Hydrology and Land Surface Studies
Utilizing chromophoric dissolved organic matter measurements to derive export and reactivity of dissolved organic carbon exported to the Arctic Ocean: A case study of the Yukon River, Alaska
Article first published online: 18 MAR 2009
DOI: 10.1029/2008GL036831
Copyright 2009 by the American Geophysical Union.
Additional Information
How to Cite
, , , , , and (2009), Utilizing chromophoric dissolved organic matter measurements to derive export and reactivity of dissolved organic carbon exported to the Arctic Ocean: A case study of the Yukon River, Alaska, Geophys. Res. Lett., 36, L06401, doi:10.1029/2008GL036831.
Publication History
- Issue published online: 18 MAR 2009
- Article first published online: 18 MAR 2009
- Manuscript Accepted: 28 JAN 2009
- Manuscript Revised: 21 JAN 2009
- Manuscript Received: 27 NOV 2008
Keywords:
- dissolved organic carbon;
- chromophoric dissolved organic matter;
- Arctic river
[1] The quality and quantity of dissolved organic matter (DOM) exported by Arctic rivers is known to vary with hydrology and this exported material plays a fundamental role in the biogeochemical cycling of carbon at high latitudes. We highlight the potential of optical measurements to examine DOM quality across the hydrograph in Arctic rivers. Furthermore, we establish chromophoric DOM (CDOM) relationships to dissolved organic carbon (DOC) and lignin phenols in the Yukon River and model DOC and lignin loads from CDOM measurements, the former in excellent agreement with long-term DOC monitoring data. Intensive sampling across the historically under-sampled spring flush period highlights the importance of this time for total export of DOC and particularly lignin. Calculated riverine DOC loads to the Arctic Ocean show an increase from previous estimates, especially when new higher discharge data are incorporated. Increased DOC loads indicate decreased residence times for terrigenous DOM in the Arctic Ocean with important implications for the reactivity and export of this material to the Atlantic Ocean.

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