Zobrazeno 1 - 10
of 83
pro vyhledávání: '"Luke C Skinner"'
Autor:
Vasiliki Margari, Luke C. Skinner, Laurie Menviel, Emilie Capron, Rachael H. Rhodes, Maryline J. Mleneck-Vautravers, Mohamed M. Ezat, Belen Martrat, Joan O. Grimalt, David A. Hodell, Polychronis C. Tzedakis
Publikováno v:
Communications Earth & Environment, Vol 1, Iss 1, Pp 1-9 (2020)
Interstadial North Atlantic warming during the last glacial period involved the operation of both fast and slow components of the coupled atmosphere–ocean–sea-ice system, according to analyses from the Portuguese Margin and climate model simulati
Externí odkaz:
https://doaj.org/article/9bf04e66bc204733b65255d4e3dc8bcc
Autor:
Francesco Muschitiello, William J. D’Andrea, Andreas Schmittner, Timothy J. Heaton, Nicholas L. Balascio, Nicole deRoberts, Marc W. Caffee, Thomas E. Woodruff, Kees C. Welten, Luke C. Skinner, Margit H. Simon, Trond M. Dokken
Publikováno v:
Nature Communications, Vol 10, Iss 1, Pp 1-10 (2019)
The response time of North Atlantic climate to changes in high-latitude deep-water formation during the last deglaciation is still unclear. Here the authors show that gradual changes in Nordic Seas deep-water circulation systematically lead ahead of
Externí odkaz:
https://doaj.org/article/9585679d3e264897aef07f7f7c51c9a0
Autor:
Julia Gottschalk, Luke C. Skinner, Jörg Lippold, Hendrik Vogel, Norbert Frank, Samuel L. Jaccard, Claire Waelbroeck
Publikováno v:
Nature Communications, Vol 7, Iss 1, Pp 1-11 (2016)
Direct proxy evidence for the many explanations for past millennial-scale atmospheric CO2 changes remains scarce. Here, the authors show that changes in the efficiency of respired carbon storage in the deep Southern Ocean were linked to variations in
Externí odkaz:
https://doaj.org/article/adbb270b69ff48f2ba20b119e47fa43f
Autor:
David Hodell, Simon Crowhurst, Lucas Lourens, Vasiliki Margari, John Nicolson, James E. Rolfe, Luke C. Skinner, Nicola Thomas, Polychronis C. Tzedakis, Maryline J. Mleneck-Vautravers, Eric W. Wolff
Climate during the last glacial period was marked by abrupt instability on millennial timescales that included large swings of temperature in and around Greenland (Daansgard–Oeschger events) and smaller, more gradual changes in Antarctica (AIM even
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e62753a1c2ca002c62a0944aa0afe18e
https://www.repository.cam.ac.uk/handle/1810/347661
https://www.repository.cam.ac.uk/handle/1810/347661
Autor:
Luke C Skinner, Eric D. Galbraith
Publikováno v:
Annual Review of Marine Science. 12:559-586
Much of the global cooling during ice ages arose from changes in ocean carbon storage that lowered atmospheric CO2. A slew of mechanisms, both physical and biological, have been proposed as key drivers of these changes. Here we discuss the current un
Autor:
Lise Missiaen, Tobias Friedrich, Paul Spence, Jimin Yu, Kazuyo Tachikawa, Luke C Skinner, Laurie Menviel
While paleoproxy records and modelling studies consistently suggest that North Atlantic Deep Water (NADW) was shallower at the Last Glacial Maximum (LGM) than during pre-industrial times, its strength is still subject to debate partly due to differen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f5f44f752a1a62ee3cee50d5c8672899
https://hal.science/hal-03541566
https://hal.science/hal-03541566
Autor:
Sönke Szidat, Mervyn Greaves, Mohamed Ezat, Thomas M Marchitto, Tine Lander Rasmussen, Mathis P. Hain, Katarzyna Zamelczyk, James W. B. Rae, Luke C Skinner
Publikováno v:
Ezat, Mohamed M.; Rasmussen, Tine L.; Hain, Mathis P.; Greaves, Mervyn; Rae, James W. B.; Zamelczyk, Katarzyna; Marchitto, Thomas M.; Szidat, Sönke; Skinner, Luke C. (2021). Deep Ocean Storage of Heat and CO2 in the Fram Strait, Arctic Ocean During the Last Glacial Period. Paleoceanography and paleoclimatology, 36(8) American Geophysical Union 10.1029/2021PA004216
Funder: Tromsø Research Foundation : A31720
The Fram Strait is the only deep gateway between the Arctic Ocean and the Nordic Seas and thus is a key area to study past changes in ocean circulation and the marine carbon cycle. Here, we study deep
The Fram Strait is the only deep gateway between the Arctic Ocean and the Nordic Seas and thus is a key area to study past changes in ocean circulation and the marine carbon cycle. Here, we study deep
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::661b0eb66d0489e0cd1aa6bf7f6543f1
https://hdl.handle.net/10023/23685
https://hdl.handle.net/10023/23685
Publikováno v:
Paleoceanography and Paleoclimatology. 34:1807-1815
Marine radiocarbon dates, corrected for ocean‐atmosphere reservoir age offsets (R‐ages), are widely used to constrain marine chronologies. R‐ages also represent the surface boundary condition that links the ocean interior radiocarbon distributi
Publikováno v:
Earth and Planetary Science Letters, 518 . pp. 67-75.
Highlights • Strong ocean stratification in the Fram Strait during the late glacial (33–26 ka). • Breakup of ocean stratification during the LGM (26–20 ka) due to enhanced upwelling. • No extreme aging of >6000 yr in the Arctic Mediterranea
Autor:
Nicholas L. Balascio, Thomas E. Woodruff, Kees C. Welten, Trond Dokken, Francesco Muschitiello, William J. D'Andrea, Luke C Skinner, Nicole deRoberts, M.H. Simon, Marc W. Caffee, Timothy J Heaton, Andreas Schmittner
Publikováno v:
Nature Communications, Vol 10, Iss 1, Pp 1-10 (2019)
Nature Communications
Nature Communications
Constraining the response time of the climate system to changes in North Atlantic Deep Water (NADW) formation is fundamental to improving climate and Atlantic Meridional Overturning Circulation predictability. Here we report a new synchronization of