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  • Wiley-Blackwell  (2)
  • 1
    Publication Date: 2015-11-20
    Description: The annual cycle of modal and mean sea ice thickness was derived from upward looking sonar ice thickness observations (1990-2011) in Fram Strait. The average annual peak-to-trough amplitude of the mode of 0.54 m is superimposed on interannual variability with peak-to-trough amplitudes of 0.73 m on timescales of 6-8 years, which again is superimposed on a long-term trend of -0.55 m/decade over the observation period. The long-term trend is stronger for April than for August, the average months of maximum and minimum modal thickness. As a result, the annual peak-to-trough modal thickness amplitude was reduced by 30% between the 1990s and the 2000s. The average annual peak-to-trough amplitude of the mean ice thickness of 1.20 m is also superimposed on interannual variability, with as much as 0.97 m thickness change over only 3 years. These two modes of variability are superimposed on a long-term trend of -0.35 m/decade through the entire data set. In contrast to the modal thickness, the long-term trend is weaker for the average month of maximum mean thickness (June), than for the average month of minimum (September). Therefore, the annual peak-to-trough amplitude of the mean ice thickness increased by 14% between the 1990s and the 2000s. This article is protected by copyright. All rights reserved.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
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  • 2
    Publication Date: 2014-10-02
    Description: An attempt to quantify the temporal variability in the volume composition of Arctic sea ice is presented. Categories of sea ice in the Transpolar Drift in Fram Strait are derived from monthly ice thickness distributions obtained by moored sonars (1990-2011). The inflection points on each side of the old ice modal peak are used to separate modal ice from ice which is thinner and thicker than ice in the modal range. The volume composition is then quantified through the relative amount of ice belonging to each of the three categories thin, modal and thick ice in the monthly ice thickness distributions. The trend of thin ice was estimated to be negative at -9.2% per decade (relative to the long-term mean), which was compensated for by increasing trends in modal and thick ice of 8.1% and 4.9% per decade, respectively. A 7-8 year cycle is apparent in the thin and thick ice records, which may explain a loss of deformed ice since 2007. We also quantify how the categories contribute to the mean ice thickness over time. Thick (predominantly deformed) ice dominates the mean ice thickness, constituting on average 66% of the total mean. Following the loss of deformed ice since 2007, the contribution of thick ice to the mean decreased from 75% to 52% at the end of the record. Thin deformed ice did not contribute to this reduction; it was pressure ridges thicker than 5 m that were lost and hence caused the decrease in mean ice thickness.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Location Call Number Limitation Availability
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