Arctic epishelf lakes as sentinel ecosystems: Past, present and future

Ice shelves are a prominent but diminishing feature of the northern coastline of Ellesmere Island in the Canadian High Arctic (latitude 82-83°N). By blocking embayments and fiords, this thick coastal ice can create epishelf lakes, which are characterized by a perennially ice-capped water column of f...

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Published in:Journal of Geophysical Research: Biogeosciences
Main Authors: Veillette, J. (Julie), Mueller, D. (Derek), Antoniades, D. (Dermot), Vincent, W.F. (Warwick F.)
Format: Article in Journal/Newspaper
Language:English
Published: 2008
Subjects:
Online Access:https://ir.library.carleton.ca/pub/25919
https://doi.org/10.1029/2008JG000730
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spelling ftcarletonunivir:oai:carleton.ca:25919 2023-05-15T14:47:06+02:00 Arctic epishelf lakes as sentinel ecosystems: Past, present and future Veillette, J. (Julie) Mueller, D. (Derek) Antoniades, D. (Dermot) Vincent, W.F. (Warwick F.) 2008-12-28 https://ir.library.carleton.ca/pub/25919 https://doi.org/10.1029/2008JG000730 en eng https://ir.library.carleton.ca/pub/25919 doi:10.1029/2008JG000730 Journal of Geophysical Research B: Solid Earth vol. 113 no. 4 info:eu-repo/semantics/article 2008 ftcarletonunivir https://doi.org/10.1029/2008JG000730 2022-02-06T21:51:19Z Ice shelves are a prominent but diminishing feature of the northern coastline of Ellesmere Island in the Canadian High Arctic (latitude 82-83°N). By blocking embayments and fiords, this thick coastal ice can create epishelf lakes, which are characterized by a perennially ice-capped water column of freshwater overlying seawater. The goal of this study was to synthesize new, archived, and published data on Arctic epishelf lakes in the context of climate change. Long-term changes along this coastline were evaluated using historical reports, cartographic analysis, RADARSAT imagery, and field measurements. These data, including salinity-temperature profiling records from Disraeli Fiord spanning 54 years, show the rapid decline and near disappearance of this lake type in the Arctic. Salinity-temperature profiling of Milne Fiord, currently blocked by the Milne Ice Shelf, confirmed that it contained an epishelf lake composed of a 16-m thick freshwater layer overlying seawater. A profiling survey along the coast showed that there was a continuum of ice-dammed lakes from shallow systems dammed by multiyear landfast sea ice to deep epishelf lakes behind ice shelves. The climate warming recently observed in this region likely contributed to the decline of epishelf lakes over the last century, and the air temperature trend predicted for the Arctic over the next several decades implies the imminent loss of this ecosystem type. Our results underscore the distinctive properties of coastal ice-dammed lakes and their value as sentinel ecosystems for the monitoring of regional and global climate change. Copyright 2008 by the American Geophysical Union. Article in Journal/Newspaper Arctic Climate change Ellesmere Island Ice Shelf Ice Shelves Milne Fiord Milne Ice Shelf Sea ice Carleton University's Institutional Repository Arctic Disraeli Fiord ENVELOPE(-73.344,-73.344,82.819,82.819) Ellesmere Island Milne Fiord ENVELOPE(-81.447,-81.447,82.636,82.636) Milne Ice Shelf ENVELOPE(-81.747,-81.747,82.736,82.736) Journal of Geophysical Research: Biogeosciences 113 G4
institution Open Polar
collection Carleton University's Institutional Repository
op_collection_id ftcarletonunivir
language English
description Ice shelves are a prominent but diminishing feature of the northern coastline of Ellesmere Island in the Canadian High Arctic (latitude 82-83°N). By blocking embayments and fiords, this thick coastal ice can create epishelf lakes, which are characterized by a perennially ice-capped water column of freshwater overlying seawater. The goal of this study was to synthesize new, archived, and published data on Arctic epishelf lakes in the context of climate change. Long-term changes along this coastline were evaluated using historical reports, cartographic analysis, RADARSAT imagery, and field measurements. These data, including salinity-temperature profiling records from Disraeli Fiord spanning 54 years, show the rapid decline and near disappearance of this lake type in the Arctic. Salinity-temperature profiling of Milne Fiord, currently blocked by the Milne Ice Shelf, confirmed that it contained an epishelf lake composed of a 16-m thick freshwater layer overlying seawater. A profiling survey along the coast showed that there was a continuum of ice-dammed lakes from shallow systems dammed by multiyear landfast sea ice to deep epishelf lakes behind ice shelves. The climate warming recently observed in this region likely contributed to the decline of epishelf lakes over the last century, and the air temperature trend predicted for the Arctic over the next several decades implies the imminent loss of this ecosystem type. Our results underscore the distinctive properties of coastal ice-dammed lakes and their value as sentinel ecosystems for the monitoring of regional and global climate change. Copyright 2008 by the American Geophysical Union.
format Article in Journal/Newspaper
author Veillette, J. (Julie)
Mueller, D. (Derek)
Antoniades, D. (Dermot)
Vincent, W.F. (Warwick F.)
spellingShingle Veillette, J. (Julie)
Mueller, D. (Derek)
Antoniades, D. (Dermot)
Vincent, W.F. (Warwick F.)
Arctic epishelf lakes as sentinel ecosystems: Past, present and future
author_facet Veillette, J. (Julie)
Mueller, D. (Derek)
Antoniades, D. (Dermot)
Vincent, W.F. (Warwick F.)
author_sort Veillette, J. (Julie)
title Arctic epishelf lakes as sentinel ecosystems: Past, present and future
title_short Arctic epishelf lakes as sentinel ecosystems: Past, present and future
title_full Arctic epishelf lakes as sentinel ecosystems: Past, present and future
title_fullStr Arctic epishelf lakes as sentinel ecosystems: Past, present and future
title_full_unstemmed Arctic epishelf lakes as sentinel ecosystems: Past, present and future
title_sort arctic epishelf lakes as sentinel ecosystems: past, present and future
publishDate 2008
url https://ir.library.carleton.ca/pub/25919
https://doi.org/10.1029/2008JG000730
long_lat ENVELOPE(-73.344,-73.344,82.819,82.819)
ENVELOPE(-81.447,-81.447,82.636,82.636)
ENVELOPE(-81.747,-81.747,82.736,82.736)
geographic Arctic
Disraeli Fiord
Ellesmere Island
Milne Fiord
Milne Ice Shelf
geographic_facet Arctic
Disraeli Fiord
Ellesmere Island
Milne Fiord
Milne Ice Shelf
genre Arctic
Climate change
Ellesmere Island
Ice Shelf
Ice Shelves
Milne Fiord
Milne Ice Shelf
Sea ice
genre_facet Arctic
Climate change
Ellesmere Island
Ice Shelf
Ice Shelves
Milne Fiord
Milne Ice Shelf
Sea ice
op_source Journal of Geophysical Research B: Solid Earth vol. 113 no. 4
op_relation https://ir.library.carleton.ca/pub/25919
doi:10.1029/2008JG000730
op_doi https://doi.org/10.1029/2008JG000730
container_title Journal of Geophysical Research: Biogeosciences
container_volume 113
container_issue G4
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