Zobrazeno 1 - 10
of 14
pro vyhledávání: '"S. J. Koenig"'
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:
S. J. Koenig, A. M. Dolan, B. de Boer, E. J. Stone, D. J. Hill, R. M. DeConto, A. Abe-Ouchi, D. J. Lunt, D. Pollard, A. Quiquet, F. Saito, J. Savage, R. van de Wal
Publikováno v:
Climate of the Past, Vol 11, Iss 3, Pp 369-381 (2015)
The understanding of the nature and behavior of ice sheets in past warm periods is important for constraining the potential impacts of future climate change. The Pliocene warm period (between 3.264 and 3.025 Ma) saw global temperatures similar to tho
Externí odkaz:
https://doaj.org/article/1b0ab5fbe5944159bc64d66acb035ddc
Publikováno v:
Geoscientific Model Development, Vol 5, Iss 4, Pp 963-974 (2012)
During the mid-Pliocene warm period (3.264 to 3.025 million years ago), global mean temperature was similar to that predicted for the next century and atmospheric carbon dioxide concentrations were slightly higher than today. Sea level was also highe
Externí odkaz:
https://doaj.org/article/91bfbe24a5bb417ab3678033d800b7d5
Publikováno v:
Geoscientific Model Development, Vol 5, Iss 1, Pp 73-85 (2012)
The mid-Pliocene Warm Period (3.29 to 2.97 Ma BP) has been identified as an analogue for the future, with the potential to help understand climate processes in a warmer than modern world. Sets of climate proxies, combined to provide boundary conditio
Externí odkaz:
https://doaj.org/article/94ba4bdf1017466c9048cea32e5e95b1
Impact of reduced Arctic sea ice on Greenland ice sheet variability in a warmer than present climate
Publikováno v:
Geophysical Research Letters. 41:3933-3942
A global climate model with interactive vegetation and a coupled ice sheet-shelf component is used to test the response of the Greenland ice sheet (GIS) to increased sea surface temperatures (SSTs) and reduced sea ice (SI) cover during the mid-Plioce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::212541e65556242ed4c315450efe517c
https://doi.org/10.1002/2014gl059770
https://doi.org/10.1002/2014gl059770
Autor:
Catalina Gebhardt, Andrei Andreev, Norbert R. Nowaczyk, Eeva Haltia, Pavel S Minyuk, Pavel E. Tarasov, Peter Rosén, Ulrike Herzschuh, Carsten Meyer-Jacob, Volker Wennrich, S. J. Koenig, Martin Melles, Jeff Snyder, Robert M. DeConto, Timothy L Cook, Julie Brigham-Grette
Publikováno v:
Science
From Russia with Lovely Data Climate and the atmospheric concentration of CO 2 are closely linked. Brigham-Grette et al. (p. 1421 , published online 9 May) present data from Lake El'gygytgyn, in northeast Arctic Russia, that shows how climate varied
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::95079a996250dd1eb53695bb639bf8aa
https://doi.org/10.1126/science.1233137
https://doi.org/10.1126/science.1233137
Publikováno v:
Geoscientific Model Development, Vol 5, Iss 1, Pp 73-85 (2012)
The mid-Pliocene Warm Period (3.29 to 2.97 Ma BP) has been identified as an analogue for the future, with the potential to help understand climate processes in a warmer than modern world. Sets of climate proxies, combined to provide boundary conditio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::22442eef7a0247ea36a88476b3287c3a
http://www.geosci-model-dev.net/5/73/2012/gmd-5-73-2012.pdf
http://www.geosci-model-dev.net/5/73/2012/gmd-5-73-2012.pdf
Publikováno v:
Climate Dynamics. 37:1247-1268
The timing and nature of ice sheet variations on Greenland over the last ∼5 million years remain largely uncertain. Here, we use a coupled climate-vegetation-ice sheet model to determine the climatic sensitivity of Greenland to combined sets of ext
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7eb0e938f62aeab1677ec5b082247d7f
https://doi.org/10.1007/s00382-011-1050-0
https://doi.org/10.1007/s00382-011-1050-0
Autor:
Hiroaki Ueda, Fran Bragg, Bette L. Otto-Bliesner, Wing-Le Chan, Linda E. Sohl, Daniel J. Hill, Nan Rosenbloom, Ayako Abe-Ouchi, Mark A. Chandler, Aisling M. Dolan, Gerrit Lohmann, Daniel J. Lunt, Zhongshi Zhang, Alan M. Haywood, Youichi Kamae, Anne Jost, Christian Stepanek, Qing Yan, Gilles Ramstein, S. J. Koenig, Camille Contoux, Stephen J. Hunter
Publikováno v:
Dolan, A M, Hunter, S J, Hill, D J, Haywood, A M, Koenig, S J, Otto-Bliesner, B L, Abe-Ouchi, A, Bragg, F J, Chan, W-L, Chandler, M A, Contoux, C, Jost, A, Kamae, Y, Lohmann, G, Lunt, D J, Ramstein, G, Rosenbloom, N A, Sohl, L, Stepanek, C, Ueda, H, Yan, Q & Zhang, Z 2015, ' Using results from the PlioMIP ensemble to investigate the Greenland Ice Sheet during the mid-Pliocene Warm Period ', Climate of the Past, vol. 11, no. 3, pp. 403-424 . https://doi.org/10.5194/cp-11-403-2015
Climate of the Past
Climate of the Past, 2015, 11 (3), pp.403-424. ⟨10.5194/cp-11-403-2015⟩
Climate of the Past Discussions
Climate of the Past Discussions, European Geosciences Union (EGU), 2015, 11 (3), pp.403-424. ⟨10.5194/cp-11-403-2015⟩
Climate of the Past, European Geosciences Union (EGU), 2015, 11 (3), pp.403-424. ⟨10.5194/cp-11-403-2015⟩
Climate of the Past, Vol 11, Iss 3, Pp 403-424 (2015)
EPIC3Climate of the Past, COPERNICUS GESELLSCHAFT MBH, 11, pp. 403-424, ISSN: 1814-9324
Climate of the Past
Climate of the Past, 2015, 11 (3), pp.403-424. ⟨10.5194/cp-11-403-2015⟩
Climate of the Past Discussions
Climate of the Past Discussions, European Geosciences Union (EGU), 2015, 11 (3), pp.403-424. ⟨10.5194/cp-11-403-2015⟩
Climate of the Past, European Geosciences Union (EGU), 2015, 11 (3), pp.403-424. ⟨10.5194/cp-11-403-2015⟩
Climate of the Past, Vol 11, Iss 3, Pp 403-424 (2015)
EPIC3Climate of the Past, COPERNICUS GESELLSCHAFT MBH, 11, pp. 403-424, ISSN: 1814-9324
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://explore.openaire.eu/search/publication?articleId=doi_dedup___::fdaf4b142fa7025e92787e2557c4fc37
https://research-information.bris.ac.uk/en/publications/c9d4362c-5cfc-423b-9516-5b020731ad44
https://research-information.bris.ac.uk/en/publications/c9d4362c-5cfc-423b-9516-5b020731ad44
Autor:
S. J. Koenig, Ayako Abe-Ouchi, Daniel J. Hill, Qing Yan, Yoichi Kamae, Camille Contoux, Wing-Le Chan, Stephen J. Hunter, Linda E. Sohl, Alan M. Haywood, Gilles Ramstein, Daniel J. Lunt, Hiroaki Ueda, Bette L. Otto-Bliesner, Nan Rosenbloom, Fran Bragg, Christian Stepanek, Zhongshi Zhang, Gerrit Lohmann, Mark A. Chandler, Anne Jost, Aisling M. Dolan
During the mid-Pliocene Warm Period (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 concentrations were higher than pre-industrial levels. Sea level
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a9cc2d9eef76034630bc0a97f993d29b
https://doi.org/10.5194/cpd-10-3483-2014
https://doi.org/10.5194/cpd-10-3483-2014