Exploration of an ice-cliff grounding zone in Antarctica reveals frozen-on meltwater and high productivity

Ice fluxes across the grounding zone affect global ice-sheet mass loss and sea level rise. Although recent changes in ice fluxes are well constrained by remote sensing, future projections remain uncertain, because key environments affecting ice-sheet dynamics – the ice-sheet bed and grounding zone –...

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Published in:Communications Earth & Environment
Main Authors: Owsianowski, Nils, Richter, Claudio, Alfred-Wegener-Institut Helmholtz Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany, Universität Bremen, Bremen, Germany
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group UK 2021
Subjects:
Online Access:https://doi.org/10.1038/s43247-021-00166-y
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/11350
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spelling ftsubggeo:oai:e-docs.geo-leo.de:11858/11350 2024-02-11T09:55:03+01:00 Exploration of an ice-cliff grounding zone in Antarctica reveals frozen-on meltwater and high productivity Owsianowski, Nils Richter, Claudio Alfred-Wegener-Institut Helmholtz Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany Universität Bremen, Bremen, Germany 2021-05-25 https://doi.org/10.1038/s43247-021-00166-y http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/11350 eng eng Nature Publishing Group UK doi:10.1038/s43247-021-00166-y http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/11350 https://creativecommons.org/licenses/by/4.0/ ddc:577.7 Cryospheric science Environmental impact Marine biology Physical oceanography doc-type:article 2021 ftsubggeo https://doi.org/10.1038/s43247-021-00166-y 2024-01-21T23:12:30Z Ice fluxes across the grounding zone affect global ice-sheet mass loss and sea level rise. Although recent changes in ice fluxes are well constrained by remote sensing, future projections remain uncertain, because key environments affecting ice-sheet dynamics – the ice-sheet bed and grounding zone – are largely unknown. Here, we used a remotely operated vehicle to explore the grounding zone of a Weddell Sea tidewater ice cliff. At 148 m we found a 0.3–0.5 m gap between the ice and the seafloor and a 0.4 m clear facies of debris- and bubble-free basal ice, suggesting freeze-on of meltwater in the distal marine portion of the ice sheet over the last 400 yr. Ploughmarks and low epifauna cover reveal recent grounding line retreat, as corroborated by satellite remote sensing. We found dense algal tufts on the ice cliff and high phytoplankton pigment concentrations, suggesting high productivity fuelled by nutrients from ice melt. As grounded tidewater ice cliffs rim 38% of the Antarctic continent, sinking and downwelling of organic matter along with low benthic turnover may contribute to enhanced carbon sequestration, providing a potentially important feedback to climate. Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research (Alfred-Wegener- Institute, Helmholtz Centre for Polar and Marine Research) https://doi.org/10.13039/501100003207 https://doi.org/10.1594/PANGAEA.909526 https://doi.org/10.1594/PANGAEA.924822 Article in Journal/Newspaper Alfred Wegener Institute Antarc* Antarctic Antarctica Ice Sheet Weddell Sea GEO-LEOe-docs (FID GEO) Antarctic The Antarctic Weddell Sea Weddell Communications Earth & Environment 2 1
institution Open Polar
collection GEO-LEOe-docs (FID GEO)
op_collection_id ftsubggeo
language English
topic ddc:577.7
Cryospheric science
Environmental impact
Marine biology
Physical oceanography
spellingShingle ddc:577.7
Cryospheric science
Environmental impact
Marine biology
Physical oceanography
Owsianowski, Nils
Richter, Claudio
Alfred-Wegener-Institut Helmholtz Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
Universität Bremen, Bremen, Germany
Exploration of an ice-cliff grounding zone in Antarctica reveals frozen-on meltwater and high productivity
topic_facet ddc:577.7
Cryospheric science
Environmental impact
Marine biology
Physical oceanography
description Ice fluxes across the grounding zone affect global ice-sheet mass loss and sea level rise. Although recent changes in ice fluxes are well constrained by remote sensing, future projections remain uncertain, because key environments affecting ice-sheet dynamics – the ice-sheet bed and grounding zone – are largely unknown. Here, we used a remotely operated vehicle to explore the grounding zone of a Weddell Sea tidewater ice cliff. At 148 m we found a 0.3–0.5 m gap between the ice and the seafloor and a 0.4 m clear facies of debris- and bubble-free basal ice, suggesting freeze-on of meltwater in the distal marine portion of the ice sheet over the last 400 yr. Ploughmarks and low epifauna cover reveal recent grounding line retreat, as corroborated by satellite remote sensing. We found dense algal tufts on the ice cliff and high phytoplankton pigment concentrations, suggesting high productivity fuelled by nutrients from ice melt. As grounded tidewater ice cliffs rim 38% of the Antarctic continent, sinking and downwelling of organic matter along with low benthic turnover may contribute to enhanced carbon sequestration, providing a potentially important feedback to climate. Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research (Alfred-Wegener- Institute, Helmholtz Centre for Polar and Marine Research) https://doi.org/10.13039/501100003207 https://doi.org/10.1594/PANGAEA.909526 https://doi.org/10.1594/PANGAEA.924822
format Article in Journal/Newspaper
author Owsianowski, Nils
Richter, Claudio
Alfred-Wegener-Institut Helmholtz Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
Universität Bremen, Bremen, Germany
author_facet Owsianowski, Nils
Richter, Claudio
Alfred-Wegener-Institut Helmholtz Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
Universität Bremen, Bremen, Germany
author_sort Owsianowski, Nils
title Exploration of an ice-cliff grounding zone in Antarctica reveals frozen-on meltwater and high productivity
title_short Exploration of an ice-cliff grounding zone in Antarctica reveals frozen-on meltwater and high productivity
title_full Exploration of an ice-cliff grounding zone in Antarctica reveals frozen-on meltwater and high productivity
title_fullStr Exploration of an ice-cliff grounding zone in Antarctica reveals frozen-on meltwater and high productivity
title_full_unstemmed Exploration of an ice-cliff grounding zone in Antarctica reveals frozen-on meltwater and high productivity
title_sort exploration of an ice-cliff grounding zone in antarctica reveals frozen-on meltwater and high productivity
publisher Nature Publishing Group UK
publishDate 2021
url https://doi.org/10.1038/s43247-021-00166-y
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/11350
geographic Antarctic
The Antarctic
Weddell Sea
Weddell
geographic_facet Antarctic
The Antarctic
Weddell Sea
Weddell
genre Alfred Wegener Institute
Antarc*
Antarctic
Antarctica
Ice Sheet
Weddell Sea
genre_facet Alfred Wegener Institute
Antarc*
Antarctic
Antarctica
Ice Sheet
Weddell Sea
op_relation doi:10.1038/s43247-021-00166-y
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/11350
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1038/s43247-021-00166-y
container_title Communications Earth & Environment
container_volume 2
container_issue 1
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