Over the next century, near‐surface permafrost across the circumpolar Arctic is expected to
degrade significantly, particularly for land areas south of 70° N. This is likely to cause …

This chapter reviews and synthesizes the current state of knowledge on sources,
transformations, cycling, and fluxes of dissolved organic carbon (DOC) in river-estuarine and …

Carbon in thawing permafrost soils may have global impacts on climate change; however,
the factors that control its processing and fate are poorly understood. The dominant fate of …

A major surface circulation feature of the Arctic Ocean is the Transpolar Drift (TPD), a current
that transports river‐influenced shelf water from the Laptev and East Siberian Seas toward …

A one‐year study was carried out to investigate the seasonal fluxes and source variation of
organic carbon transported by two major Chinese rivers, the Yellow River and Changjiang …

As high latitudes warm, a portion of the large organic carbon pool stored in permafrost will
become available for transport to aquatic ecosystems as dissolved organic carbon (DOC). If …

High‐latitude northern rivers export globally significant quantities of dissolved organic
carbon (DOC) to the Arctic Ocean. Climate change, and its associated impacts on hydrology …

In sunlit waters, photochemical alteration of dissolved organic carbon (DOC) impacts the
microbial respiration of DOC to CO2. This coupled photochemical and biological …

The biomarker composition of dissolved organic carbon (DOC) of the six largest Arctic rivers
was studied between 2003 and 2007 as part of the PARTNERS Project. Samples were …

A comprehensive data set of dissolved organic carbon (DOC) and colored dissolved organic
matter (CDOM) absorption measurements is analysed in light of tracing the supply and …