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AGU: Geophysical Research Letters

 

Keywords

  • sea ice
  • passive microwave
  • melt

Index Terms

  • Cryosphere: Sea ice
  • Cryosphere: Remote sensing
  • Cryosphere: Properties
  • Cryosphere: General or miscellaneous

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 36, L24501, 5 PP., 2009
doi:10.1029/2009GL041434

Perennial pack ice in the southern Beaufort Sea was not as it appeared in the summer of 2009

David G. Barber

Centre for Earth Observation Science, Faculty of Environment, Earth and Resources, University of Manitoba, Winnipeg, Manitoba, Canada

Ryan Galley

Centre for Earth Observation Science, Faculty of Environment, Earth and Resources, University of Manitoba, Winnipeg, Manitoba, Canada

Matthew G. Asplin

Centre for Earth Observation Science, Faculty of Environment, Earth and Resources, University of Manitoba, Winnipeg, Manitoba, Canada

Roger De Abreu

Canadian Ice Service, Environment Canada, Ottawa, Ontario, Canada

Kerri-Ann Warner

Centre for Earth Observation Science, Faculty of Environment, Earth and Resources, University of Manitoba, Winnipeg, Manitoba, Canada

Monika Pućko

Centre for Earth Observation Science, Faculty of Environment, Earth and Resources, University of Manitoba, Winnipeg, Manitoba, Canada

Freshwater Institute, Fisheries and Oceans, Winnipeg, Manitoba, Canada

Mukesh Gupta

Centre for Earth Observation Science, Faculty of Environment, Earth and Resources, University of Manitoba, Winnipeg, Manitoba, Canada

Simon Prinsenberg

Bedford Institute of Oceanography, Fisheries and Oceans, Halifax, Nova Scotia, Canada

Stéphane Julien

Laurentian Region, Canadian Coast Guard, Quebec, Quebec, Canada

In September 2009 we observed a much different sea icescape in the Southern Beaufort Sea than anticipated, based on remotely sensed products. Radarsat derived ice charts predicted 7 to 9 tenths multi-year (MY) or thick first-year (FY) sea ice throughout most of the Southern Beaufort Sea in the deep water of the Canada Basin. In situ observations found heavily decayed, very small remnant MY and FY floes interspersed with new ice between floes, in melt ponds, thaw holes and growing over negative freeboard older ice. This icescape contained approximately 25% open water, predominantly distributed in between floes or in thaw holes connected to the ocean below. Although this rotten ice regime was quite different that the expected MY regime in terms of ice volume and strength, their near-surface physical properties were found to be sufficiently alike that their radiometric and scattering characteristics were almost identical.

Received 22 October 2009; accepted 23 November 2009; published 24 December 2009.

Citation: Barber, D. G., R. Galley, M. G. Asplin, R. De Abreu, K.-A. Warner, M. Pućko, M. Gupta, S. Prinsenberg, and S. Julien (2009), Perennial pack ice in the southern Beaufort Sea was not as it appeared in the summer of 2009, Geophys. Res. Lett., 36, L24501, doi:10.1029/2009GL041434.

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