PUBLICATIONS Journal of Geophysical Research: Oceans RESEARCH ARTICLE Invisible polynyas: Modulation of fast ice thickness by ocean 10.1002/2014JC010404 heat flux on the Canadian polar shelf Key Points: Humfrey Melling1, Christian Haas2, and Eric Brossier3 Fast-ice thickness varies with surface ocean temperature, as well as snow 1Institute of Ocean Sciences, Ocean Science Division, Fisheries and Oceans Canada, Sidney, British Columbia, Canada, depth 2Department of Earth and Space Science and Engineering, York University, Toronto, Ontario, Canada, 3Association Nord- Thickness anomalies are linked to tidal enhancement of ocean heat flux Est., Lanton, Hanvec, France Reductions up to 80 percent are undetectable by eye or infrared sensor Abstract Although the Canadian polar shelf is dominated by thick fast ice in winter, areas of young ice or open water do recur annually at locations within and adjacent to the fast ice. These polynyas are detectable by Correspondence to: eye and sustained by wind or tide-driven ice divergence and ocean heat flux. Our ice-thickness surveys by dril- H. Melling, ling and towed electromagnetic sounder reveal that visible polynyas comprise only a subset of thin-ice cover-
[email protected] age. Additional area in the coastal zone, in shallow channels and in fjords is covered by thin ice which is too thick to be discerned by eye. Our concurrent surveys by CTD reveal correlation between thin fast ice and above- Citation: Melling, H., C. Haas, and E. Brossier freezing seawater beneath it. We use winter time series of air and ocean temperatures and ice and snow thick- 2 (2015), Invisible polynyas: Modulation nesses to calculate the ocean-to-ice heat flux as 15 and 22 W/m at locations with thin ice in Penny Strait and of fast ice thickness by ocean heat flux South Cape Fjord, respectively.