28
views
0
recommends
+1 Recommend
0 collections
    0
    shares
      • Record: found
      • Abstract: not found
      • Article: not found

      Controls on the composition and lability of dissolved organic matter in Siberia's Kolyma River basin : DOM COMPOSITION AND LABILITY IN KOLYMA RIVER BASIN

      Read this article at

      ScienceOpenPublisher
      Bookmark
          There is no author summary for this article yet. Authors can add summaries to their articles on ScienceOpen to make them more accessible to a non-specialist audience.

          Related collections

          Most cited references71

          • Record: found
          • Abstract: not found
          • Article: not found

          Visualization of an Oxygen-deficient Bottom Water Circulation in Osaka Bay, Japan

            Bookmark
            • Record: found
            • Abstract: found
            • Article: not found

            Evaluation of specific ultraviolet absorbance as an indicator of the chemical composition and reactivity of dissolved organic carbon.

            Specific UV absorbance (SUVA) is defined as the UV absorbance of a water sample at a given wavelength normalized for dissolved organic carbon (DOC) concentration. Our data indicate that SUVA, determined at 254 nm, is strongly correlated with percent aromaticity as determined by 13C NMR for 13 organic matter isolates obtained from a variety of aquatic environments. SUVA, therefore, is shown to be a useful parameter for estimating the dissolved aromatic carbon content in aquatic systems. Experiments involving the reactivity of DOC with chlorine and tetramethylammonium hydroxide (TMAH), however, show a wide range of reactivity for samples with similar SUVA values. These results indicate that, while SUVA measurements are good predictors of general chemical characteristics of DOC, they do not provide information about reactivity of DOC derived from different types of source materials. Sample pH, nitrate, and iron were found to influence SUVA measurements.
              Bookmark
              • Record: found
              • Abstract: found
              • Article: not found

              Increasing river discharge to the Arctic Ocean.

              Synthesis of river-monitoring data reveals that the average annual discharge of fresh water from the six largest Eurasian rivers to the Arctic Ocean increased by 7% from 1936 to 1999. The average annual rate of increase was 2.0 +/- 0.7 cubic kilometers per year. Consequently, average annual discharge from the six rivers is now about 128 cubic kilometers per year greater than it was when routine measurements of discharge began. Discharge was correlated with changes in both the North Atlantic Oscillation and global mean surface air temperature. The observed large-scale change in freshwater flux has potentially important implications for ocean circulation and climate.
                Bookmark

                Author and article information

                Journal
                Journal of Geophysical Research: Biogeosciences
                J. Geophys. Res.
                American Geophysical Union (AGU)
                01480227
                March 2012
                March 2012
                : 117
                : G1
                Article
                10.1029/2011JG001798
                a175bd2b-b5cc-46a7-bda0-9350eead5910
                © 2012

                http://doi.wiley.com/10.1002/tdm_license_1

                History

                Comments

                Comment on this article