Interannual variations in river water content and distribution over the Laptev Sea between 2007 and 2011: The Arctic Dipole connection

Five years of oxygen isotope and hydrological surveys reveal interannual variations in the inventory and distribution of river water over the Laptev Sea. In 2007, 2009, and 2010 relatively low amounts of river water (≤1500 km3) were found and were mostly located in the southeastern Laptev Sea. In 20...

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Published inGeophysical research letters Vol. 41; no. 20; pp. 7237 - 7244
Main Authors Thibodeau, Benoit, Bauch, Dorothea, Kassens, Heidemarie, Timokhov, Leonid A.
Format Journal Article
LanguageEnglish
Published Washington Blackwell Publishing Ltd 28.10.2014
John Wiley & Sons, Inc
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Summary:Five years of oxygen isotope and hydrological surveys reveal interannual variations in the inventory and distribution of river water over the Laptev Sea. In 2007, 2009, and 2010 relatively low amounts of river water (≤1500 km3) were found and were mostly located in the southeastern Laptev Sea. In 2008 and 2011, high amounts of river water (~1600 km3 and ~2000 km3) were found, especially in the central and northern part of the shelf, suggesting a northward export of this water. This temporal pattern is coherent with the summer Arctic Dipole index that was higher in 2008 and 2011. Our results suggest that the Arctic Dipole might influence the export of river water from the Laptev Sea. Moreover, the river water inventory in the Laptev Sea seems related to the freshwater content of the Arctic Ocean with a 2 years lag. Key Points Link between Arctic Dipole anomaly and river water content in the Laptev SeaLaptev Sea river water might be linked to the Arctic‐wide freshwater contentThe Laptev Sea could contributes up to 20% of the Arctic‐wide freshening
Bibliography:ark:/67375/WNG-P1QBMLS8-4
ReadmeText S2 and Tables 3 and 4Figure S1Figure S5Figure S6Table S7
istex:251EC7B5345AFBFB99FB3849569ECA2B81B20C1A
ArticleID:GRL52162
ISSN:0094-8276
1944-8007
DOI:10.1002/2014GL061814