Rapid formation of a sea ice barrier east of Svalbard

• Published in: Journal of Geophysical Research. C. Oceans 2005-11, Vol.110 (C11), p.C11013.1-n/a
• Main Authors: Nghiem, S. V., Van Woert, M. L., Neumann, G.
• Format: Article
• Language: English
• Subjects: Barents Sea; Barriers; bathymetry; Channels; Earth sciences; Earth, ocean, space; Elongation; Exact sciences and technology; Historic; Marine; Scatterometers; Sea ice; Surface water
• ISSN: 0148-0227; 2169-9275; 2156-2202; 2169-9291
• DOI: 10.1029/2004JC002654

Daily SeaWinds scatterometer images acquired by the QuikSCAT satellite show an elongated sea ice feature that formed very rapidly (∼1–2 days) in November 2001 east of Svalbard over the Barents Sea. This sea ice structure, called “the Svalbard sea ice barrier,” spanning approximately 10° in longitude and 2° in latitude, restricts the sea route and poses a significant navigation hazard. The secret of its formation appears to lie in the bottom of the sea: A comparison between bathymetry from the International Bathymetric Chart of the Arctic Ocean data and the pattern of sea ice formation from scatterometer data reveals that the sea ice barrier conforms well with and stretches above a deep elongated channel connecting the Franz Josef–Victoria Trough to the Hinlopen Basin between Svalbard and Franz Josef Land. Historic hydrographic data from this area indicate that this sea channel contains cold Arctic water less than 50 m below the surface. Strong and persistent cold northerly winds force strong heat loss from this shallow surface layer, leading to the rapid formation of the sea ice barrier. Heat transfer rates estimated from European Centre for Medium‐Range Weather Forecasts temperature and wind data over this region suggest that the surface water along the deep channel can be rapidly cooled to the freezing point. Scatterometer results in 1999–2003 show that sea ice forms in this area between October and December. Understanding the ice formation mechanisms helps to select appropriate locations for deployment of buoys measuring wind and air‐sea temperature profile and to facilitate ice monitoring, modeling, and forecasting.