Abstract
Sea ice is the predominant natural threat to marine structures and oil-gas exploitation in the Arctic. However, for ice-resistant structural design, long-term successive level ice thickness measurements are still lacking. To fill this gap in the southern Kara Sea, the Los Alamos Sea Ice Model (CICE) is applied to achieve better simulation at the local and regional scales. Based on the validation against ice thickness observations in March and April in 1980–1986, the statistical root-mean-square error is determined to be less than 0.2 m. Then, based on the hindcast data, the spatiotemporal distributions of level ice thickness are analyzed annually, seasonally, and monthly, with thicker level ice of 1.2–1.5 m in spring and large ice-free zones in September and October. For floating platforms, a novel ice grade criterion with five classifications, namely, excellent, good, moderate, severe, and catastrophic, is proposed. The first two grades are most suitable for offshore activities, particularly from August to October, and the moderate grade is acceptable if with ice-resistant protections. Furthermore, hostile ice conditions are discussed in terms of the generalized extreme value distribution. The statistics reveal that at a return period of 100 yr, extreme level ice is primarily between 0.6 m and 1.0 m in December. The present investigation could be a useful reference for a feasibility study of the potential risk analysis and ice-resistant operation of oil-gas exploitation in the Arctic.
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The study is supported by the National Key Research and Development Program of China (No. 2016YFC0303401), the National Natural Science Foundation of China (No. 51779236), and the National Natural Science Foundation of China—Shandong Joint Fund (No. U1706226).
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Duan, C., Wang, Z. & Dong, S. Intensity of Level Ice Simulated with the CICE Model for Oil-Gas Exploitation in the Southern Kara Sea, Arctic. J. Ocean Univ. China 21, 1099–1108 (2022). https://doi.org/10.1007/s11802-022-4914-5
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DOI: https://doi.org/10.1007/s11802-022-4914-5