Differences in the Quantity and Quality of Organic Matter Exported From Greenlandic Glacial and Deglaciated Watersheds

• Main Authors: Pain, Andrea J., Martin, Jonathan B., Martin, Ellen E., Rahman, Shaily, Ackermann, Philip
• Format: Text
• Language: unknown
• Published: The Aquila Digital Community 2020
• Subjects: Arctic; discharge; Greenland; organic carbon; periglacial; watersheds; Oceanography and Atmospheric Sciences and Meteorology; Physical Sciences and Mathematics; Arctic Ocean; greenlandic; Ice; Ice Sheet; permafrost
• Online Access: https://aquila.usm.edu/fac_pubs/18212; https://doi-org.lynx.lib.usm.edu/10.1029/2020GB006614

©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.