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Urban, Nathan M.; Holden, Philip B.; Edwards, Neil R.; Sriver, Ryan L. and Keller, Klaus
(2014).
DOI: https://doi.org/10.1002/2014GL059484
URL: http://onlinelibrary.wiley.com/doi/10.1002/2014GL0...
Abstract
Equilibrium climate sensitivity measures the long-term response of surface temperature to changes in atmospheric CO2. The range of climate sensitivities in the IPCC AR5 Report is unchanged from that published almost 30 years earlier in the Charney Report. We conduct perfect-model experiments using an energy balance model to study the rate at which uncertainties might be reduced by observation of global temperature and ocean heat uptake. We find that a climate sensitivity of 1.5 <°C can be statistically distinguished from 3 °C by 2030; 3 °C from 4.5 °C by 2040; and 4.5 °C from 6 °C by 2065. Learning rates are slowest in the scenarios of greatest concern (high sensitivities), due to a longer ocean response time, which may have bearing on wait-and-see vs. precautionary mitigation policies. Learning rates are optimistic in presuming the availability of whole- ocean heat data, but pessimistic by using simple aggregated metrics and model physics.
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About
- Item ORO ID
- 40078
- Item Type
- Journal Item
- ISSN
- 1944-8007
- Project Funding Details
-
Funded Project Name Project ID Funding Body Program in Science, Technology, and Environmental Policy Not Set Not Set Network for Sustainable Climate Risk Management (SCRiM) NSF cooperative agreement GEO-1240507 Not Set - Keywords
- climate sensitivity; uncertainty; learning; feedback; transient; ocean heat
- Academic Unit or School
-
Faculty of Science, Technology, Engineering and Mathematics (STEM) > Environment, Earth and Ecosystem Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM) - Research Group
- ?? idii ??
- Copyright Holders
- © 2014 American Geophysical Union
- Depositing User
- Philip Holden