Zobrazeno 1 - 10
of 36
pro vyhledávání: '"Edward Gasson"'
Publikováno v:
Nature Communications, Vol 15, Iss 1, Pp 1-16 (2024)
Abstract Pliocene global temperatures periodically exceeded modern levels, offering insights into ice sheet sensitivity to warm climates. Ice-proximal geologic records from this period provide crucial but limited glimpses of Antarctic Ice Sheet behav
Externí odkaz:
https://doaj.org/article/b1dbbcfb8d6a42e79420ba7a0571ad1c
Autor:
Heather M. Stoll, Isabel Cacho, Edward Gasson, Jakub Sliwinski, Oliver Kost, Ana Moreno, Miguel Iglesias, Judit Torner, Carlos Perez-Mejias, Negar Haghipour, Hai Cheng, R. Lawrence Edwards
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-16 (2022)
Stalagmites from NW Iberia record the rapid demise of large ice sheets during the penultimate deglaciation, and reveal decadal-scale feedbacks between warming and ice melting.
Externí odkaz:
https://doaj.org/article/42f6facecb7249f2962fdcea8b0e8acf
Autor:
James W. Marschalek, Edward Gasson, Tina van de Flierdt, Claus-Dieter Hillenbrand, Martin J. Siegert, Liam Holder
Ice sheet models must be able to accurately simulate palaeo ice sheets to have confidence in their predictions of future Antarctic ice mass loss and resulting global sea-level rise, particularly over longer timescales. This requires accurate reconstr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a84f322afc348621230237b5b69a689b
https://doi.org/10.5194/gmd-2023-8
https://doi.org/10.5194/gmd-2023-8
Autor:
Chris D. Clark, Jeremy C. Ely, Richard C. A. Hindmarsh, Sarah Bradley, Adam Ignéczi, Derek Fabel, Colm Ó Cofaigh, Richard C. Chiverrell, James Scourse, Sara Benetti, Tom Bradwell, David J. A. Evans, David H. Roberts, Matt Burke, S. Louise Callard, Alicia Medialdea, Margot Saher, David Small, Rachel K. Smedley, Edward Gasson, Lauren Gregoire, Niall Gandy, Anna L. C. Hughes, Colin Ballantyne, Mark D. Bateman, Grant R. Bigg, Jenny Doole, Dayton Dove, Geoff A. T. Duller, Geraint T. H. Jenkins, Stephen L. Livingstone, Stephen McCarron, Steve Moreton, David Pollard, Daniel Praeg, Hans Petter Sejrup, Katrien J. J. Van Landeghem, Peter Wilson
Publikováno v:
Boreas
Boreas, 2022, 51 (4), pp.699-758. ⟨10.1111/bor.12594⟩
Boreas, 2022, Vol.51(4), pp.699-758 [Peer Reviewed Journal]
Clark, C D, Ely, J C, Hindmarsh, R C A, Bradley, S, Ignéczi, A, Fabel, D, Ó Cofaigh, C, Chiverrell, R C, Scourse, J, Benetti, S, Bradwell, T, Evans, D J A, Roberts, D H, Burke, M, Callard, S L, Medialdea, A, Saher, M, Small, D, Smedley, R K, Gasson, E, Gregoire, L, Gandy, N, Hughes, A L C, Ballantyne, C, Bateman, M D, Bigg, G R, Doole, J, Dove, D, Duller, G A T, Jenkins, G T H, Livingstone, S L, McCarron, S, Moreton, S, Pollard, D, Praeg, D, Sejrup, H P, Van Landeghem, K J J & Wilson, P 2022, ' Growth and retreat of the last British–Irish Ice Sheet, 31 000 to 15 000 years ago : the BRITICE-CHRONO reconstruction ', Boreas, vol. 51, no. 4, pp. 699-758 . https://doi.org/10.1111/bor.12594
Boreas, 2022, 51 (4), pp.699-758. ⟨10.1111/bor.12594⟩
Boreas, 2022, Vol.51(4), pp.699-758 [Peer Reviewed Journal]
Clark, C D, Ely, J C, Hindmarsh, R C A, Bradley, S, Ignéczi, A, Fabel, D, Ó Cofaigh, C, Chiverrell, R C, Scourse, J, Benetti, S, Bradwell, T, Evans, D J A, Roberts, D H, Burke, M, Callard, S L, Medialdea, A, Saher, M, Small, D, Smedley, R K, Gasson, E, Gregoire, L, Gandy, N, Hughes, A L C, Ballantyne, C, Bateman, M D, Bigg, G R, Doole, J, Dove, D, Duller, G A T, Jenkins, G T H, Livingstone, S L, McCarron, S, Moreton, S, Pollard, D, Praeg, D, Sejrup, H P, Van Landeghem, K J J & Wilson, P 2022, ' Growth and retreat of the last British–Irish Ice Sheet, 31 000 to 15 000 years ago : the BRITICE-CHRONO reconstruction ', Boreas, vol. 51, no. 4, pp. 699-758 . https://doi.org/10.1111/bor.12594
Funding information: This work was funded by the Natural Environment Research Council consortium grant BRITICE-CHRONO NE/J009768/1 and by the NERC Radio- carbon Facility and the NERC Cosmogenic Isotope Analysis Facility. The project benefited from th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7f6c9e34df57a51d8df8de3a8205650c
https://shura.shu.ac.uk/30706/1/clark2022boreas.pdf
https://shura.shu.ac.uk/30706/1/clark2022boreas.pdf
Autor:
Edward Gasson, Carrie Lear, Amy Sparkes, Ruthie Halberstadt, Rob DeConto, Matt Trevers, Tony Payne, David Pollard
Despite a major effort to constrain peak sea level during the mid-Pliocene warm period, uncertainties remain large. This interval is of interest because of the analogous CO2 concentration to present day and because of the potential retreat of a large
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::33a76becfcd787771f919eca9d7b8869
https://doi.org/10.5194/egusphere-gc10-pliocene-8
https://doi.org/10.5194/egusphere-gc10-pliocene-8
Autor:
David Pollard, Shaina Sadai, Edward Gasson, Robert E. Kopp, Alan Condron, Natalya Gomez, Erica Ashe, Richard B. Alley, Robert M. DeConto, Andrea Dutton, Isabella Velicogna, Daniel M. Gilford, Dawei Li
Publikováno v:
Nature. 593:83-89
The Paris Agreement aims to limit global mean warming in the twenty-first century to less than 2 degrees Celsius above preindustrial levels, and to promote further efforts to limit warming to 1.5 degrees Celsius1. The amount of greenhouse gas emissio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e1b5d7b432efdabf328862377120da36
https://doi.org/10.1038/s41586-021-03427-0
https://doi.org/10.1038/s41586-021-03427-0
Autor:
Edward Gasson, Heather Stoll
Compared with the intensely studied interval of the last glacial maximum and termination, significantly less attention has been given to the preceding glacial period and Termination 2. This is perhaps understandable as the Greenland ice cores do not
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::28cb5b33a78aa16aa1252efba76506c4
https://doi.org/10.5194/egusphere-egu22-7456
https://doi.org/10.5194/egusphere-egu22-7456
Tracing the provenance of Antarctic sediments yields unique insights into the form and flow of past ice sheets. However, sediment provenance studies are typically limited to qualitative interpretations by uncertainties regarding subglacial geology, g
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9a3af96c9b5b0c7f4ef0b47854e3f240
https://doi.org/10.5194/egusphere-egu22-1667
https://doi.org/10.5194/egusphere-egu22-1667
Autor:
A. R. Lewis, H. Chorley, Ross D. Powell, Fabio Florindo, Francesca Sangiorgi, Richard H. Levy, Christian Ohneiser, Trevor Williams, Laura De Santis, Molly O. Patterson, Tina van de Flierdt, Warren W. Dickinson, Nicholas R. Golledge, Carlota Escutia, Lara F. Pérez, Anna Ruth W. Halberstadt, David M. Harwood, Tim R Naish, Robert M. McKay, Edward Gasson, Aisling M. Dolan, Georgia R. Grant, Amelia E. Shevenell, Stephen R. Meyers, D. E. Kowalewski, Marjolaine Verret
Publikováno v:
Antarctic Climate Evolution ISBN: 9780128191095
The Miocene to Pliocene (Neogene) occurred between 23.04 and 2.58 million years ago and includes intervals of peak global warmth where Earth’s average surface temperature was up to 8℃ warmer than present. Major cooling steps also occurred, across
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ca164b651c752f654245fc60315ca844
https://doi.org/10.1016/b978-0-12-819109-5.00014-1
https://doi.org/10.1016/b978-0-12-819109-5.00014-1
Autor:
Robert M. DeConto, Florence Colleoni, Laura De Santis, Edward Gasson, Robert M. McKay, Bella Duncan, Tim R Naish, Richard H. Levy, Gary S. Wilson, Carlota Escutia
Publikováno v:
Antarctic Climate Evolution ISBN: 9780128191095
The Oligocene-Miocene transition (OMT) is one of the most enigmatic periods (~23.3–22.9 Ma) in Earth’s Cenozoic climate history. It is characterised in deep-sea benthic foraminiferal (δ18O) records by an increase of up to +1‰ spanning a 200–
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::78b9ef60462735b74e99a1c9d6d08e80
https://doi.org/10.1016/b978-0-12-819109-5.00013-x
https://doi.org/10.1016/b978-0-12-819109-5.00013-x