Zobrazeno 1 - 10
of 1 505
pro vyhledávání: '"Abe-Ouchi A"'
Autor:
Sebastian Steinig, Ayako Abe-Ouchi, Agatha M. de Boer, Wing-Le Chan, Yannick Donnadieu, David K. Hutchinson, Gregor Knorr, Jean-Baptiste Ladant, Polina Morozova, Igor Niezgodzki, Christopher J. Poulsen, Evgeny M. Volodin, Zhongshi Zhang, Jiang Zhu, David Evans, Gordon N. Inglis, A. Nele Meckler, Daniel J. Lunt
Publikováno v:
Scientific Data, Vol 11, Iss 1, Pp 1-13 (2024)
Abstract Paleoclimate model simulations provide reference data to help interpret the geological record and offer a unique opportunity to evaluate the performance of current models under diverse boundary conditions. Here, we present a dataset of 35 cl
Externí odkaz:
https://doaj.org/article/526a866f6b4f4a469dfd69c47630652c
Autor:
Yong Sun, Haibin Wu, Lin Ding, Lixin Chen, Christian Stepanek, Yan Zhao, Ning Tan, Baohuang Su, Xiayu Yuan, Wenchao Zhang, Bo Liu, Stephen Hunter, Alan Haywood, Ayako Abe-Ouchi, Bette Otto-Bliesner, Camille Contoux, Daniel J. Lunt, Aisling Dolan, Deepak Chandan, Gerrit Lohmann, Harry Dowsett, Julia Tindall, Michiel Baatsen, W. Richard Peltier, Qiang Li, Ran Feng, Ulrich Salzmann, Wing-Le Chan, Zhongshi Zhang, Charles J. R. Williams, Gilles Ramstein
Publikováno v:
npj Climate and Atmospheric Science, Vol 7, Iss 1, Pp 1-10 (2024)
Abstract The mid-Piacenzian warm period (MPWP, ~3.264–3.025 Ma) has gained widespread interest due to its partial analogy with future climate. However, quantitative data–model comparison of East Asian Summer Monsoon (EASM) precipitation during th
Externí odkaz:
https://doaj.org/article/a17bf41105bb4dd0bbb313e85f2643de
Autor:
Hélène Seroussi, Tyler Pelle, William H. Lipscomb, Ayako Abe‐Ouchi, Torsten Albrecht, Jorge Alvarez‐Solas, Xylar Asay‐Davis, Jean‐Baptiste Barre, Constantijn J. Berends, Jorge Bernales, Javier Blasco, Justine Caillet, David M. Chandler, Violaine Coulon, Richard Cullather, Christophe Dumas, Benjamin K. Galton‐Fenzi, Julius Garbe, Fabien Gillet‐Chaulet, Rupert Gladstone, Heiko Goelzer, Nicholas Golledge, Ralf Greve, G. Hilmar Gudmundsson, Holly Kyeore Han, Trevor R. Hillebrand, Matthew J. Hoffman, Philippe Huybrechts, Nicolas C. Jourdain, Ann Kristin Klose, Petra M. Langebroek, Gunter R. Leguy, Daniel P. Lowry, Pierre Mathiot, Marisa Montoya, Mathieu Morlighem, Sophie Nowicki, Frank Pattyn, Antony J. Payne, Aurélien Quiquet, Ronja Reese, Alexander Robinson, Leopekka Saraste, Erika G. Simon, Sainan Sun, Jake P. Twarog, Luke D. Trusel, Benoit Urruty, Jonas VanBreedam, Roderik S. W. van deWal, Yu Wang, Chen Zhao, Thomas Zwinger
Publikováno v:
Earth's Future, Vol 12, Iss 9, Pp n/a-n/a (2024)
Abstract The Ice Sheet Model Intercomparison Project for CMIP6 (ISMIP6) is the primary effort of CMIP6 (Coupled Model Intercomparison Project–Phase 6) focusing on ice sheets, designed to provide an ensemble of process‐based projections of the ice
Externí odkaz:
https://doaj.org/article/f85068d514034cbdac91ead931b6e5bb
Autor:
Kodama, Takanori, Takasuka, Daisuke, Sherriff-Tadano, Sam, Kuroda, Takeshi, Miyakawa, Tomoki, Abe-Ouchi, Ayako, Satoh, Masaki
Planetary climates are strongly affected by planetary orbital parameters such as obliquity, eccentricity, and precession. In exoplanetary systems, exo-terrestrial planets should have various obliquities. High-obliquity planets would have extreme seas
Externí odkaz:
http://arxiv.org/abs/2210.05094
Autor:
J. E. Weiffenbach, H. A. Dijkstra, A. S. von der Heydt, A. Abe-Ouchi, W.-L. Chan, D. Chandan, R. Feng, A. M. Haywood, S. J. Hunter, X. Li, B. L. Otto-Bliesner, W. R. Peltier, C. Stepanek, N. Tan, J. C. Tindall, Z. Zhang
Publikováno v:
Climate of the Past, Vol 20, Pp 1067-1086 (2024)
During the mid-Pliocene warm period (mPWP; 3.264–3.025 Ma), atmospheric CO2 concentrations were approximately 400 ppm, and the Antarctic Ice Sheet was substantially reduced compared to today. Antarctica is surrounded by the Southern Ocean, which pl
Externí odkaz:
https://doaj.org/article/8daab18e584f4a1aa76fe43328a36d98
Autor:
B. Snoll, R. Ivanovic, L. Gregoire, S. Sherriff-Tadano, L. Menviel, T. Obase, A. Abe-Ouchi, N. Bouttes, C. He, F. He, M. Kapsch, U. Mikolajewicz, J. Muglia, P. Valdes
Publikováno v:
Climate of the Past, Vol 20, Pp 789-815 (2024)
The last deglaciation (∼20–11 ka BP) is a period of a major, long-term climate transition from a glacial to interglacial state that features multiple centennial- to decadal-scale abrupt climate variations whose root cause is still not fully under
Externí odkaz:
https://doaj.org/article/75936d5b12964583bbfbb217f772b4a1
Publikováno v:
Climate of the Past, Vol 20, Pp 769-787 (2024)
Atmospheric carbon dioxide concentration (pCO2) has increased by approximately 80 ppm from the Last Glacial Maximum (LGM) to the early Holocene. The change in this atmospheric greenhouse gas is recognized as a climate system response to gradual chang
Externí odkaz:
https://doaj.org/article/03e77968a812476aa72c6068475faa89
Autor:
H. Seroussi, V. Verjans, S. Nowicki, A. J. Payne, H. Goelzer, W. H. Lipscomb, A. Abe-Ouchi, C. Agosta, T. Albrecht, X. Asay-Davis, A. Barthel, R. Calov, R. Cullather, C. Dumas, B. K. Galton-Fenzi, R. Gladstone, N. R. Golledge, J. M. Gregory, R. Greve, T. Hattermann, M. J. Hoffman, A. Humbert, P. Huybrechts, N. C. Jourdain, T. Kleiner, E. Larour, G. R. Leguy, D. P. Lowry, C. M. Little, M. Morlighem, F. Pattyn, T. Pelle, S. F. Price, A. Quiquet, R. Reese, N.-J. Schlegel, A. Shepherd, E. Simon, R. S. Smith, F. Straneo, S. Sun, L. D. Trusel, J. Van Breedam, P. Van Katwyk, R. S. W. van de Wal, R. Winkelmann, C. Zhao, T. Zhang, T. Zwinger
Publikováno v:
The Cryosphere, Vol 17, Pp 5197-5217 (2023)
The Antarctic Ice Sheet represents the largest source of uncertainty in future sea level rise projections, with a contribution to sea level by 2100 ranging from −5 to 43 cm of sea level equivalent under high carbon emission scenarios estimated by t
Externí odkaz:
https://doaj.org/article/602d0106f5dc44e2a4a46926008676ae
The climates of terrestrial planets with a small amount of water on their surface, called land planets, are significantly different from the climates of planets having a large amount of surface water. Land planets have a higher runaway greenhouse thr
Externí odkaz:
http://arxiv.org/abs/2111.12913
Autor:
X. Ren, D. J. Lunt, E. Hendy, A. von der Heydt, A. Abe-Ouchi, B. Otto-Bliesner, C. J. R. Williams, C. Stepanek, C. Guo, D. Chandan, G. Lohmann, J. C. Tindall, L. E. Sohl, M. A. Chandler, M. Kageyama, M. L. J. Baatsen, N. Tan, Q. Zhang, R. Feng, S. Hunter, W.-L. Chan, W. R. Peltier, X. Li, Y. Kamae, Z. Zhang, A. M. Haywood
Publikováno v:
Climate of the Past, Vol 19, Pp 2053-2077 (2023)
The Maritime Continent (MC) forms the western boundary of the tropical Pacific Ocean, and relatively small changes in this region can impact the climate locally and remotely. In the mid-Piacenzian warm period of the Pliocene (mPWP; 3.264 to 3.025 Ma)
Externí odkaz:
https://doaj.org/article/986ecfa3dd4e4bd0b0d5f5e8130ffc59