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: Stocchi, P., Offre, P., Spang, A.
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:https://www.vliz.be/imisdocs/publications/22/374522.pdf
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spelling ftnioz:oai:imis.nioz.nl:350712 2023-05-15T13:47:57+02:00 Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C) Stocchi, P. Offre, P. Spang, A. 2022 application/pdf https://www.vliz.be/imisdocs/publications/22/374522.pdf en eng info:eu-repo/semantics/altIdentifier/wos/000763332900001 info:eu-repo/semantics/altIdentifier/doi/doi.org/10.5194/sd-30-101-2022 https://www.vliz.be/imisdocs/publications/22/374522.pdf info:eu-repo/semantics/openAccess %3Ci%3ESci.+Drill.+30%3C%2Fi%3E%3A+101-112.+%3Ca+href%3D%22https%3A%2F%2Fdx.doi.org%2F10.5194%2Fsd-30-101-2022%22+target%3D%22_blank%22%3Ehttps%3A%2F%2Fdx.doi.org%2F10.5194%2Fsd-30-101-2022%3C%2Fa%3E info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2022 ftnioz https://doi.org/10.5194/sd-30-101-2022 2022-05-01T14:16:10Z 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). Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Ice Shelf Kamb Ice Stream NIOZ Repository (Royal Netherlands Institute for Sea Research) 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
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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 Article in Journal/Newspaper
author Stocchi, P.
Offre, P.
Spang, A.
spellingShingle Stocchi, P.
Offre, P.
Spang, A.
Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C)
author_facet Stocchi, P.
Offre, P.
Spang, A.
author_sort Stocchi, P.
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://www.vliz.be/imisdocs/publications/22/374522.pdf
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
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https://www.vliz.be/imisdocs/publications/22/374522.pdf
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