Ice draft and current measurements from the north-western Barents Sea, 1993–96 Einar Povl Abrahamsen, Svein Østerhus & Tor Gammelsrød From 1993 to 1996, three oceanographic moorings were deployed in the north-western Barents Sea, each with a current meter and an upward- looking sonar for measuring ice drafts. These yielded three years of cur- rents and two years of ice draft measurements. An interannual variability of almost 1 m was measured in the average ice draft. Causes for this variability are explored, particularly its possible connection to changes in atmospheric circulation patterns. We found that the fl ow of Northern Barents Atlantic-derived Water and the transport of ice from the Central Arctic into the Barents Sea appears to be controlled by winds between Nordaustlandet and Franz Josef Land, which in turn may be infl uenced by larger-scale variations such as the Arctic Oscillation/North Atlantic Oscillation. E. P. Abrahamsen, British Antarctic Survey, Natural Environment Research Council, High Cross, Mading- ley Road, Cambridge CB3 0ET, UK,
[email protected]; S. Østerhus, Bjerknes Centre for Climate Research, University of Bergen, Allégaten 55, NO-5007 Bergen, Norway; T. Gammelsrød, Geophysical Institute, Uni- versity of Bergen, Allégaten 70, NO-5007 Bergen, Norway. The Barents Sea plays an important role in the emerge from satellite altimetry observations climate system of the Arctic (Schauer et al. 1997; (Laxon et al. 2003). Maslowski et al. 2004, for example). About half Here we present two years of ice draft obser- of the heat loss to the atmosphere in the entire vations obtained from a mooring at 77° 55' N 28° Nordic seas takes place here (Simonsen & Haugan 20' E equipped with upward looking sonar (ULS).