Long-Term Climate Commitments Projected with Climate

Metadata Label Value
Author(s) Plattner, G.-K., Knutti, Reto, Joos, F., Stocker, T.F., Bloh, W. von, Brovkin, V., Cameron, D., Driesschaert, E., Dutkiewicz, S., Eby, M., Edwards, N.R., Fichefet, T., Hargreaves, J.C., Jones, C.D., Loutre, M.F., Matthews, H.D., Mouchet, A., Müller, S.A., Nawrath, S., Price, A., Sokolov, A., Strassmann, K.M., Weaver, A.J.
Publication Type Journal Items, Publication Status: Published
Full Text Search SFX for a Full-Text version of this document
Import to Mendeley

Detailed Information

Metadata Field Content
Title Long-Term Climate Commitments Projected with Climate
Subtitle Carbon Cycle Models
Author(s) Plattner, G.-K.
Knutti, Reto
Joos, F.
Stocker, T.F.
Bloh, W. von
Brovkin, V.
Cameron, D.
Driesschaert, E.
Dutkiewicz, S.
Eby, M.
Edwards, N.R.
Fichefet, T.
Hargreaves, J.C.
Jones, C.D.
Loutre, M.F.
Matthews, H.D.
Mouchet, A.
Müller, S.A.
Nawrath, S.
Price, A.
Sokolov, A.
Strassmann, K.M.
Weaver, A.J.
Journal or Series Title Journal of climate
Volume Number 21
Issue Number 12
Start Page 2721
End Page 2751
ISSN 0894-8755
Publisher American Meteorological Society
Publication Place Boston, MA
Publication Date 2008
Abstract Eight earth system models of intermediate complexity (EMICs) are used to project climate change commitments for the recent Intergovernmental Panel on Climate Change’s (IPCC’s) Fourth Assessment Report (AR4). Simulations are run until the year 3000 a.d. and extend substantially farther into the future than conceptually similar simulations with atmosphere–ocean general circulation models (AOGCMs) coupled to carbon cycle models. In this paper the following are investigated: 1) the climate change commitment in response to stabilized greenhouse gases and stabilized total radiative forcing, 2) the climate change commitment in response to earlier CO2 emissions, and 3) emission trajectories for profiles leading to the stabilization of atmospheric CO2 and their uncertainties due to carbon cycle processes. Results over the twenty-first century compare reasonably well with results from AOGCMs, and the suite of EMICs proves well suited to complement more complex models. Substantial climate change commitments for sea level rise and global mean surface temperature increase after a stabilization of atmospheric greenhouse gases and radiative forcing in the year 2100 are identified. The additional warming by the year 3000 is 0.6–1.6 K for the low-CO2 IPCC Special Report on Emissions Scenarios (SRES) B1 scenario and 1.3–2.2 K for the high-CO2 SRES A2 scenario. Correspondingly, the post-2100 thermal expansion commitment is 0.3–1.1 m for SRES B1 and 0.5–2.2 m for SRES A2. Sea level continues to rise due to thermal expansion for several centuries after CO2 stabilization. In contrast, surface temperature changes slow down after a century. The meridional overturning circulation is weakened in all EMICs, but recovers to nearly initial values in all but one of the models after centuries for the scenarios considered. Emissions during the twenty-first century continue to impact atmospheric CO2 and climate even at year 3000. All models find that most of the anthropogenic carbon emissions are eventually taken up by the ocean (49%–62%) in year 3000, and that a substantial fraction (15%–28%) is still airborne even 900 yr after carbon emissions have ceased. Future stabilization of atmospheric CO2 and climate change requires a substantial reduction of CO2 emissions below present levels in all EMICs. This reduction needs to be substantially larger if carbon cycle–climate feedbacks are accounted for or if terrestrial CO2 fertilization is not operating. Large differences among EMICs are identified in both the response to increasing atmospheric CO2 and the response to climate change. This highlights the need for improved representations of carbon cycle processes in these models apart from the sensitivity to climate change. Sensitivity simulations with one single EMIC indicate that both carbon cycle and climate sensitivity related uncertainties on projected allowable emissions are substantial.
DOI 10.1175/2007JCLI1905.1
Additional Notes Manuscript received 21 February 2007, In final form 1 October 2007
Document Type Article
Publication Status Published
Language English
Assigned Organisational Unit(s) 03731
Organisational Unit(s)
NEBIS System Number 000490902
Source Database ID PP-43370
Description File Name MIME Type Size
No details could be found
There are no links available for this record.
This record has not been viewed during this period

  author = "Plattner, G.-K. and Knutti, Reto and Joos, F. and Stocker, T.F. and Bloh, W. von and Brovkin, V. and Cameron, D. and Driesschaert, E. and Dutkiewicz, S. and Eby, M. and Edwards, N.R. and Fichefet, T. and Hargreaves, J.C. and Jones, C.D. and Loutre, M.F. and Matthews, H.D. and Mouchet, A. and M{\"{u}}ller, S.A. and Nawrath, S. and Price, A. and Sokolov, A. and Strassmann, K.M. and Weaver, A.J.",
  title = "{L}ong-{T}erm {C}limate {C}ommitments {P}rojected with {C}limate: {C}arbon {C}ycle {M}odels",
  journal = "Journal of climate",
  year = 2008,
  volume = "21",
  number = "12",
  pages = "2721--2751",

E-Citations record created: Fri, 02 Apr 2010, 00:12:53 CET