Abstract
How has the Atlantic Meridional Overturning Circulation (AMOC) varied over the past centuries and what is the risk of an anthropogenic AMOC collapse? We report probabilistic projections of the future climate which improve on previous AMOC projection studies by (i) greatly expanding the considered observational constraints and (ii) carefully sampling the tail areas of the parameter probability distribution function (pdf).We use a Bayesian inversion to constrain a simple model of the coupled climate, carbon cycle and AMOC systems using observations to derive multicentury hindcasts and projections. Our hindcasts show considerable skill in representing the observational constraints. We show that robust AMOC risk estimates can require carefully sampling the parameter pdfs. We find a low probability of experiencing an AMOC collapse within the 21st century for a business-as-usual emissions scenario. The probability of experiencing an AMOC collapse within two centuries is 1/10. The probability of crossing a forcing threshold and triggering a future AMOC collapse (by 2300) is approximately 1/30 in the 21st century and over 1/3 in the 22nd. Given the simplicity of the model structure and uncertainty in the forcing assumptions, our analysis should be considered a proof of concept and the quantitative conclusions subject to severe caveats.
Urban, Nathan M. (Dept. of Geosciences, Penn State Univ., University Park (United States)), e-mail: nurban@psu.edu;
Keller, Klaus;
[1]
Earth and Environmental Systems Inst., Penn State Univ. (United States))
- Dept. of Geosciences, Penn State Univ., University Park (United States)
Citation Formats
Urban, Nathan M. (Dept. of Geosciences, Penn State Univ., University Park (United States)), e-mail: nurban@psu.edu, Keller, Klaus, and Earth and Environmental Systems Inst., Penn State Univ. (United States)).
Probabilistic hindcasts and projections of the coupled climate, carbon cycle and Atlantic meridional overturning circulation system: a Bayesian fusion of century-scale observations with a simple model.
Sweden: N. p.,
2010.
Web.
doi:10.1111/J.1600-0870.2010.00471.X.
Urban, Nathan M. (Dept. of Geosciences, Penn State Univ., University Park (United States)), e-mail: nurban@psu.edu, Keller, Klaus, & Earth and Environmental Systems Inst., Penn State Univ. (United States)).
Probabilistic hindcasts and projections of the coupled climate, carbon cycle and Atlantic meridional overturning circulation system: a Bayesian fusion of century-scale observations with a simple model.
Sweden.
https://doi.org/10.1111/J.1600-0870.2010.00471.X
Urban, Nathan M. (Dept. of Geosciences, Penn State Univ., University Park (United States)), e-mail: nurban@psu.edu, Keller, Klaus, and Earth and Environmental Systems Inst., Penn State Univ. (United States)).
2010.
"Probabilistic hindcasts and projections of the coupled climate, carbon cycle and Atlantic meridional overturning circulation system: a Bayesian fusion of century-scale observations with a simple model."
Sweden.
https://doi.org/10.1111/J.1600-0870.2010.00471.X.
@misc{etde_1008074,
title = {Probabilistic hindcasts and projections of the coupled climate, carbon cycle and Atlantic meridional overturning circulation system: a Bayesian fusion of century-scale observations with a simple model}
author = {Urban, Nathan M. (Dept. of Geosciences, Penn State Univ., University Park (United States)), e-mail: nurban@psu.edu, Keller, Klaus, and Earth and Environmental Systems Inst., Penn State Univ. (United States))}
abstractNote = {How has the Atlantic Meridional Overturning Circulation (AMOC) varied over the past centuries and what is the risk of an anthropogenic AMOC collapse? We report probabilistic projections of the future climate which improve on previous AMOC projection studies by (i) greatly expanding the considered observational constraints and (ii) carefully sampling the tail areas of the parameter probability distribution function (pdf).We use a Bayesian inversion to constrain a simple model of the coupled climate, carbon cycle and AMOC systems using observations to derive multicentury hindcasts and projections. Our hindcasts show considerable skill in representing the observational constraints. We show that robust AMOC risk estimates can require carefully sampling the parameter pdfs. We find a low probability of experiencing an AMOC collapse within the 21st century for a business-as-usual emissions scenario. The probability of experiencing an AMOC collapse within two centuries is 1/10. The probability of crossing a forcing threshold and triggering a future AMOC collapse (by 2300) is approximately 1/30 in the 21st century and over 1/3 in the 22nd. Given the simplicity of the model structure and uncertainty in the forcing assumptions, our analysis should be considered a proof of concept and the quantitative conclusions subject to severe caveats.}
doi = {10.1111/J.1600-0870.2010.00471.X}
journal = []
issue = {5}
volume = {62A}
place = {Sweden}
year = {2010}
month = {Oct}
}
title = {Probabilistic hindcasts and projections of the coupled climate, carbon cycle and Atlantic meridional overturning circulation system: a Bayesian fusion of century-scale observations with a simple model}
author = {Urban, Nathan M. (Dept. of Geosciences, Penn State Univ., University Park (United States)), e-mail: nurban@psu.edu, Keller, Klaus, and Earth and Environmental Systems Inst., Penn State Univ. (United States))}
abstractNote = {How has the Atlantic Meridional Overturning Circulation (AMOC) varied over the past centuries and what is the risk of an anthropogenic AMOC collapse? We report probabilistic projections of the future climate which improve on previous AMOC projection studies by (i) greatly expanding the considered observational constraints and (ii) carefully sampling the tail areas of the parameter probability distribution function (pdf).We use a Bayesian inversion to constrain a simple model of the coupled climate, carbon cycle and AMOC systems using observations to derive multicentury hindcasts and projections. Our hindcasts show considerable skill in representing the observational constraints. We show that robust AMOC risk estimates can require carefully sampling the parameter pdfs. We find a low probability of experiencing an AMOC collapse within the 21st century for a business-as-usual emissions scenario. The probability of experiencing an AMOC collapse within two centuries is 1/10. The probability of crossing a forcing threshold and triggering a future AMOC collapse (by 2300) is approximately 1/30 in the 21st century and over 1/3 in the 22nd. Given the simplicity of the model structure and uncertainty in the forcing assumptions, our analysis should be considered a proof of concept and the quantitative conclusions subject to severe caveats.}
doi = {10.1111/J.1600-0870.2010.00471.X}
journal = []
issue = {5}
volume = {62A}
place = {Sweden}
year = {2010}
month = {Oct}
}