The cryoconite ecosystem on the Greenland ice sheet

This paper presents an assessment of biological activity associated with ice surface debris (cryoconite) at the ice-sheet scale. Estimates of the mass distribution of cryoconite over the Greenland ice sheet (GIS) and the biological activity associated with it are presented and then coupled with a su...

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Published in:Annals of Glaciology
Main Authors: Hodson, Andy, Bøggild, Carl, Hanna, Edward, Huybrechts, Phillipe, Langford, Harry, Cameron, Karen, Houldsworth, Alexandra
Format: Article in Journal/Newspaper
Language:unknown
Published: International Glaciological Society 2010
Subjects:
Online Access:http://eprints.gla.ac.uk/215732/
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spelling ftuglasgow:oai:eprints.gla.ac.uk:215732 2023-05-15T13:29:43+02:00 The cryoconite ecosystem on the Greenland ice sheet Hodson, Andy Bøggild, Carl Hanna, Edward Huybrechts, Phillipe Langford, Harry Cameron, Karen Houldsworth, Alexandra 2010 http://eprints.gla.ac.uk/215732/ unknown International Glaciological Society Hodson, A., Bøggild, C., Hanna, E., Huybrechts, P., Langford, H., Cameron, K. <http://eprints.gla.ac.uk/view/author/55427.html> and Houldsworth, A. (2010) The cryoconite ecosystem on the Greenland ice sheet. Annals of Glaciology <http://eprints.gla.ac.uk/view/journal_volume/Annals_of_Glaciology.html>, 51(56), pp. 123-129. (doi:10.3189/172756411795931985 <http://dx.doi.org/10.3189/172756411795931985>) Articles PeerReviewed 2010 ftuglasgow https://doi.org/10.3189/172756411795931985 2021-10-21T22:10:17Z This paper presents an assessment of biological activity associated with ice surface debris (cryoconite) at the ice-sheet scale. Estimates of the mass distribution of cryoconite over the Greenland ice sheet (GIS) and the biological activity associated with it are presented and then coupled with a surface mass-balance model to estimate total carbon fluxes due to respiration and photosynthesis. We find an average loading of 66gm−2 at Kangerlussuaq, southwest Greenland, which compares well with recent estimates from Kronprins Christians Land (17–440 gm−2: Bøggild and others, 2010) in northeast Greenland. We also report a significant microbial biomass in cryoconite at both these places (103–104 cells mg−1) and carbon fluxes of the order of 1–3 μM C g−1d−1 for both respiration and photosynthesis. The modelling indicates that total respiration and photosynthesis fluxes are likely to be ∼101–102 GgCa−1 and thus far from trivial. However, estimation of the net ecosystem impact across the entire ice sheet on atmospheric CO2 concentrations is problematic because photosynthesis rates were almost certainly low during our field campaign. Therefore, like its water balance, the carbon balance of the GIS is now known to be important, but its accurate quantification will remain elusive until more data are forthcoming. Article in Journal/Newspaper Annals of Glaciology Greenland Ice Sheet Kangerlussuaq University of Glasgow: Enlighten - Publications Greenland Kangerlussuaq ENVELOPE(-55.633,-55.633,72.633,72.633) Annals of Glaciology 51 56 123 129
institution Open Polar
collection University of Glasgow: Enlighten - Publications
op_collection_id ftuglasgow
language unknown
description This paper presents an assessment of biological activity associated with ice surface debris (cryoconite) at the ice-sheet scale. Estimates of the mass distribution of cryoconite over the Greenland ice sheet (GIS) and the biological activity associated with it are presented and then coupled with a surface mass-balance model to estimate total carbon fluxes due to respiration and photosynthesis. We find an average loading of 66gm−2 at Kangerlussuaq, southwest Greenland, which compares well with recent estimates from Kronprins Christians Land (17–440 gm−2: Bøggild and others, 2010) in northeast Greenland. We also report a significant microbial biomass in cryoconite at both these places (103–104 cells mg−1) and carbon fluxes of the order of 1–3 μM C g−1d−1 for both respiration and photosynthesis. The modelling indicates that total respiration and photosynthesis fluxes are likely to be ∼101–102 GgCa−1 and thus far from trivial. However, estimation of the net ecosystem impact across the entire ice sheet on atmospheric CO2 concentrations is problematic because photosynthesis rates were almost certainly low during our field campaign. Therefore, like its water balance, the carbon balance of the GIS is now known to be important, but its accurate quantification will remain elusive until more data are forthcoming.
format Article in Journal/Newspaper
author Hodson, Andy
Bøggild, Carl
Hanna, Edward
Huybrechts, Phillipe
Langford, Harry
Cameron, Karen
Houldsworth, Alexandra
spellingShingle Hodson, Andy
Bøggild, Carl
Hanna, Edward
Huybrechts, Phillipe
Langford, Harry
Cameron, Karen
Houldsworth, Alexandra
The cryoconite ecosystem on the Greenland ice sheet
author_facet Hodson, Andy
Bøggild, Carl
Hanna, Edward
Huybrechts, Phillipe
Langford, Harry
Cameron, Karen
Houldsworth, Alexandra
author_sort Hodson, Andy
title The cryoconite ecosystem on the Greenland ice sheet
title_short The cryoconite ecosystem on the Greenland ice sheet
title_full The cryoconite ecosystem on the Greenland ice sheet
title_fullStr The cryoconite ecosystem on the Greenland ice sheet
title_full_unstemmed The cryoconite ecosystem on the Greenland ice sheet
title_sort cryoconite ecosystem on the greenland ice sheet
publisher International Glaciological Society
publishDate 2010
url http://eprints.gla.ac.uk/215732/
long_lat ENVELOPE(-55.633,-55.633,72.633,72.633)
geographic Greenland
Kangerlussuaq
geographic_facet Greenland
Kangerlussuaq
genre Annals of Glaciology
Greenland
Ice Sheet
Kangerlussuaq
genre_facet Annals of Glaciology
Greenland
Ice Sheet
Kangerlussuaq
op_relation Hodson, A., Bøggild, C., Hanna, E., Huybrechts, P., Langford, H., Cameron, K. <http://eprints.gla.ac.uk/view/author/55427.html> and Houldsworth, A. (2010) The cryoconite ecosystem on the Greenland ice sheet. Annals of Glaciology <http://eprints.gla.ac.uk/view/journal_volume/Annals_of_Glaciology.html>, 51(56), pp. 123-129. (doi:10.3189/172756411795931985 <http://dx.doi.org/10.3189/172756411795931985>)
op_doi https://doi.org/10.3189/172756411795931985
container_title Annals of Glaciology
container_volume 51
container_issue 56
container_start_page 123
op_container_end_page 129
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