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JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 106, NO. C6, PAGES 11,469–11,480, 2001

Wind-driven transport pathways for Eurasian Arctic river discharge

Christopher K. H. Guay

College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon


Kelly Kenison Falkner

College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon


Robin D. Muench

Earth and Space Research, Seattle, Washington


Manfred Mensch

Institut für Umweltphysik, Ruprecht-Karls-Universität, Heidelberg, Germany


Markus Frank

Institut für Umweltphysik, Ruprecht-Karls-Universität, Heidelberg, Germany


Reinhold Bayer

Institut für Umweltphysik, Ruprecht-Karls-Universität, Heidelberg, Germany


Abstract

Distributions of temperature, salinity, and barium in near-surface waters (depth ≤ 50 m) of the Laptev Sea and adjacent areas of the Arctic Ocean are presented for the summers of 1993, 1995, and 1996. The tracer data indicate that while fluvial discharge was largely confined to the shelf region of the Laptev Sea in the summer of 1993, surface waters containing a significant fluvial component extended beyond the shelf break and over the slope and basin areas north of the Laptev Sea in the summers of 1995 and 1996. These distributions of fluvial discharge are consistent with local winds and suggest two principal pathways by which river waters can enter the central Arctic basins from the Laptev Sea. When southerly to southeasterly wind conditions prevail, river waters are transported northward beyond the shelf break and over the slope and adjacent basin areas. These waters can then enter the interior Arctic Ocean via upper layer flow in the vicinity of the Lomonosov Ridge. Under other wind conditions, river waters are steered primarily along the inner Laptev shelf and into the East Siberian Sea as part of the predominantly eastward coastal current system. These waters then appear to cross the shelf and enter the interior Arctic Ocean via upper layer flow aligned roughly along the Mendeleyev Ridge. The extent to which either pathway is favored in a given year is largely determined by local wind patterns during the summer months, when fluvial discharge is greatest and shelf waters are at the lowest salinity of their annual cycle.

Received 26 January 2000; accepted 12 February 2001.

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Citation: Guay, C. K. H., K. K. Falkner, R. D. Muench, M. Mensch, M. Frank, and R. Bayer (2001), Wind-driven transport pathways for Eurasian Arctic river discharge, J. Geophys. Res., 106(C6), 11,469–11,480.