Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Julia C. Tindall"'
Autor:
Ran Feng, Tripti Bhattacharya, Bette L. Otto-Bliesner, Esther C. Brady, Alan M. Haywood, Julia C. Tindall, Stephen J. Hunter, Ayako Abe-Ouchi, Wing-Le Chan, Masa Kageyama, Camille Contoux, Chuncheng Guo, Xiangyu Li, Gerrit Lohmann, Christian Stepanek, Ning Tan, Qiong Zhang, Zhongshi Zhang, Zixuan Han, Charles J. R. Williams, Daniel J. Lunt, Harry J. Dowsett, Deepak Chandan, W. Richard Peltier
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-11 (2022)
In contrast to future projections, paleoclimate records often find wetter subtropics in tandem with elevated CO2. Here, a compilation of proxies and simulations are used to reveal the climate dynamics and feedbacks responsible for generating wet subt
Externí odkaz:
https://doaj.org/article/38526b15bb344822b5f9a956f28a82a6
Autor:
Max D. Holloway, Louise C. Sime, Joy S. Singarayer, Julia C. Tindall, Pete Bunch, Paul J. Valdes
Publikováno v:
Nature Communications, Vol 7, Iss 1, Pp 1-9 (2016)
The peak in Antarctic ice core isotope values, 128,000 years before present, was concurrent with a significantly warmer-than-present Antarctic climate. Here, the authors show that this isotope maximum was associated with a major retreat of sea ice an
Externí odkaz:
https://doaj.org/article/bec92aed13d14acc9dec2240af183665
Autor:
Lauren E. Burton, Alan M. Haywood, Julia C. Tindall, Aisling M. Dolan, Daniel J. Hill, Ayako Abe-Ouchi, Wing-Le Chan, Deepak Chandan, Ran Feng, Stephen J. Hunter, Xiangyu Li, W. Richard Peltier, Ning Tan, Christian Stepanek, Zhongshi Zhang
Publikováno v:
EPIC3Climate of the Past, Copernicus GmbH, 19(3), pp. 747-764, ISSN: 1814-9324
Understanding the dominant climate forcings in the Pliocene is crucial to assessing the usefulness of the Pliocene as an analogue for our warmer future. Here, we implement a novel yet simple linear factorisation method to assess the relative influenc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aa6a269aa94f9419c89f5eab34adc9a8
https://cp.copernicus.org/articles/19/747/2023/
https://cp.copernicus.org/articles/19/747/2023/
Autor:
Xin Ren, Daniel J. Lunt, Erica Hendy, Anna von der Heydt, Ayako Abe-Ouchi, Bette L. Otto-Bliesner, Charles J. R. Williams, Christian Stepanek, Chuncheng Guo, Deepak Chandan, Gerrit Lohmann, Julia C. Tindall, Linda E. Sohl, Mark A. Chandler, Masa Kageyama, Michiel L. J. Baatsen, Ning Tan, Qiong Zhang, Ran Feng, Wing-Le Chan, W. Richard Peltier, Xiangyu Li, Youichi Kamae, Zhongshi Zhang, Alan M. Haywood
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1dab12ff0a1f9f0d6dff9bade7307d60
https://doi.org/10.5194/egusphere-2022-1281-supplement
https://doi.org/10.5194/egusphere-2022-1281-supplement
Autor:
Xin Ren, Daniel J. Lunt, Erica Hendy, Anna von der Heydt, Ayako Abe-Ouchi, Bette L. Otto-Bliesner, Charles J. R. Williams, Christian Stepanek, Chuncheng Guo, Deepak Chandan, Gerrit Lohmann, Julia C. Tindall, Linda E. Sohl, Mark A. Chandler, Masa Kageyama, Michiel L. J. Baatsen, Ning Tan, Qiong Zhang, Ran Feng, Wing-Le Chan, W. Richard Peltier, Xiangyu Li, Youichi Kamae, Zhongshi Zhang, Alan M. Haywood
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-Pliocene (from 3.264 to 3.025 million years before present), atm
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::28d24c931ba4f374ea7eb6fd81a523a1
https://doi.org/10.5194/egusphere-2022-1281
https://doi.org/10.5194/egusphere-2022-1281
Reconciling palaeodata with model simulations of the Pliocene climate is essential for understanding a world with atmospheric CO2 concentration near 400 ppmv (parts per million by volume). Both models and data indicate an amplified warming of the hig
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::49326e52531780d11307a25b2835ec81
https://cp.copernicus.org/articles/18/1385/2022/
https://cp.copernicus.org/articles/18/1385/2022/
Autor:
Julia E. Weiffenbach, Michiel L. J. Baatsen, Henk A. Dijkstra, Anna S. von der Heydt, Ayako Abe-Ouchi, Esther C. Brady, Wing-Le Chan, Deepak Chandan, Mark A. Chandler, Camille Contoux, Ran Feng, Chuncheng Guo, Zixuan Han, Alan M. Haywood, Qiang Li, Xiangyu Li, Gerrit Lohmann, Daniel J. Lunt, Kerim H. Nisancioglu, Bette L. Otto-Bliesner, W. Richard Peltier, Gilles Ramstein, Linda E. Sohl, Christian Stepanek, Ning Tan, Julia C. Tindall, Charles J. R. Williams, Qiong Zhang, Zhongshi Zhang
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7aba63db21378c4d486db779bb4e02a6
https://doi.org/10.5194/cp-2022-35-supplement
https://doi.org/10.5194/cp-2022-35-supplement
Autor:
Julia E. Weiffenbach, Michiel L. J. Baatsen, Henk A. Dijkstra, Anna S. von der Heydt, Ayako Abe-Ouchi, Esther C. Brady, Wing-Le Chan, Deepak Chandan, Mark A. Chandler, Camille Contoux, Ran Feng, Chuncheng Guo, Zixuan Han, Alan M. Haywood, Qiang Li, Xiangyu Li, Gerrit Lohmann, Daniel J. Lunt, Kerim H. Nisancioglu, Bette L. Otto-Bliesner, W. Richard Peltier, Gilles Ramstein, Linda E. Sohl, Christian Stepanek, Ning Tan, Julia C. Tindall, Charles J. R. Williams, Qiong Zhang, Zhongshi Zhang
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://explore.openaire.eu/search/publication?articleId=doi_________::0f6c35c5a53de88e519dd5dbbe2b8dce
https://doi.org/10.5194/cp-2022-35
https://doi.org/10.5194/cp-2022-35
Reconciling palaeodata with model simulations of the Pliocene climate is essential for understanding a world with atmospheric CO2 concentration near 400 parts per million by volume. Both models and data indicate an amplified warming of the high latit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::441c151491fd14892e2bfedfea9cdae1
https://cp.copernicus.org/preprints/cp-2021-186/
https://cp.copernicus.org/preprints/cp-2021-186/