Differences in the Quantity and Quality of Organic Matter Exported From Greenlandic Glacial and Deglaciated Watersheds
©2020. American Geophysical Union. All Rights Reserved. Riverine input of terrestrial dissolved organic matter (DOM) is an important component of the marine carbon cycle and drives net carbon dioxide production in coastal zones. DOM exports to the Arctic Ocean are likely to increase due to melting o...
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ftsouthmissispun:oai:aquila.usm.edu:fac_pubs-19526 2023-07-30T04:01:21+02:00 Differences in the Quantity and Quality of Organic Matter Exported From Greenlandic Glacial and Deglaciated Watersheds Pain, Andrea J. Martin, Jonathan B. Martin, Ellen E. Rahman, Shaily Ackermann, Philip 2020-10-01T07:00:00Z https://aquila.usm.edu/fac_pubs/18212 https://doi-org.lynx.lib.usm.edu/10.1029/2020GB006614 unknown The Aquila Digital Community https://aquila.usm.edu/fac_pubs/18212 https://doi-org.lynx.lib.usm.edu/10.1029/2020GB006614 Faculty Publications Arctic discharge Greenland organic carbon periglacial watersheds Oceanography and Atmospheric Sciences and Meteorology Physical Sciences and Mathematics text 2020 ftsouthmissispun 2023-07-15T18:54:37Z ©2020. American Geophysical Union. All Rights Reserved. Riverine input of terrestrial dissolved organic matter (DOM) is an important component of the marine carbon cycle and drives net carbon dioxide production in coastal zones. DOM exports to the Arctic Ocean are likely to increase due to melting of permafrost and the Greenland Ice Sheet, but the quantity and quality of DOM exports from deglaciated watersheds in Greenland, as well as expected changes with future melting, are unknown. We compare DOM quantity and quality in Greenland over the melt seasons of 2017–2018 between two rivers directly draining the Greenland Ice Sheet (meltwater rivers) and four streams draining deglaciated catchments that are disconnected from the ice (nonglacial streams). We couple these data with discharge records to compare dissolved organic carbon (DOC) exports. DOM sources and quality differ significantly between watershed types: fluorescence characteristics and organic molar C:N ratios suggest that DOM from deglaciated watersheds is derived from terrestrial vegetation and soil organic matter, while that in glacial watersheds contains greater proportions of algal and/or freshly produced biomass and may be more reactive. DOC specific yield is similar for nonglacial streams (0.1–1.2 Mg/km2/year) compared to a glacial meltwater river (0.2–1.1 Mg/km2/year), despite orders of magnitude differences in instantaneous discharge. Upscaling based on land cover leads to an estimate of total DOC contributions from Greenland between 0.2 and 0.5 Tg/year, much of which is derived from deglaciated watersheds. These results suggest that future warming and ice retreat may increase DOC fluxes from Greenland with consequences for the Arctic carbon cycle. Text Arctic Arctic Ocean Greenland greenlandic Ice Ice Sheet permafrost The University of Southern Mississippi: The Aquila Digital Community Arctic Arctic Ocean Greenland |
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Open Polar |
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The University of Southern Mississippi: The Aquila Digital Community |
op_collection_id |
ftsouthmissispun |
language |
unknown |
topic |
Arctic discharge Greenland organic carbon periglacial watersheds Oceanography and Atmospheric Sciences and Meteorology Physical Sciences and Mathematics |
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Arctic discharge Greenland organic carbon periglacial watersheds Oceanography and Atmospheric Sciences and Meteorology Physical Sciences and Mathematics Pain, Andrea J. Martin, Jonathan B. Martin, Ellen E. Rahman, Shaily Ackermann, Philip Differences in the Quantity and Quality of Organic Matter Exported From Greenlandic Glacial and Deglaciated Watersheds |
topic_facet |
Arctic discharge Greenland organic carbon periglacial watersheds Oceanography and Atmospheric Sciences and Meteorology Physical Sciences and Mathematics |
description |
©2020. American Geophysical Union. All Rights Reserved. Riverine input of terrestrial dissolved organic matter (DOM) is an important component of the marine carbon cycle and drives net carbon dioxide production in coastal zones. DOM exports to the Arctic Ocean are likely to increase due to melting of permafrost and the Greenland Ice Sheet, but the quantity and quality of DOM exports from deglaciated watersheds in Greenland, as well as expected changes with future melting, are unknown. We compare DOM quantity and quality in Greenland over the melt seasons of 2017–2018 between two rivers directly draining the Greenland Ice Sheet (meltwater rivers) and four streams draining deglaciated catchments that are disconnected from the ice (nonglacial streams). We couple these data with discharge records to compare dissolved organic carbon (DOC) exports. DOM sources and quality differ significantly between watershed types: fluorescence characteristics and organic molar C:N ratios suggest that DOM from deglaciated watersheds is derived from terrestrial vegetation and soil organic matter, while that in glacial watersheds contains greater proportions of algal and/or freshly produced biomass and may be more reactive. DOC specific yield is similar for nonglacial streams (0.1–1.2 Mg/km2/year) compared to a glacial meltwater river (0.2–1.1 Mg/km2/year), despite orders of magnitude differences in instantaneous discharge. Upscaling based on land cover leads to an estimate of total DOC contributions from Greenland between 0.2 and 0.5 Tg/year, much of which is derived from deglaciated watersheds. These results suggest that future warming and ice retreat may increase DOC fluxes from Greenland with consequences for the Arctic carbon cycle. |
format |
Text |
author |
Pain, Andrea J. Martin, Jonathan B. Martin, Ellen E. Rahman, Shaily Ackermann, Philip |
author_facet |
Pain, Andrea J. Martin, Jonathan B. Martin, Ellen E. Rahman, Shaily Ackermann, Philip |
author_sort |
Pain, Andrea J. |
title |
Differences in the Quantity and Quality of Organic Matter Exported From Greenlandic Glacial and Deglaciated Watersheds |
title_short |
Differences in the Quantity and Quality of Organic Matter Exported From Greenlandic Glacial and Deglaciated Watersheds |
title_full |
Differences in the Quantity and Quality of Organic Matter Exported From Greenlandic Glacial and Deglaciated Watersheds |
title_fullStr |
Differences in the Quantity and Quality of Organic Matter Exported From Greenlandic Glacial and Deglaciated Watersheds |
title_full_unstemmed |
Differences in the Quantity and Quality of Organic Matter Exported From Greenlandic Glacial and Deglaciated Watersheds |
title_sort |
differences in the quantity and quality of organic matter exported from greenlandic glacial and deglaciated watersheds |
publisher |
The Aquila Digital Community |
publishDate |
2020 |
url |
https://aquila.usm.edu/fac_pubs/18212 https://doi-org.lynx.lib.usm.edu/10.1029/2020GB006614 |
geographic |
Arctic Arctic Ocean Greenland |
geographic_facet |
Arctic Arctic Ocean Greenland |
genre |
Arctic Arctic Ocean Greenland greenlandic Ice Ice Sheet permafrost |
genre_facet |
Arctic Arctic Ocean Greenland greenlandic Ice Ice Sheet permafrost |
op_source |
Faculty Publications |
op_relation |
https://aquila.usm.edu/fac_pubs/18212 https://doi-org.lynx.lib.usm.edu/10.1029/2020GB006614 |
_version_ |
1772812094915215360 |