Zobrazeno 1 - 10
of 69
pro vyhledávání: '"C. Contoux"'
Autor:
J. E. Weiffenbach, M. L. J. Baatsen, H. A. Dijkstra, A. S. von der Heydt, A. Abe-Ouchi, E. C. Brady, W.-L. Chan, D. Chandan, M. A. Chandler, C. Contoux, R. Feng, C. Guo, Z. Han, A. M. Haywood, Q. Li, X. Li, G. Lohmann, D. J. Lunt, K. H. Nisancioglu, B. L. Otto-Bliesner, W. R. Peltier, G. Ramstein, L. E. Sohl, C. Stepanek, N. Tan, J. C. Tindall, C. J. R. Williams, Q. Zhang, Z. Zhang
Publikováno v:
Climate of the Past, Vol 19, Pp 61-85 (2023)
The mid-Pliocene warm period (3.264–3.025 Ma) is the most recent geological period in which the atmospheric CO2 concentration was approximately equal to the concentration we measure today (ca. 400 ppm). Sea surface temperature (SST) proxies indicat
Externí odkaz:
https://doaj.org/article/0a22b6523a274734a40b7ae5cbd1e78a
Autor:
A. M. Oldeman, M. L. J. Baatsen, A. S. von der Heydt, H. A. Dijkstra, J. C. Tindall, A. Abe-Ouchi, A. R. Booth, E. C. Brady, W.-L. Chan, D. Chandan, M. A. Chandler, C. Contoux, R. Feng, C. Guo, A. M. Haywood, S. J. Hunter, Y. Kamae, Q. Li, X. Li, G. Lohmann, D. J. Lunt, K. H. Nisancioglu, B. L. Otto-Bliesner, W. R. Peltier, G. M. Pontes, G. Ramstein, L. E. Sohl, C. Stepanek, N. Tan, Q. Zhang, Z. Zhang, I. Wainer, C. J. R. Williams
Publikováno v:
Climate of the Past, Vol 17, Pp 2427-2450 (2021)
The mid-Pliocene warm period (3.264–3.025 Ma) is the most recent geological period during which atmospheric CO2 levels were similar to recent historical values (∼400 ppm). Several proxy reconstructions for the mid-Pliocene show highly reduced zon
Externí odkaz:
https://doaj.org/article/d46acf44fd7540139ae7c55c354a7a84
Autor:
E. Berntell, Q. Zhang, Q. Li, A. M. Haywood, J. C. Tindall, S. J. Hunter, Z. Zhang, X. Li, C. Guo, K. H. Nisancioglu, C. Stepanek, G. Lohmann, L. E. Sohl, M. A. Chandler, N. Tan, C. Contoux, G. Ramstein, M. L. J. Baatsen, A. S. von der Heydt, D. Chandan, W. R. Peltier, A. Abe-Ouchi, W.-L. Chan, Y. Kamae, C. J. R. Williams, D. J. Lunt, R. Feng, B. L. Otto-Bliesner, E. C. Brady
Publikováno v:
Climate of the Past, Vol 17, Pp 1777-1794 (2021)
The mid-Pliocene warm period (mPWP; ∼3.2 million years ago) is seen as the most recent time period characterized by a warm climate state, with similar to modern geography and ∼400 ppmv atmospheric CO2 concentration, and is therefore often conside
Externí odkaz:
https://doaj.org/article/02b4160ced3141e284cc47624998b7cc
Autor:
Z. Zhang, X. Li, C. Guo, O. H. Otterå, K. H. Nisancioglu, N. Tan, C. Contoux, G. Ramstein, R. Feng, B. L. Otto-Bliesner, E. Brady, D. Chandan, W. R. Peltier, M. L. J. Baatsen, A. S. von der Heydt, J. E. Weiffenbach, C. Stepanek, G. Lohmann, Q. Zhang, Q. Li, M. A. Chandler, L. E. Sohl, A. M. Haywood, S. J. Hunter, J. C. Tindall, C. Williams, D. J. Lunt, W.-L. Chan, A. Abe-Ouchi
Publikováno v:
Climate of the Past, Vol 17, Pp 529-543 (2021)
In the Pliocene Model Intercomparison Project Phase 2 (PlioMIP2), coupled climate models have been used to simulate an interglacial climate during the mid-Piacenzian warm period (mPWP; 3.264 to 3.025 Ma). Here, we compare the Atlantic Meridional Over
Externí odkaz:
https://doaj.org/article/35c336516f9f46e19a2a0484592631f3
Autor:
W. de Nooijer, Q. Zhang, Q. Li, X. Li, Z. Zhang, C. Guo, K. H. Nisancioglu, A. M. Haywood, J. C. Tindall, S. J. Hunter, H. J. Dowsett, C. Stepanek, G. Lohmann, B. L. Otto-Bliesner, R. Feng, L. E. Sohl, M. A. Chandler, N. Tan, C. Contoux, G. Ramstein, M. L. J. Baatsen, A. S. von der Heydt, D. Chandan, W. R. Peltier, A. Abe-Ouchi, W.-L. Chan, Y. Kamae, C. M. Brierley
Publikováno v:
Climate of the Past, Vol 16, Pp 2325-2341 (2020)
Palaeoclimate simulations improve our understanding of the climate, inform us about the performance of climate models in a different climate scenario, and help to identify robust features of the climate system. Here, we analyse Arctic warming in an e
Externí odkaz:
https://doaj.org/article/45ffd6281f3943e8bcfb97e79cacf97e
Autor:
A. M. Haywood, J. C. Tindall, H. J. Dowsett, A. M. Dolan, K. M. Foley, S. J. Hunter, D. J. Hill, W.-L. Chan, A. Abe-Ouchi, C. Stepanek, G. Lohmann, D. Chandan, W. R. Peltier, N. Tan, C. Contoux, G. Ramstein, X. Li, Z. Zhang, C. Guo, K. H. Nisancioglu, Q. Zhang, Q. Li, Y. Kamae, M. A. Chandler, L. E. Sohl, B. L. Otto-Bliesner, R. Feng, E. C. Brady, A. S. von der Heydt, M. L. J. Baatsen, D. J. Lunt
Publikováno v:
Climate of the Past, Vol 16, Pp 2095-2123 (2020)
The Pliocene epoch has great potential to improve our understanding of the long-term climatic and environmental consequences of an atmospheric CO2 concentration near ∼400 parts per million by volume. Here we present the large-scale features of Plio
Externí odkaz:
https://doaj.org/article/e324750e9a7743cc94547358d398759f
Publikováno v:
Climate of the Past, Vol 16, Pp 1-16 (2020)
The mid-Piacenzian warm period (3.264 to 3.025 Ma) is the most recent geological period with present-like atmospheric pCO2 and is thus expected to have exhibited a warm climate similar to or warmer than the present day. On the basis of understandin
Externí odkaz:
https://doaj.org/article/c14117212ad642ac813ccc2cfd3ecadd
Autor:
F. W. Howell, A. M. Haywood, B. L. Otto-Bliesner, F. Bragg, W.-L. Chan, M. A. Chandler, C. Contoux, Y. Kamae, A. Abe-Ouchi, N. A. Rosenbloom, C. Stepanek, Z. Zhang
Publikováno v:
Climate of the Past, Vol 12, Iss 3, Pp 749-767 (2016)
Eight general circulation models have simulated the mid-Pliocene warm period (mid-Pliocene, 3.264 to 3.025 Ma) as part of the Pliocene Modelling Intercomparison Project (PlioMIP). Here, we analyse and compare their simulation of Arctic sea ice for bo
Externí odkaz:
https://doaj.org/article/1cafe868493c4be5b4cafca77663e3d5
Autor:
A. M. Dolan, S. J. Hunter, D. J. Hill, A. M. Haywood, S. J. Koenig, B. L. Otto-Bliesner, A. Abe-Ouchi, F. Bragg, W.-L. Chan, M. A. Chandler, C. Contoux, A. Jost, Y. Kamae, G. Lohmann, D. J. Lunt, G. Ramstein, N. A. Rosenbloom, L. Sohl, C. Stepanek, H. Ueda, Q. Yan, Z. Zhang
Publikováno v:
Climate of the Past, Vol 11, Iss 3, Pp 403-424 (2015)
During an interval of the Late Pliocene, referred to here as the mid-Pliocene Warm Period (mPWP; 3.264 to 3.025 million years ago), global mean temperature was similar to that predicted for the end of this century, and atmospheric carbon dioxide conc
Externí odkaz:
https://doaj.org/article/f71a08cb5b1e449a86c181372f2564ad
Autor:
D. J. Hill, A. M. Haywood, D. J. Lunt, S. J. Hunter, F. J. Bragg, C. Contoux, C. Stepanek, L. Sohl, N. A. Rosenbloom, W.-L. Chan, Y. Kamae, Z. Zhang, A. Abe-Ouchi, M. A. Chandler, A. Jost, G. Lohmann, B. L. Otto-Bliesner, G. Ramstein, H. Ueda
Publikováno v:
Climate of the Past, Vol 10, Iss 1, Pp 79-90 (2014)
The Pliocene Model Intercomparison Project (PlioMIP) is the first coordinated climate model comparison for a warmer palaeoclimate with atmospheric CO2 significantly higher than pre-industrial concentrations. The simulations of the mid-Pliocene warm p
Externí odkaz:
https://doaj.org/article/1795f1a57cf74b1cad8d9859c6c9b6e9