Coralline Algae Archive Fjord Surface Water Temperatures in Southwest Greenland

Abstract One of the most dramatic signs of ongoing global change is the mass loss of the Greenland Ice Sheet and the resulting rise in sea level, whereby most of the recent ice sheet mass loss can be attributed to an increase in meltwater runoff. The retreat and thinning of Greenland glaciers has be...

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Published in:Journal of Geophysical Research: Biogeosciences
Main Authors: Williams, Siobhan, Halfar, Jochen, Zack, Thomas, Hetzinger, Steffen, Blicher, Martin, Juul‐Pedersen, Thomas, Kronz, Andreas, Noël, Brice, van den Broeke, Michiel, van de Berg, Willem Jan
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:https://resolver.sub.uni-goettingen.de/purl?gro-2/133775
https://doi.org/10.1029/2018JG004385
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spelling ftsubgoettingen:oai:publications.goettingen-research-online.de:2/133775 2023-11-05T03:42:08+01:00 Coralline Algae Archive Fjord Surface Water Temperatures in Southwest Greenland Williams, Siobhan Halfar, Jochen Zack, Thomas Hetzinger, Steffen Blicher, Martin Juul‐Pedersen, Thomas Kronz, Andreas Noël, Brice van den Broeke, Michiel van de Berg, Willem Jan Williams, Siobhan Halfar, Jochen Zack, Thomas Hetzinger, Steffen Blicher, Martin Juul‐Pedersen, Thomas Kronz, Andreas Noël, Brice van den Broeke, Michiel van de Berg, Willem Jan 2018 https://resolver.sub.uni-goettingen.de/purl?gro-2/133775 https://doi.org/10.1029/2018JG004385 en eng https://resolver.sub.uni-goettingen.de/purl?gro-2/133775 doi:10.1029/2018JG004385 info:eu-repo/semantics/openAccess http://onlinelibrary.wiley.com/termsAndConditions#vor info:eu-repo/semantics/article journal_article yes 2018 ftsubgoettingen https://doi.org/10.1029/2018JG004385 2023-10-08T16:57:58Z Abstract One of the most dramatic signs of ongoing global change is the mass loss of the Greenland Ice Sheet and the resulting rise in sea level, whereby most of the recent ice sheet mass loss can be attributed to an increase in meltwater runoff. The retreat and thinning of Greenland glaciers has been caused by rising air and ocean temperatures over the past decades. Despite the global scale impact of the changing ice sheet balance, estimates of glacial runoff in Greenland rarely extend past several decades, thus limiting our understanding of long‐term glacial response to temperature. Here we present a 42‐year long annually resolved red coralline algal Mg/Ca proxy temperature record from a southwestern Greenland fjord, with temperature ranging from 1.5 to 4 °C (standard error = 1.06 °C). This temperature time series in turn tracks the general trend of glacial runoff from four West Greenland glaciers discharging freshwater into the fjord (all p < 0.001). The algal time series further exhibits significant correlations to Irminger Sea temperature patterns, which are transmitted to western Greenland fjords via the West Greenland Current. The 42‐year long record demonstrates the potential of annual increment forming coralline algae, which are known to live up to 650 years and which are abundant along the Greenland coastline, for reconstructing time series of sea surface temperature. Key Points Coralline algal Mg/Ca ratios have a strong correlation with regional SST Coralline algae enable reconstruction of a 42‐year temperature time series Funder: Geological Society of America https://doi.org/10.13039/100005720 Funder: Natural Sciences and Engineering Research Council of Canada https://doi.org/10.13039/501100000038 Funder: Geological Society of America https://doi.org/10.13039/100005720 Article in Journal/Newspaper glacier* Greenland Ice Sheet Georg-August-Universität Göttingen: GoeScholar Journal of Geophysical Research: Biogeosciences 123 8 2617 2626
institution Open Polar
collection Georg-August-Universität Göttingen: GoeScholar
op_collection_id ftsubgoettingen
language English
description Abstract One of the most dramatic signs of ongoing global change is the mass loss of the Greenland Ice Sheet and the resulting rise in sea level, whereby most of the recent ice sheet mass loss can be attributed to an increase in meltwater runoff. The retreat and thinning of Greenland glaciers has been caused by rising air and ocean temperatures over the past decades. Despite the global scale impact of the changing ice sheet balance, estimates of glacial runoff in Greenland rarely extend past several decades, thus limiting our understanding of long‐term glacial response to temperature. Here we present a 42‐year long annually resolved red coralline algal Mg/Ca proxy temperature record from a southwestern Greenland fjord, with temperature ranging from 1.5 to 4 °C (standard error = 1.06 °C). This temperature time series in turn tracks the general trend of glacial runoff from four West Greenland glaciers discharging freshwater into the fjord (all p < 0.001). The algal time series further exhibits significant correlations to Irminger Sea temperature patterns, which are transmitted to western Greenland fjords via the West Greenland Current. The 42‐year long record demonstrates the potential of annual increment forming coralline algae, which are known to live up to 650 years and which are abundant along the Greenland coastline, for reconstructing time series of sea surface temperature. Key Points Coralline algal Mg/Ca ratios have a strong correlation with regional SST Coralline algae enable reconstruction of a 42‐year temperature time series Funder: Geological Society of America https://doi.org/10.13039/100005720 Funder: Natural Sciences and Engineering Research Council of Canada https://doi.org/10.13039/501100000038 Funder: Geological Society of America https://doi.org/10.13039/100005720
author2 Williams, Siobhan
Halfar, Jochen
Zack, Thomas
Hetzinger, Steffen
Blicher, Martin
Juul‐Pedersen, Thomas
Kronz, Andreas
Noël, Brice
van den Broeke, Michiel
van de Berg, Willem Jan
format Article in Journal/Newspaper
author Williams, Siobhan
Halfar, Jochen
Zack, Thomas
Hetzinger, Steffen
Blicher, Martin
Juul‐Pedersen, Thomas
Kronz, Andreas
Noël, Brice
van den Broeke, Michiel
van de Berg, Willem Jan
spellingShingle Williams, Siobhan
Halfar, Jochen
Zack, Thomas
Hetzinger, Steffen
Blicher, Martin
Juul‐Pedersen, Thomas
Kronz, Andreas
Noël, Brice
van den Broeke, Michiel
van de Berg, Willem Jan
Coralline Algae Archive Fjord Surface Water Temperatures in Southwest Greenland
author_facet Williams, Siobhan
Halfar, Jochen
Zack, Thomas
Hetzinger, Steffen
Blicher, Martin
Juul‐Pedersen, Thomas
Kronz, Andreas
Noël, Brice
van den Broeke, Michiel
van de Berg, Willem Jan
author_sort Williams, Siobhan
title Coralline Algae Archive Fjord Surface Water Temperatures in Southwest Greenland
title_short Coralline Algae Archive Fjord Surface Water Temperatures in Southwest Greenland
title_full Coralline Algae Archive Fjord Surface Water Temperatures in Southwest Greenland
title_fullStr Coralline Algae Archive Fjord Surface Water Temperatures in Southwest Greenland
title_full_unstemmed Coralline Algae Archive Fjord Surface Water Temperatures in Southwest Greenland
title_sort coralline algae archive fjord surface water temperatures in southwest greenland
publishDate 2018
url https://resolver.sub.uni-goettingen.de/purl?gro-2/133775
https://doi.org/10.1029/2018JG004385
genre glacier*
Greenland
Ice Sheet
genre_facet glacier*
Greenland
Ice Sheet
op_relation https://resolver.sub.uni-goettingen.de/purl?gro-2/133775
doi:10.1029/2018JG004385
op_rights info:eu-repo/semantics/openAccess
http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1029/2018JG004385
container_title Journal of Geophysical Research: Biogeosciences
container_volume 123
container_issue 8
container_start_page 2617
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