Title Surface freshening in the Arctic Ocean's Eurasian Basin; an apparent consequence of recent change in the wind- driven circulation
Author Timmermans, M.L.; Proshutinsky, A.; Krishfield, R.A.; Perovich, D.K.; Richter- Menge, J.A.; Station, T.P.; Toole, J.M.
Author Affil Timmermans, M.L., Yale University, Department of Geology and Geophysics, New Haven, CT. Other: Woods Hole Oceanographic Institution; U. S. Army Cold Regions Research and Engineering Laboratory; Naval Postgraduate School
Source Journal of Geophysical Research, 116(C), Citation C00D03. Publisher: American Geophysical Union, Washington, DC, United States. ISSN: 0148-0227. CRREL Report No: ERDC/CRREL MP-11-7493
Publication Date 2011
Notes In English. Part of special section on Arctic Ocean investigation employing AOMIP-2 models, edited by Proshutinsky, A., NSF grants ARC-0519899, ARC-0856479 and ARC- 0806306. 50 refs. GeoRef Acc. No: 309836
Index Terms atmospheric circulation; ice; ice cover; ice cover thickness; meltwater; ocean currents; salinity; snow; storms; temperature; Arctic Ocean--Eurasia Basin; anticyclones; Arctic Ocean; currents; Eurasia Basin; fresh water; ice cover distribution; ocean circulation; sea ice; sea surface water; sea water; thermohaline circulation; winds
Abstract Data collected by an autonomous ice- based observatory that drifted into the Eurasian Basin between April and November 2010 indicate that the upper ocean was appreciably fresher than in 2007 and 2008. Sea ice and snowmelt over the course of the 2010 drift amounted to an input of less than 0.5 m of liquid freshwater to the ocean (comparable to the freshening by melting estimated for those previous years), while the observed change in upper-ocean salinity over the melt period implies a freshwater gain of about 0.7 m. Results of a wind-driven ocean model corroborate the observations of freshening and suggest that unusually fresh surface waters observed in parts of the Eurasian Basin in 2010 may have been due to the spreading of anomalously fresh water previously residing in the Beaufort Gyre. This flux is likely associated with a 2009 shift in the large-scale atmospheric circulation to a significant reduction in strength of the anticyclonic Beaufort Gyre and the Transpolar Drift Stream.
URL http://hdl.handle.net/10.1029/2011JC006975
Publication Type journal article
Record ID 65006483