4.0 Article

Increase in Storm Activity in the Kara Sea from 1979 to 2019: Numerical Simulation Data

期刊

DOKLADY EARTH SCIENCES
卷 498, 期 2, 页码 502-508

出版社

MAIK NAUKA/INTERPERIODICA/SPRINGER
DOI: 10.1134/S1028334X2106012X

关键词

storm activity; Kara Sea; wind waves; wave modeling; sea ice cover extent decline

资金

  1. Russian Foundation for Basic Research [18-05-60147]
  2. Interdisciplinary Scientific and Educational School of Moscow State University The Future of the Planet and Global Environmental Changes
  3. [0128-2021-0002]

向作者/读者索取更多资源

This study analyzes storm activity in the Kara Sea from 1979 to 2019 using a wind wave model, finding that with decreasing sea ice extent, storm frequency has significantly increased. The largest amount of storms occur from July to December, with a strong positive trend observed from October to December. Storms in January to March have been observed due to the absence of ice cover.
Wind wave modeling (WAVEWATCH III model) is used to analyze the storm activity in the Kara Sea for the period from 1979 to 2019. The NCEP/CFSR/CFSv2 reanalysis data used as forcing. Simulations realized on the nonstructural grid with a resolution of 700 m to 10 km. The quality of wind wave simulation is assessed through a comparison with direct measurements and satellite data. The storm wave frequencies are analyzed separately for each year. It is found that storms with waves more than 3 m are observed on average about 30 times a year. The frequency of storms with waves more than 3-5 m increased twofold from 1979 to 2019. The increase in the storm frequency is due to a decrease in the sea ice cover extent. Analysis of the seasonal variations in storm activity shows that the largest amount of storms is observed from July to December. A strong positive trend in the frequency of storms is observed from October to December. Storms in January, February, and March have been observed since 2005 due to the absence of ice, which contributes significantly to the ultimate increase in the storm frequency.

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