SeaicevelocityintheFramStraitmonitoredbymooredinstruments Correction published 11 December 2003

Polar Water (PW) ,Greenland Sea Arctic Surface Water (GS-ASW), East Greenland Shelf Bottom Water (EGS-BW), Re- circulating Atlantic Water (RAW), upper Greenland Sea Arctic

We then transitioned into the hydrographic phase of the cruise and occupied a set of high-resolution CTD/velocity/water- sample transects across the East Greenland shelf and

Mean monthly volume transport (Sv) through the strait between Novaya Zemlya and Frans ]osef Land calculated from the mean current velocity observed by the

The temperature distribution indicates little transport of water from the East Greenland Current to the Jan Mayen current and the East Iceland current.. It was

Horizontal drift velocity measured for Wisting C weathered water-free residues and emulsions as a function of current in the flume for three different ice conditions: smooth

Figure 8: Current roses for the 4 vector velocity meters inside the cage, giving the statistical distribution (appearance) of the current direction and the mean velocity for

We present an approach for modelling the complete marginal distribution (bulk and tail distribution) of each residual current component, describe the application of the

While focusing more on the water velocity and dissolved oxygen profile (when possible) along the diametrical plane through the tank ’ s centre, this report also describes water