Zobrazeno 1 - 10
of 35
pro vyhledávání: '"Willem P. Sijp"'
Autor:
David K. Hutchinson, Helen K. Coxall, Daniel J. Lunt, Margret Steinthorsdottir, Agatha M. de Boer, Michiel Baatsen, Anna von der Heydt, Matthew Huber, Alan T. Kennedy-Asser, Lutz Kunzmann, Jean-Baptiste Ladant, Caroline H. Lear, Karolin Moraweck, Paul N. Pearson, Emanuela Piga, Matthew J. Pound, Ulrich Salzmann, Howie D. Scher, Willem P. Sijp, Kasia K. Śliwińska, Paul A. Wilson, Zhongshi Zhang
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7fe417bf26bba0698d10095f2999af12
https://doi.org/10.5194/cp-2020-68-supplement
https://doi.org/10.5194/cp-2020-68-supplement
Autor:
David K. Hutchinson, Helen K. Coxall, Daniel J. Lunt, Margret Steinthorsdottir, Agatha M. de Boer, Michiel Baatsen, Anna von der Heydt, Matthew Huber, Alan T. Kennedy-Asser, Lutz Kunzmann, Jean-Baptiste Ladant, Caroline H. Lear, Karolin Moraweck, Paul N. Pearson, Emanuela Piga, Matthew J. Pound, Ulrich Salzmann, Howie D. Scher, Willem P. Sijp, Kasia K. Śliwińska, Paul A. Wilson, Zhongshi Zhang
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 ∼
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::04b4b0bd06a6bd43b34ae5ea4925227d
https://orca.cardiff.ac.uk/id/eprint/136888/8/cp-17-269-2021.pdf
https://orca.cardiff.ac.uk/id/eprint/136888/8/cp-17-269-2021.pdf
Publikováno v:
Journal of Climate. 30:5775-5790
The response of the global climate system to Drake Passage (DP) closure is examined using a fully coupled ocean–atmosphere–ice model. Unlike most previous studies, a full three-dimensional atmospheric general circulation model is included with a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9ca7da96352da5584fa66d5569fc1344
https://doi.org/10.1175/jcli-d-15-0554.1
https://doi.org/10.1175/jcli-d-15-0554.1
Autor:
Willem P. Sijp, Matthew H. England
Publikováno v:
Climate of the Past, Vol 12, Iss 2, Pp 543-552 (2016)
We examine whether the reduced meridional temperature gradients of past greenhouse climates might have reduced oceanic overturning, leading to a more quiescent subsurface ocean. A substantial reduction of the pole-to-Equator temperature difference is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::020c704823c91e59b6f30d6cb28fe77f
http://www.clim-past.net/12/543/2016/cp-12-543-2016.pdf
http://www.clim-past.net/12/543/2016/cp-12-543-2016.pdf
Publikováno v:
Geophysical Research Letters. 42:4940-4948
Heat transport between the surface and deep ocean strongly influences transient climate change. Mechanisms setting this transport are investigated using coupled climate models and by projecting ocean circulation into the temperature-depth diagram. In
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cc1a81225437dce7eed93b96162cc641
https://doi.org/10.1002/2015gl064156
https://doi.org/10.1002/2015gl064156
Autor:
Marie-Louise Ward, Katrin J. Meissner, K. Alexander, Timothy J. Bralower, Willem P. Sijp, T. Dunkley Jones
Publikováno v:
Paleoceanography. 29:946-963
The Paleocene-Eocene Thermal Maximum (PETM), ∼55.53 million years before present, was an abrupt warming event that involved profound changes in the carbon cycle and led to major perturbations of marine and terrestrial ecosystems. The PETM was trigg
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8319feaecf79c5c7185a158deac32c3c
https://doi.org/10.1002/2014pa002650
https://doi.org/10.1002/2014pa002650
Publikováno v:
Climate Dynamics. 43:1661-1676
A stochastic analytical model of the Atlantic meridional overturning circulation (AMOC) is presented and tested against climate model data. AMOC stability is characterised by an underlying deterministic differential equation describing the evolution
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::86b877231bcf3b81fd5c1b01a0b407d7
https://doi.org/10.1007/s00382-013-1992-5
https://doi.org/10.1007/s00382-013-1992-5
Publikováno v:
Journal of Physical Oceanography. 43:2095-2112
Vertical transport of heat by ocean circulation is investigated using a coupled climate model and novel thermodynamic methods. Using a streamfunction in temperature–depth coordinates, cells are identified by whether they are thermally direct (flux
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d83dce2879a131e30f5f4338776c0dd8
https://doi.org/10.1175/jpo-d-12-0179.1
https://doi.org/10.1175/jpo-d-12-0179.1
Publikováno v:
Journal of Climate. 26:2651-2667
The North Atlantic climate response to the catastrophic drainage of proglacial Lake Agassiz into the Labrador Sea is analyzed with coarse and ocean eddy-permitting versions of a global coupled climate model. The North Atlantic climate response is qua
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4f653a3f513f5cdad67e43fe9d866e5f
https://doi.org/10.1175/jcli-d-11-00683.1
https://doi.org/10.1175/jcli-d-11-00683.1
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7be1ebafeaec80ce21ad508a1156fd68
https://doi.org/10.1130/abs/2016am-286792
https://doi.org/10.1130/abs/2016am-286792