Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C)

The West Antarctic Ice Sheet (WAIS) presently holds enough ice to raise global sea level by 4.3m if completely melted. The unknown response of the WAIS to future warming remains a significant challenge for numerical models in quantifying predictions of future sea level rise. Sea level rise is one of...

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Published in:Scientific Drilling
Main Authors: Molly O. Patterson, Richard H. Levy, Denise K. Kulhanek, Tina van de Flierdt, Huw Horgan, Gavin B. Dunbar, Timothy R. Naish, Jeanine Ash, Alex Pyne, Darcy Mandeno, Paul Winberry, David M. Harwood, Fabio Florindo, Francisco J. Jimenez-Espejo, Andreas Laufer, Kyu-Cheul Yoo, Osamu Seki, Paolo Stocchi, Johann P. Klages, Jae Il Lee, Florence Colleoni, Yusuke Suganuma, Edward Gasson, Christian Ohneiser, Jose-Abel Flores, David Try, Rachel Kirkman, Daleen Koch, the SWAIS 2C Science Team
Other Authors: Patterson, Molly O., Levy, Richard H., Kulhanek, Denise K., van de Flierdt, Tina, Horgan, Huw, Dunbar, Gavin B., Naish, Timothy R., Ash, Jeanine, Pyne, Alex, Mandeno, Darcy, Winberry, Paul, Harwood, David M., Florindo, Fabio, Jimenez-Espejo, Francisco J., Laufer, Andrea, Yoo, Kyu-Cheul, Seki, Osamu, Stocchi, Paolo, Klages, Johann P., Il Lee, Jae, Colleoni, Florence, Suganuma, Yusuke, Gasson, Edward, Ohneiser, Christian, Flores, Jose-Abel, Try, David, Kirkman, Rachel, Koch, Daleen, Sandroni, Sonia
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:https://hdl.handle.net/11365/1239727
https://doi.org/10.5194/sd-30-101-2022
https://sd.copernicus.org/articles/30/101/2022/
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description The West Antarctic Ice Sheet (WAIS) presently holds enough ice to raise global sea level by 4.3m if completely melted. The unknown response of the WAIS to future warming remains a significant challenge for numerical models in quantifying predictions of future sea level rise. Sea level rise is one of the clearest planetwide signals of human-induced climate change. The Sensitivity of the West Antarctic Ice Sheet to a Warming of 2 degrees C (SWAIS 2C) Project aims to understand past and current drivers and thresholds of WAIS dynamics to improve projections of the rate and size of ice sheet changes under a range of elevated greenhouse gas levels in the atmosphere as well as the associated average global temperature scenarios to and beyond the +2 degrees C target of the Paris Climate Agreement.Despite efforts through previous land and ship-based drilling on and along the Antarctic margin, unequivocal evidence of major WAIS retreat or collapse and its causes has remained elusive. To evaluate and plan for the interdisciplinary scientific opportunities and engineering challenges that an International Continental Drilling Program (ICDP) project along the Siple coast near the grounding zone of the WAIS could offer (Fig. 1), researchers, engineers, and logistics providers representing 10 countries held a virtual workshop in October 2020. This international partnership comprised of geologists, glaciologists, oceanographers, geophysicists, microbiologists, climate and ice sheet modelers, and engineers outlined specific research objectives and logistical challenges associated with the recovery of Neogene and Quaternary geological records from the West Antarctic interior adjacent to the Kamb Ice Stream and at Crary Ice Rise. New geophysical surveys at these locations have identified drilling targets in which new drilling technologies will allow for the recovery of up to 200m of sediments beneath the ice sheet. Sub-ice-shelf records have so far proven difficult to obtain but are critical to better constrain marine ice sheet ...
author2 Patterson, Molly O.
Levy, Richard H.
Kulhanek, Denise K.
van de Flierdt, Tina
Horgan, Huw
Dunbar, Gavin B.
Naish, Timothy R.
Ash, Jeanine
Pyne, Alex
Mandeno, Darcy
Winberry, Paul
Harwood, David M.
Florindo, Fabio
Jimenez-Espejo, Francisco J.
Laufer, Andrea
Yoo, Kyu-Cheul
Seki, Osamu
Stocchi, Paolo
Klages, Johann P.
Il Lee, Jae
Colleoni, Florence
Suganuma, Yusuke
Gasson, Edward
Ohneiser, Christian
Flores, Jose-Abel
Try, David
Kirkman, Rachel
Koch, Daleen
Sandroni, Sonia
format Article in Journal/Newspaper
author Molly O. Patterson
Richard H. Levy
Denise K. Kulhanek
Tina van de Flierdt
Huw Horgan
Gavin B. Dunbar
Timothy R. Naish
Jeanine Ash
Alex Pyne
Darcy Mandeno
Paul Winberry
David M. Harwood
Fabio Florindo
Francisco J. Jimenez-Espejo
Andreas Laufer
Kyu-Cheul Yoo
Osamu Seki
Paolo Stocchi
Johann P. Klages
Jae Il Lee
Florence Colleoni
Yusuke Suganuma
Edward Gasson
Christian Ohneiser
Jose-Abel Flores
David Try
Rachel Kirkman
Daleen Koch
the SWAIS 2C Science Team
spellingShingle Molly O. Patterson
Richard H. Levy
Denise K. Kulhanek
Tina van de Flierdt
Huw Horgan
Gavin B. Dunbar
Timothy R. Naish
Jeanine Ash
Alex Pyne
Darcy Mandeno
Paul Winberry
David M. Harwood
Fabio Florindo
Francisco J. Jimenez-Espejo
Andreas Laufer
Kyu-Cheul Yoo
Osamu Seki
Paolo Stocchi
Johann P. Klages
Jae Il Lee
Florence Colleoni
Yusuke Suganuma
Edward Gasson
Christian Ohneiser
Jose-Abel Flores
David Try
Rachel Kirkman
Daleen Koch
the SWAIS 2C Science Team
Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C)
author_facet Molly O. Patterson
Richard H. Levy
Denise K. Kulhanek
Tina van de Flierdt
Huw Horgan
Gavin B. Dunbar
Timothy R. Naish
Jeanine Ash
Alex Pyne
Darcy Mandeno
Paul Winberry
David M. Harwood
Fabio Florindo
Francisco J. Jimenez-Espejo
Andreas Laufer
Kyu-Cheul Yoo
Osamu Seki
Paolo Stocchi
Johann P. Klages
Jae Il Lee
Florence Colleoni
Yusuke Suganuma
Edward Gasson
Christian Ohneiser
Jose-Abel Flores
David Try
Rachel Kirkman
Daleen Koch
the SWAIS 2C Science Team
author_sort Molly O. Patterson
title Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C)
title_short Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C)
title_full Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C)
title_fullStr Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C)
title_full_unstemmed Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C)
title_sort sensitivity of the west antarctic ice sheet to +2 °c (swais 2c)
publishDate 2022
url https://hdl.handle.net/11365/1239727
https://doi.org/10.5194/sd-30-101-2022
https://sd.copernicus.org/articles/30/101/2022/
long_lat ENVELOPE(-172.500,-172.500,-82.933,-82.933)
ENVELOPE(-145.000,-145.000,-82.250,-82.250)
ENVELOPE(-83.917,-83.917,-75.917,-75.917)
ENVELOPE(-155.000,-155.000,-82.000,-82.000)
geographic Antarctic
Crary Ice Rise
Kamb Ice Stream
Siple
Siple Coast
The Antarctic
West Antarctic Ice Sheet
geographic_facet Antarctic
Crary Ice Rise
Kamb Ice Stream
Siple
Siple Coast
The Antarctic
West Antarctic Ice Sheet
genre Antarc*
Antarctic
Ice Sheet
Ice Shelf
Kamb Ice Stream
genre_facet Antarc*
Antarctic
Ice Sheet
Ice Shelf
Kamb Ice Stream
op_relation info:eu-repo/semantics/altIdentifier/wos/WOS:000763332900001
volume:30
firstpage:101
lastpage:112
numberofpages:12
journal:SCIENTIFIC DRILLING
https://hdl.handle.net/11365/1239727
doi:10.5194/sd-30-101-2022
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85126043751
https://sd.copernicus.org/articles/30/101/2022/
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container_title Scientific Drilling
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spelling ftunivsiena:oai:usiena-air.unisi.it:11365/1239727 2024-04-14T08:01:42+00:00 Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C) Molly O. Patterson Richard H. Levy Denise K. Kulhanek Tina van de Flierdt Huw Horgan Gavin B. Dunbar Timothy R. Naish Jeanine Ash Alex Pyne Darcy Mandeno Paul Winberry David M. Harwood Fabio Florindo Francisco J. Jimenez-Espejo Andreas Laufer Kyu-Cheul Yoo Osamu Seki Paolo Stocchi Johann P. Klages Jae Il Lee Florence Colleoni Yusuke Suganuma Edward Gasson Christian Ohneiser Jose-Abel Flores David Try Rachel Kirkman Daleen Koch the SWAIS 2C Science Team Patterson, Molly O. Levy, Richard H. Kulhanek, Denise K. van de Flierdt, Tina Horgan, Huw Dunbar, Gavin B. Naish, Timothy R. Ash, Jeanine Pyne, Alex Mandeno, Darcy Winberry, Paul Harwood, David M. Florindo, Fabio Jimenez-Espejo, Francisco J. Laufer, Andrea Yoo, Kyu-Cheul Seki, Osamu Stocchi, Paolo Klages, Johann P. Il Lee, Jae Colleoni, Florence Suganuma, Yusuke Gasson, Edward Ohneiser, Christian Flores, Jose-Abel Try, David Kirkman, Rachel Koch, Daleen Sandroni, Sonia 2022 STAMPA https://hdl.handle.net/11365/1239727 https://doi.org/10.5194/sd-30-101-2022 https://sd.copernicus.org/articles/30/101/2022/ eng eng info:eu-repo/semantics/altIdentifier/wos/WOS:000763332900001 volume:30 firstpage:101 lastpage:112 numberofpages:12 journal:SCIENTIFIC DRILLING https://hdl.handle.net/11365/1239727 doi:10.5194/sd-30-101-2022 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85126043751 https://sd.copernicus.org/articles/30/101/2022/ info:eu-repo/semantics/openAccess info:eu-repo/semantics/article 2022 ftunivsiena https://doi.org/10.5194/sd-30-101-2022 2024-03-21T15:51:40Z The West Antarctic Ice Sheet (WAIS) presently holds enough ice to raise global sea level by 4.3m if completely melted. The unknown response of the WAIS to future warming remains a significant challenge for numerical models in quantifying predictions of future sea level rise. Sea level rise is one of the clearest planetwide signals of human-induced climate change. The Sensitivity of the West Antarctic Ice Sheet to a Warming of 2 degrees C (SWAIS 2C) Project aims to understand past and current drivers and thresholds of WAIS dynamics to improve projections of the rate and size of ice sheet changes under a range of elevated greenhouse gas levels in the atmosphere as well as the associated average global temperature scenarios to and beyond the +2 degrees C target of the Paris Climate Agreement.Despite efforts through previous land and ship-based drilling on and along the Antarctic margin, unequivocal evidence of major WAIS retreat or collapse and its causes has remained elusive. To evaluate and plan for the interdisciplinary scientific opportunities and engineering challenges that an International Continental Drilling Program (ICDP) project along the Siple coast near the grounding zone of the WAIS could offer (Fig. 1), researchers, engineers, and logistics providers representing 10 countries held a virtual workshop in October 2020. This international partnership comprised of geologists, glaciologists, oceanographers, geophysicists, microbiologists, climate and ice sheet modelers, and engineers outlined specific research objectives and logistical challenges associated with the recovery of Neogene and Quaternary geological records from the West Antarctic interior adjacent to the Kamb Ice Stream and at Crary Ice Rise. New geophysical surveys at these locations have identified drilling targets in which new drilling technologies will allow for the recovery of up to 200m of sediments beneath the ice sheet. Sub-ice-shelf records have so far proven difficult to obtain but are critical to better constrain marine ice sheet ... Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Ice Shelf Kamb Ice Stream Università degli Studi di Siena: USiena air Antarctic Crary Ice Rise ENVELOPE(-172.500,-172.500,-82.933,-82.933) Kamb Ice Stream ENVELOPE(-145.000,-145.000,-82.250,-82.250) Siple ENVELOPE(-83.917,-83.917,-75.917,-75.917) Siple Coast ENVELOPE(-155.000,-155.000,-82.000,-82.000) The Antarctic West Antarctic Ice Sheet Scientific Drilling 30 101 112