4.7 Article

Variability in the meteoric water, sea-ice melt, and Pacific water contributions to the central Arctic Ocean, 2000-2014

期刊

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
卷 120, 期 3, 页码 1573-1598

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1002/2014JC010023

关键词

central Arctic Ocean; chemical tracers; interannual variability; meteoric water; sea ice melt; Pacific water

资金

  1. National Science Foundation [OPP-9910335, OPP-0352984]
  2. Office of Polar Programs (OPP)
  3. Directorate For Geosciences [1135072] Funding Source: National Science Foundation

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Fourteen years (2000-2014) of bottle chemistry data collected during the North Pole Environmental Observatory were compiled to examine variations in the composition of freshwater (meteoric water, net sea-ice meltwater, and Pacific water) over mixed layer of the Central Arctic Ocean. In addition to significant spatial and interannual variability, there was a general decrease in meteoric water (MW) fractions at the majority of stations reoccupied over the duration of the program that was approximately balanced by a concomitant increase in freshwater from sea-ice melt (SIM FW) between 2000 and 2012. Inventories (0-120 m) of MW and SIM FW computed using available data between 2005 and 2012 exhibited similar variations over the study area, allowing for first-order estimates of the mean annual changes in MW (-389194 km(3) yr(-1)) and SIM FW (29297 km(3) yr(-1)) for the Central Arctic region. These mean annual changes were attributed to the diversion of Siberian river runoff to the Beaufort Gyre and the overall reduction of sea ice volume across the Arctic, respectively. In addition to this lower-frequency variability, spatial gradients and interannual variations in MW, SIM FW, and Pacific water contributions to specific locations were attributed to shifts in the Transpolar Drift that advects waters of eastern and western Arctic origin through the study area.

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