Export of Pacific carbon through the Arctic Archipelago to the North Atlantic

• Published in: Continental Shelf Research
• Main Authors: Shadwick, EH, Thomas, H, Gratton, Y, Leong, D, Moore, SA, Papakyriakou, T, Prowe, AEF
• Format: Article in Journal/Newspaper
• Language: English
• Published: Pergamon-Elsevier Science Ltd 2011
• Subjects: Earth Sciences; Oceanography; Chemical Oceanography; Arctic; Canadian Arctic Archipelago; Mackenzie River; Pacific; Arctic Archipelago; Mackenzie river; North Atlantic; Sea ice
• Online Access: https://doi.org/10.1016/j.csr.2011.01.014; http://ecite.utas.edu.au/75936

During an east-to-west transect through the Canadian Arctic Archipelago, dissolved inorganic carbon (DIC) and total alkalinity (TA) were measured. The watermass composition throughout the Archipelago is determined using TA and the seawater oxygen isotope fractionation (d18O) data, and the carboncharacteristics of these waters are examined. The influence of the Mackenzie River is primarily limited to the upper water column in the western Archipelago while the fraction of sea-ice melt water in the surface waters increases eastward with maximum values at the outflows of Jones and Lancaster Sounds.The depth of Pacific-origin upper halocline waters increases eastward through the Archipelago. In the western Archipelago, non-conservative variations in deep water DIC are used to compute a subsurface carbon surplus, which appears to be fueled by organic matter produced in the surface layer and bybenthic respiration. The eastward transport of carbon from the Pacific, via the Arctic Archipelago, to the North Atlantic is estimated, and the impact of increased export of sea-ice melt water to the North Atlantic is discussed.