a user-friendly earth system model of low complexity: the escimo system dynamics model of global warming towards 2100
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2016
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Abstract
We have made a simple system dynamics model, ESCIMO (Earth System Climate
Interpretable Model), which runs on a desktop
computer in seconds and is able to reproduce the main output from more
complex climate models. ESCIMO represents the main causal mechanisms at work
in the Earth system and is able to reproduce the broad outline of climate
history from 1850 to 2015.
We have run many simulations with ESCIMO to 2100 and beyond. In this paper we present the effects of introducing in 2015 six possible global policy interventions that cost around USD 1000 billion per year – around 1 % of world GDP. We tentatively conclude (a) that these policy interventions can at most reduce the global mean surface temperature – GMST – by up to 0.5 °C in 2050 and up to 1.0 °C in 2100 relative to no intervention. The exception is injection of aerosols into the stratosphere, which can reduce the GMST by more than 1.0 °C in a decade but creates other serious problems. We also conclude (b) that relatively cheap human intervention can keep global warming in this century below +2 °C relative to preindustrial times. Finally, we conclude (c) that run-away warming is unlikely to occur in this century but is likely to occur in the longer run. The ensuing warming is slow, however. In ESCIMO, it takes several hundred years to lift the GMST to +3 °C above preindustrial times through gradual self-reinforcing melting of the permafrost.
We call for research to test whether more complex climate models support our tentative conclusions from ESCIMO.
We have run many simulations with ESCIMO to 2100 and beyond. In this paper we present the effects of introducing in 2015 six possible global policy interventions that cost around USD 1000 billion per year – around 1 % of world GDP. We tentatively conclude (a) that these policy interventions can at most reduce the global mean surface temperature – GMST – by up to 0.5 °C in 2050 and up to 1.0 °C in 2100 relative to no intervention. The exception is injection of aerosols into the stratosphere, which can reduce the GMST by more than 1.0 °C in a decade but creates other serious problems. We also conclude (b) that relatively cheap human intervention can keep global warming in this century below +2 °C relative to preindustrial times. Finally, we conclude (c) that run-away warming is unlikely to occur in this century but is likely to occur in the longer run. The ensuing warming is slow, however. In ESCIMO, it takes several hundred years to lift the GMST to +3 °C above preindustrial times through gradual self-reinforcing melting of the permafrost.
We call for research to test whether more complex climate models support our tentative conclusions from ESCIMO.
| Reference Key |
randers2016eartha
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|---|---|
| Authors | ;J. Randers;U. Golüke;F. Wenstøp;S. Wenstøp |
| Journal | itinéraires |
| Year | 2016 |
| DOI |
10.5194/esd-7-831-2016
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| URL | |
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