The Transpolar Drift as a Source of Riverine and Shelf-Derived Trace Elements to the Central Arctic Ocean

• Main Authors: Charette, Matthew A., Kipp, Lauren E., Jensen, Laramie T., Dabrowski, Jessica S., Whitmore, Laura M., Fitzsimmons, Jessica N., Williford, Tatiana, Ulfsbo, Adam, Jones, Elizabeth, Bundy, Randelle M., Vivancos, Sebastian M., Pahnke, Katharina, John, Seth G., Xiang, Yang, Hatta, Mariko, Petrova, Mariia V., Heimbürger-Boavida, Lars Eric, Bauch, Dorothea, Newton, Robert, Pasqualini, Angelica, Agather, Alison M., Amon, Rainer M.W., Anderson, Robert F., Andersson, Per S., Benner, Ronald, Bowman, Katlin L., Edwards, R. Lawrence, Gdaniec, Sandra, Gerringa, Loes J.A., González, Aridane G., Granskog, Mats, Haley, Brian, Hammerschmidt, Chad R.
• Format: Text
• Language: unknown
• Published: The Aquila Digital Community 2020
• Subjects: Arctic Ocean; carbon; GEOTRACES]; nutrients; trace elements; Transpolar Drift; Oceanography and Atmospheric Sciences and Meteorology; Physical Sciences and Mathematics; Arctic; Central Basin; Fram Strait; Ice; laptev; North Atlantic; permafrost
• Online Access: https://aquila.usm.edu/fac_pubs/18268; https://doi-org.lynx.lib.usm.edu/10.1029/2019JC015920

©2020. American Geophysical Union. 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 the center of the basin and Fram Strait. In 2015, the international GEOTRACES...