Zobrazeno 1 - 8
of 8
pro vyhledávání: '"H. K. Coxall"'
Autor:
N. Wunderling, A. S. von der Heydt, Y. Aksenov, S. Barker, R. Bastiaansen, V. Brovkin, M. Brunetti, V. Couplet, T. Kleinen, C. H. Lear, J. Lohmann, R. M. Roman-Cuesta, S. Sinet, D. Swingedouw, R. Winkelmann, P. Anand, J. Barichivich, S. Bathiany, M. Baudena, J. T. Bruun, C. M. Chiessi, H. K. Coxall, D. Docquier, J. F. Donges, S. K. J. Falkena, A. K. Klose, D. Obura, J. Rocha, S. Rynders, N. J. Steinert, M. Willeit
Publikováno v:
Earth System Dynamics, Vol 15, Pp 41-74 (2024)
Climate tipping elements are large-scale subsystems of the Earth that may transgress critical thresholds (tipping points) under ongoing global warming, with substantial impacts on the biosphere and human societies. Frequently studied examples of such
Externí odkaz:
https://doaj.org/article/2177790fd48f48adb242aee001aaa060
Autor:
J. R. Farmer, K. J. Keller, R. K. Poirier, G. S. Dwyer, M. F. Schaller, H. K. Coxall, M. O'Regan, T. M. Cronin
Publikováno v:
Climate of the Past, Vol 19, Pp 555-578 (2023)
The oxygen isotopic composition of benthic foraminiferal tests (δ18Ob) is one of the pre-eminent tools for correlating marine sediments and interpreting past terrestrial ice volume and deep-ocean temperatures. Despite the prevalence of δ18Ob applic
Externí odkaz:
https://doaj.org/article/3edbc8f0c8ba405b83658f7b461196df
Sea surface temperature evolution of the North Atlantic Ocean across the Eocene–Oligocene transition
Publikováno v:
Climate of the Past, Vol 19, Pp 123-140 (2023)
A major step in the long-term Cenozoic evolution toward a glacially driven climate occurred at the Eocene–Oligocene transition (EOT), ∼34.44 to 33.65 million years ago (Ma). Evidence for high-latitude cooling and increased latitudinal temperature
Externí odkaz:
https://doaj.org/article/faf98b7b1bb248a1a63fd13b4252d2aa
Autor:
D. J. Lunt, F. Bragg, W.-L. Chan, D. K. Hutchinson, J.-B. Ladant, P. Morozova, I. Niezgodzki, S. Steinig, Z. Zhang, J. Zhu, A. Abe-Ouchi, E. Anagnostou, A. M. de Boer, H. K. Coxall, Y. Donnadieu, G. Foster, G. N. Inglis, G. Knorr, P. M. Langebroek, C. H. Lear, G. Lohmann, C. J. Poulsen, P. Sepulchre, J. E. Tierney, P. J. Valdes, E. M. Volodin, T. Dunkley Jones, C. J. Hollis, M. Huber, B. L. Otto-Bliesner
Publikováno v:
Climate of the Past, Vol 17, Pp 203-227 (2021)
We present results from an ensemble of eight climate models, each of which has carried out simulations of the early Eocene climate optimum (EECO, ∼ 50 million years ago). These simulations have been carried out in the framework of the Deep-Time Mod
Externí odkaz:
https://doaj.org/article/7b6841f438e54b4f9d2617c7b44cdd2b
Autor:
D. K. Hutchinson, H. K. Coxall, D. J. Lunt, M. Steinthorsdottir, A. M. de Boer, M. Baatsen, A. von der Heydt, M. Huber, A. T. Kennedy-Asser, L. Kunzmann, J.-B. Ladant, C. H. Lear, K. Moraweck, P. N. Pearson, E. Piga, M. J. Pound, U. Salzmann, H. D. Scher, W. P. Sijp, K. K. Śliwińska, P. A. Wilson, Z. Zhang
Publikováno v:
Climate of the Past, Vol 17, Pp 269-315 (2021)
The Eocene–Oligocene transition (EOT) was a climate shift from a largely ice-free greenhouse world to an icehouse climate, involving the first major glaciation of Antarctica and global cooling occurring ∼34 million years ago (Ma) and lasting ∼7
Externí odkaz:
https://doaj.org/article/7b4ca81a6eb84d0a8275a4fd2dba06c9
Autor:
K. M. Edgar, S. M. Bohaty, H. K. Coxall, P. R. Bown, S. J. Batenburg, C. H. Lear, P. N. Pearson
Publikováno v:
Journal of Micropalaeontology, Vol 39, Pp 117-138 (2020)
The Middle Eocene Climatic Optimum (MECO) at ca. 40 Ma is one of the largest of the transient Eocene global warming events. However, it is relatively poorly known from tropical settings since few sites span the entirety of the MECO event and/or hos
Externí odkaz:
https://doaj.org/article/b929c6a493784df581e1030837149426
Publikováno v:
Climate of the Past, Vol 14, Pp 789-810 (2018)
The Eocene–Oligocene transition (EOT), which took place approximately 34 Ma ago, is an interval of great interest in Earth's climate history, due to the inception of the Antarctic ice sheet and major global cooling. Climate simulations of the tr
Externí odkaz:
https://doaj.org/article/5d12188667bf4a45a2da8b2ed14f9cb4
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