Zobrazeno 1 - 10
of 57
pro vyhledávání: '"Peter K. Bijl"'
Autor:
Xuyuan E. Ai, Lena M. Thöle, Alexandra Auderset, Mareike Schmitt, Simone Moretti, Anja S. Studer, Elisabeth Michel, Martin Wegmann, Alain Mazaud, Peter K. Bijl, Daniel M. Sigman, Alfredo Martínez-García, Samuel L. Jaccard
Publikováno v:
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-12 (2024)
Abstract Previous studies suggest that meridional migrations of the Antarctic Circumpolar Current may have altered wind-driven upwelling and carbon dioxide degassing in the Southern Ocean during past climate transitions. Here, we report a quantitativ
Externí odkaz:
https://doaj.org/article/49301435a23546558db055422a37108f
Autor:
Suning Hou, Lennert B. Stap, Ryan Paul, Mei Nelissen, Frida S. Hoem, Martin Ziegler, Appy Sluijs, Francesca Sangiorgi, Peter K. Bijl
Publikováno v:
Nature Communications, Vol 14, Iss 1, Pp 1-12 (2023)
Abstract Gradual climate cooling and CO2 decline in the Miocene were recently shown not to be associated with major ice volume expansion, challenging a fundamental paradigm in the functioning of the Antarctic cryosphere. Here, we explore Miocene ice-
Externí odkaz:
https://doaj.org/article/abbdbee3d1a44b63a7b2af7f933d831c
Autor:
Frida S. Hoem, Isabel Sauermilch, Adam K. Aleksinski, Matthew Huber, Francien Peterse, Francesca Sangiorgi, Peter K. Bijl
Publikováno v:
Communications Earth & Environment, Vol 3, Iss 1, Pp 1-8 (2022)
The deepening of the Drake Passage cooled Antarctic coasts and increased the temperature gradient between Australia and Antarctica which ultimately enhanced thermal isolation of the Antarctic Ice sheet, according to biomarker derived temperature reco
Externí odkaz:
https://doaj.org/article/7f7b3caab22243d38a1bccf008cdb3e2
Autor:
Isabel Sauermilch, Joanne M. Whittaker, Andreas Klocker, David R. Munday, Katharina Hochmuth, Peter K. Bijl, Joseph H. LaCasce
Publikováno v:
Nature Communications, Vol 12, Iss 1, Pp 1-8 (2021)
The role of Southern Ocean gateways contributing to the Eocene-Oligocene climate transition is still debated. Here, the authors present high-resolution ocean simulations to show that gateways opening led to a reorganization of ocean circulation, heat
Externí odkaz:
https://doaj.org/article/3b7c0e4a2a9848b28a92e690b0bddeac
Autor:
Peter D. Nooteboom, Philippe Delandmeter, Erik van Sebille, Peter K. Bijl, Henk A. Dijkstra, Anna S. von der Heydt, Vanesa Magar
Publikováno v:
PLoS ONE, Vol 15, Iss 9 (2020)
Any type of non-buoyant material in the ocean is transported horizontally by currents during its sinking journey. This lateral transport can be far from negligible for small sinking velocities. To estimate its magnitude and direction, the material is
Externí odkaz:
https://doaj.org/article/8da2a1876cb646a9b449c7742d47d2b9
Autor:
Francesca Sangiorgi, Peter K. Bijl, Sandra Passchier, Ulrich Salzmann, Stefan Schouten, Robert McKay, Rosemary D. Cody, Jörg Pross, Tina van de Flierdt, Steven M. Bohaty, Richard Levy, Trevor Williams, Carlota Escutia, Henk Brinkhuis
Publikováno v:
Nature Communications, Vol 9, Iss 1, Pp 1-11 (2018)
Ocean heat is important in forcing ice sheet retreat, yet past ocean temperature data from proximal ice sheet locations are sparse. Here, the authors present temperature reconstructions from the Wilkes Land subglacial basin during the mid-Miocene, an
Externí odkaz:
https://doaj.org/article/5d1d8a15101a4010af35615aec6ac5b9
Autor:
Suning Hou, Foteini Lamprou, Frida S. Hoem, Mohammad Rizky Nanda Hadju, Francesca Sangiorgi, Francien Peterse, Peter K. Bijl
Publikováno v:
Climate of the Past. 19:787-802
The Neogene (23.04–2.58 Ma) is characterised by progressive buildup of ice volume and climate cooling in the Antarctic and the Northern Hemisphere. Heat and moisture delivery to Antarctica is, to a large extent, regulated by the strength of meridio
While many palaeoclimate studies have focussed on the Eocene-Oligocene transition (EOT), little is known about the timing and drivers of the post-EOT climate recovery. To better understand and reconstruct terrestrial climate and vegetation dynamics f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::29c8b90e34771f1e12c46850f4ba4d92
https://dspace.library.uu.nl/handle/1874/428881
https://dspace.library.uu.nl/handle/1874/428881
Autor:
Frida S. Hoem, Adrián López-Quirós, Suzanna van de Lagemaat, Johan Etourneau, Marie-Alexandrine Sicre, Carlota Escutia, Henk Brinkhuis, Francien Peterse, Francesca Sangiorgi, Peter K. Bijl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aede5df198a08a18a15845281d441fa3
https://doi.org/10.5194/egusphere-2023-291-supplement
https://doi.org/10.5194/egusphere-2023-291-supplement
Autor:
Frida S. Hoem, Adrián López-Quirós, Suzanna van de Lagemaat, Johan Etourneau, Marie-Alexandrine Sicre, Carlota Escutia, Henk Brinkhuis, Francien Peterse, Francesca Sangiorgi, Peter K. Bijl
Publikováno v:
eISSN
At present, a strong latitudinal sea surface temperature (SST) gradient of ~16 °C exists across the Southern Ocean, maintained by the Antarctic Circumpolar Current (ACC) and a set of complex frontal systems. Together with the Antarctic ice masses, t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::158959bf20062a179314768053c66c7f
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-291/
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-291/