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 4.3 m 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 o...

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Published in:Scientific Drilling
Main Authors: Patterson, Molly O., Levy, Richard H., Kulhanek, Denise K., 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., Läufer, Andreas, Yoo, Kyu-Cheul, Seki, Osamu, Stocchi, Paolo, Klages, Johann P., Lee, Jae Il, Colleoni, Florence, Suganuma, Yusuke, Gasson, Edward, Ohneiser, Christian, Flores, José-Abel, Try, David, Kirkman, Rachel, Koch, Daleen, the SWAIS 2C Science Team
Format: Text
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.5194/sd-30-101-2022
https://sd.copernicus.org/articles/30/101/2022/
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spelling ftcopernicus:oai:publications.copernicus.org:sd97668 2023-05-15T14:02:17+02:00 Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C) Patterson, Molly O. Levy, Richard H. Kulhanek, Denise K. 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. Läufer, Andreas Yoo, Kyu-Cheul Seki, Osamu Stocchi, Paolo Klages, Johann P. Lee, Jae Il Colleoni, Florence Suganuma, Yusuke Gasson, Edward Ohneiser, Christian Flores, José-Abel Try, David Kirkman, Rachel Koch, Daleen the SWAIS 2C Science Team 2022-02-24 application/pdf https://doi.org/10.5194/sd-30-101-2022 https://sd.copernicus.org/articles/30/101/2022/ eng eng doi:10.5194/sd-30-101-2022 https://sd.copernicus.org/articles/30/101/2022/ eISSN: 1816-3459 Text 2022 ftcopernicus https://doi.org/10.5194/sd-30-101-2022 2022-02-28T17:22:14Z The West Antarctic Ice Sheet (WAIS) presently holds enough ice to raise global sea level by 4.3 m 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 planet-wide signals of human-induced climate change. The Sensitivity of the West Antarctic Ice Sheet to a Warming of 2 ∘ 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 ∘ 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 200 m 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 sensitivity to past and future increases in global mean surface temperature up to 2 ∘ C above pre-industrial levels. Thus, the scientific and technological advances developed through this program will enable us to test whether WAIS collapsed during past intervals of warmth and determine its sensitivity to a + 2 ∘ C global warming threshold (UNFCCC, 2015). Text Antarc* Antarctic Ice Sheet Ice Shelf Kamb Ice Stream Copernicus Publications: E-Journals 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
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The West Antarctic Ice Sheet (WAIS) presently holds enough ice to raise global sea level by 4.3 m 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 planet-wide signals of human-induced climate change. The Sensitivity of the West Antarctic Ice Sheet to a Warming of 2 ∘ 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 ∘ 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 200 m 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 sensitivity to past and future increases in global mean surface temperature up to 2 ∘ C above pre-industrial levels. Thus, the scientific and technological advances developed through this program will enable us to test whether WAIS collapsed during past intervals of warmth and determine its sensitivity to a + 2 ∘ C global warming threshold (UNFCCC, 2015).
format Text
author Patterson, Molly O.
Levy, Richard H.
Kulhanek, Denise K.
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.
Läufer, Andreas
Yoo, Kyu-Cheul
Seki, Osamu
Stocchi, Paolo
Klages, Johann P.
Lee, Jae Il
Colleoni, Florence
Suganuma, Yusuke
Gasson, Edward
Ohneiser, Christian
Flores, José-Abel
Try, David
Kirkman, Rachel
Koch, Daleen
the SWAIS 2C Science Team
spellingShingle Patterson, Molly O.
Levy, Richard H.
Kulhanek, Denise K.
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.
Läufer, Andreas
Yoo, Kyu-Cheul
Seki, Osamu
Stocchi, Paolo
Klages, Johann P.
Lee, Jae Il
Colleoni, Florence
Suganuma, Yusuke
Gasson, Edward
Ohneiser, Christian
Flores, José-Abel
Try, David
Kirkman, Rachel
Koch, Daleen
the SWAIS 2C Science Team
Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C)
author_facet Patterson, Molly O.
Levy, Richard H.
Kulhanek, Denise K.
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.
Läufer, Andreas
Yoo, Kyu-Cheul
Seki, Osamu
Stocchi, Paolo
Klages, Johann P.
Lee, Jae Il
Colleoni, Florence
Suganuma, Yusuke
Gasson, Edward
Ohneiser, Christian
Flores, José-Abel
Try, David
Kirkman, Rachel
Koch, Daleen
the SWAIS 2C Science Team
author_sort Patterson, Molly O.
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://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_source eISSN: 1816-3459
op_relation doi:10.5194/sd-30-101-2022
https://sd.copernicus.org/articles/30/101/2022/
op_doi https://doi.org/10.5194/sd-30-101-2022
container_title Scientific Drilling
container_volume 30
container_start_page 101
op_container_end_page 112
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