Abstract
JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 114,
C00A04,
17 PP., 2009
doi:10.1029/2008JC004892
Transpolar observations of the morphological properties of Arctic sea ice
CRREL, ERDC, Hanover, New Hampshire, USA
Department of Atmospheric Sciences, University of Washington, Seattle, Washington, USA
Polar Science Center, University of Washington, Seattle, Washington, USA
CRREL, ERDC, Hanover, New Hampshire, USA
Geophysical Institute, University of Alaska Fairbanks, Fairbanks, Alaska, USA
Thayer School of Engineering, Dartmouth College, Hanover, New Hampshire, USA
Terry Tucker Research, Enfield, New Hampshire, USA
Thayer School of Engineering, Dartmouth College, Hanover, New Hampshire, USA
During the 5 August to 30 September 2005 Healy Oden Trans-Arctic Expedition a trans-Arctic survey of the physical properties of the polar ice pack was conducted. The observational program consisted of four broad classes of snow and ice characterization activities: observations made while the ship was in transit, ice station measurements, helicopter survey flights, and the deployment of autonomous ice mass balance buoys. Ice conditions, including ice thicknesses, classes, and concentrations of primary, secondary, and tertiary categories were reported at 2-hour intervals. Pond fractions were large early in the cruise at the southern edge of the ice pack, reaching peak values of 0.5 and averaging 0.25. Ice concentrations ranged from 0.8 to 1.0 north of 79°N, save for an area between 88°30′N and 89°30′N, where polynyas and thin ice were observed. Surveys of snow depth, ice thickness, and ice properties were conducted at ice stations. Thickness observations suggest a general latitudinal trend of increasing ice thickness moving northward, with considerable variability from floe to floe and within a single floe. Average floe thicknesses varied from 1.0 to >2.8 m, and the standard deviation of thickness on an individual floe was as large as 1 m. Ice crystallography showed a large amount of granular ice. The average optical-equivalent soot content was 4 ng C g−1 for new snow, 8 ng C g−1 for the surface granular layer of multiyear ice, and 18 ng C g−1 for the interior of multiyear ice, indicating a tendency of the particulates to concentrate at the surface with melting.
Received 28 April 2008; accepted 13 November 2008; published 30 January 2009.
Citation: (2009), Transpolar observations of the morphological properties of Arctic sea ice, J. Geophys. Res., 114, C00A04, doi:10.1029/2008JC004892, [printed 115(C1), 2010].
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