Physical properties and isotopic characteristics of landfast sea ice around the North Water (NOW) Polynya region

An ice core sampling program was conducted during the North Water (NOW) Pol ynya Project 1998 Experiment in northern Baffin Bay during April-May 1998. The physical properties of snow and sea ice as well as the microstructure a nd stable isotopic composition of first-year landfast sea ice near the poly nya were investigated. The thickness of sea ice at the sampling sites range d between 147 and 194 cm with thinner snow cover during the period between mid-April and late May. The ice was characterized as typical first-year lan dfast sea ice, being composed of a thin granular ice layer at the top and a n underlying columnar ice layer towards the bottom of the ice. The samples obtained at a site closer to the ice edge of the polynya contained a thin g ranular ice layer originating from frazil ice near the ice bottom. Formatio n of frazil ice was considered to be caused by turbulent processes induced by winds, waves and currents forced from the polynya and also mixing with w ater masses produced at the polynya.