-57.
  • Gerlagh, R., B.C.C. van der Zwaan, M.W. Hofkes,
    and G. Klaassen (2004), Impacts of CO2-taxes in
    an economy with niche markets and
    learning-by-doing, Environmental and Resource
    Economics, forthcoming.
  • Gerlagh, R. and B.C.C. van der Zwaan (2004), A
    sensitivity analysis of timing and costs of
    greenhouse gas emission reductions under learning
    effects and niche markets, Climatic Change,
    forthcoming.

7
IV. Carbon stabilisation
  • Carbon emissions under various climate
    sensitivities.
  • Source van der Zwaan and Gerlagh, 2004.

8
IV. Savings vs. decarbonisation
  • Relative importance of energy savings and
    decarbonisation in emission reductions.
  • Source van der Zwaan and Gerlagh, 2004.

9
IV. Emission reduction timing
  • Timing of emission reduction efforts.
  • Source van der Zwaan and Gerlagh, 2004.

10
V. Conclusions
  • Allowed carbon emission path is determined to a
    large extent by the climate sensitivity, ?T(2X).
  • Even under the lowest value of ?T(2X), the energy
    system must be transformed, from fossil-based
    fuel consumption to the use of non-carbon energy
    resources.
  • In the short run, energy savings and
    decarbonisation are both important, while in the
    longer run a transformation of the energy system
    becomes the main means to achieve emission
    reductions, for all ?T(2X).
  • The timing of emission reductions is almost
    independent of ?T(2X).
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