A multicointegration model of global climate change
Stephan B. Bruns,
Zsuzsanna Csereklyei and
David Stern ()
No 336, Center for European, Governance and Economic Development Research Discussion Papers from University of Goettingen, Department of Economics
We model the role of the ocean in climate change, using the concept of multicointegration. Surface temperature and radiative forcing cointegrate and the accumulated cointegration disequilibria represent the change in Earth system heat content, which is predominantly stored in the ocean. System heat content in turn cointegrates with surface temperature. Using a multicointegrating I(2) model, we find that the climate sensitivity is 2.8°C and the rate of adjustment to equilibrium is realistically slow. These results contrast strongly with those from I(1) cointegration models and are more consistent with global circulation models. We also estimate Earth system heat content as a latent variable for the full period, 1850-2014, and this predicted heat content cointegrates with available ocean heat content observations for 1940-2014.
JEL-codes: C32 Q54 (search for similar items in EconPapers)
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Working Paper: A Multicointegration Model of Global Climate Change (2018)
Working Paper: A Multicointegration Model of Global Climate Change (2004)
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