Volume 39 Issue 9
Sep.  2020
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Xiaowei Cao, Peng Lu, Ruibo Lei, Qingkai Wang, Zhijun Li. Physical and optical characteristics of sea ice in the Pacific Arctic Sector during the summer of 2018[J]. Acta Oceanologica Sinica, 2020, 39(9): 25-37. doi: 10.1007/s13131-020-1645-6
Citation: Xiaowei Cao, Peng Lu, Ruibo Lei, Qingkai Wang, Zhijun Li. Physical and optical characteristics of sea ice in the Pacific Arctic Sector during the summer of 2018[J]. Acta Oceanologica Sinica, 2020, 39(9): 25-37. doi: 10.1007/s13131-020-1645-6

Physical and optical characteristics of sea ice in the Pacific Arctic Sector during the summer of 2018

doi: 10.1007/s13131-020-1645-6
Funds:  The National Key Research and Development Program of China under contract Nos 2017YFE0111400 and 2018YFA0605903; the National Natural Science Foundation of China under contract Nos 41922045, 41876213 and 51579024.
More Information
  • Corresponding author: E-mail: lupeng@dlut.edu.cn
  • Received Date: 2019-10-22
  • Accepted Date: 2020-01-02
  • Available Online: 2020-12-28
  • Publish Date: 2020-09-25
  • The reduction in Arctic sea ice in summer has been reported to have a significant impact on the global climate. In this study, Arctic sea ice/snow at the end of the melting season in 2018 was investigated during CHINARE-2018, in terms of its temperature, salinity, density and textural structure, the snow density, water content and albedo, as well as morphology and albedo of the refreezing melt pond. The interior melting of sea ice caused a strong stratification of temperature, salinity and density. The temperature of sea ice ranged from –0.8°C to 0°C, and exhibited linear cooling with depth. The average salinity and density of sea ice were approximately 1.3 psu and 825 kg/m3, respectively, and increased slightly with depth. The first-year sea ice was dominated by columnar grained ice. Snow cover over all the investigated floes was in the melt phase, and the average water content and density were 0.74% and 241 kg/m3, respectively. The thickness of the thin ice lid ranged from 2.2 cm to 7.0 cm, and the depth of the pond ranged from 1.8 cm to 26.8 cm. The integrated albedo of the refreezing melt pond was in the range of 0.28–0.57. Because of the thin ice lid, the albedo of the melt pond improved to twice as high as that of the mature melt pond. These results provide a reference for the current state of Arctic sea ice and the mechanism of its reduction.
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