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Published in: Mitigation and Adaptation Strategies for Global Change 8/2013

01-12-2013 | Original Article

Fail-safe solar radiation management geoengineering

Author: Takanobu Kosugi

Published in: Mitigation and Adaptation Strategies for Global Change | Issue 8/2013

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Abstract

To avoid dangerous changes to the climate system, the global mean temperature must not rise more than 2 °C from the 19th century level. The German Advisory Council on Global Change recommends maintaining the rate of change in temperature to within 0.2 °C per decade. This paper supposes that a geoengineering option of solar radiation management (SRM) by injecting aerosol into the Earth’s stratosphere becomes applicable in the future to meet those temperature conditions. However, a failure to continue the use of this option could cause a rapid temperature rebound, and thus we propose a principle of SRM use that the temperature conditions must be satisfied even after SRM termination at any time. We present economically optimal trajectories of the amounts of SRM use and the reduction of carbon dioxide (CO2) emissions under our principle by using an economic model of climate change. To meet the temperature conditions described above, the SRM must reduce radiative forcing by slightly more than 1 W/m2 at most, and industrial CO2 emissions must be cut by 80 % by the end of the 21st century relative to 2005, assuming a climate sensitivity of 3 °C. Lower-level use of SRM is required for a higher climate sensitivity; otherwise, the temperature will rise faster in the case of SRM termination. Considering potential economic damages of environmental side effects due to the use of SRM, the contribution of SRM would have to be much smaller.
Appendix
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Footnotes
1
The termination problem could be insignificant if the placement of sunshades in space is selected as an SRM option because of their longer service life time. In this case, however, the required implementation cost would grow by three orders of magnitude compared to injecting aerosol into the stratosphere (Kosugi 2010).
 
2
This assumption is based on the work of Pierce et al. (2010), which showed estimates of the decrease in radiative forcing affected by an increase in the amount of stratospheric aerosol injection. We can observe from the estimates that, while strictly speaking the effect on the decrease in radiative forcing yielded by the stratospheric aerosol injection gradually diminishes with an increase in the latter, the effect is approximately linear for a 4 W/m2 or smaller decrease in radiative forcing.
 
3
The impact of the 1991 eruption of Mt. Pinatubo in the Philippines on reducing global radiative forcing amounted to 4.5 W/m2 (Hansen et al. 1992).
 
4
The interest rates are calculated endogenously in the model and are approximately 5 %/year in all the cases considered in this study.
 
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Metadata
Title
Fail-safe solar radiation management geoengineering
Author
Takanobu Kosugi
Publication date
01-12-2013
Publisher
Springer Netherlands
Published in
Mitigation and Adaptation Strategies for Global Change / Issue 8/2013
Print ISSN: 1381-2386
Electronic ISSN: 1573-1596
DOI
https://doi.org/10.1007/s11027-012-9414-2

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