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dc.contributor.authorCooper, Lee W.  Concept link
dc.contributor.authorBenner, Ronald  Concept link
dc.contributor.authorMcClelland, James W.  Concept link
dc.contributor.authorPeterson, Bruce J.  Concept link
dc.contributor.authorHolmes, Robert M.  Concept link
dc.contributor.authorRaymond, Peter A.  Concept link
dc.contributor.authorHansell, Dennis A.  Concept link
dc.contributor.authorGrebmeier, Jacqueline M.  Concept link
dc.contributor.authorCodispoti, Louis A.  Concept link
dc.date.accessioned2006-11-01T20:15:55Z
dc.date.available2006-11-01T20:15:55Z
dc.date.issued2005-12-07
dc.identifier.citationJournal of Geophysical Research 110 (2005): G02013
dc.identifier.urihttps://hdl.handle.net/1912/1288
dc.descriptionAuthor Posting. © American Geophysical Union, 2005. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 110 (2005): G02013, doi:10.1029/2005JG000031.en
dc.description.abstractConcentrations of dissolved organic carbon (DOC) and δ18O values have been determined following sampling of runoff from a number of major arctic rivers, including the Ob, Yenisey, Lena, Kolyma, Mackenzie and Yukon in 2003-2004. These data are considered in conjunction with marine data for DOC, δ18O values, nutrients, salinity, and fluorometric indicators of DOC that were obtained as part of the Shelf-Basin Interactions program at the continental shelf-basin boundary of the Chukchi and Beaufort Seas. These marine data indicate that the freshwater component is most likely derived from regional sources, such as the Mackenzie, the Bering Strait inflow and possibly eastern Siberian rivers, including the Kolyma, or the Lena but not rivers further west in the Eurasian arctic. Contributions of freshwater from melted sea ice to marine surface waters appeared to be insignificant over annual cycles compared to runoff, although on a seasonal basis, freshwater from melted sea ice was locally dominant following a major sea-ice retreat into the Canada Basin in 2002. DOC concentrations were correlated with the runoff fraction, with an apparent meteoric water DOC concentration of 174 ± 1 μM (standard error). This concentration is lower than the flow-weighted concentrations measured at river mouths of the five largest Arctic rivers (358 to 917 μM), indicating that removal of terrigenous DOC during transport through estuaries, shelves and in the deep basin. DOC data indicate that flow-weighted concentrations in the two largest North American arctic rivers, the Yukon (625μM) and the Mackenzie (382 μM), are lower than in the three largest Eurasian arctic rivers, the Ob (825 μM), the Yenesey (858 μM) and the Lena (917 μM). A fluorometric indicator of chromophoric dissolved organic matter (CDOM) that has provided estimates of terrigenous DOC concentrations in the Eurasian Arctic was not correlated with DOC concentrations in the Amerasian marine waters studied, except below the upper Arctic Ocean halocline. Nutrient distributions and concentrations as well as derived nutrient ratios suggest the CDOM fluorometer may be responding to the release of chromophoric materials from continental shelf sediments. Shipboard incubation experiments with undisturbed sediment cores indicate that continental shelf sediments on the Bering and Chukchi Sea shelves are likely to be a net source of DOC to the Arctic Ocean.en
dc.description.sponsorshipThe PARTNERS and SBI projects have been supported by the Office of Polar Programs of the U.S. National Science Foundation.en
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen
dc.publisherAmerican Geophysical Union
dc.relation.urihttps://doi.org/10.1029/2005JG000031
dc.titleLinkages among runoff, dissolved organic carbon, and the stable oxygen isotope composition of seawater and other water mass indicators in the Arctic Oceanen
dc.typeArticleen
dc.identifier.doi10.1029/2005JG000031


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