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Formation of ice compression and ice divergence zones on the north-east Sakhalin shelf under tidal ice drift

机译:在潮汐冰漂移下,在东北萨哈林架上形成冰压缩和冰散络区

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For effective support of offshore ice-resistant structures on the north-east Sakhalin shelf during winter season it is necessary to know the variability of ice cover distribution over the water area. Ice cover redistribution followed by formation of ice compression and ice divergence zones over the Sakhalin offshore water area was earlier observed (Kalinin F.N., Truskov P.A., 1996; Kalinin F.N. 1999) as a function of various metocean conditions. Consideration and forecast of ice compression/divergence zones will facilitate efficient planning of vessels operation to support offshore ice-resistant structures. Synchronous observations of ice drift based on three onshore radar stations (RS) (cape Levenstern, bay Odoptu, village Komrvo) allow the tracing of ice cover distribution variation under changing metocean conditions in the near-shore zone of the north-east Sakhalin shelf.
机译:有效支持在冬季在东北萨哈林货架上的海上抗冰结构,有必要了解水域冰盖分布的可变性。冰盖再分配,然后形成冰素近海水域的冰压缩和冰分歧区,早期观察到(Kalinin F.N.,Truskov P.A.,1996; Kalinin F.n.1999)作为各种市区条件的职能。冰压缩/分离区的考虑和预测将促进血管操作的高效规划,以支持海上抗抗抗抗抗抗抗抗抗抗抗抗抗抗抗抗抗抗抗抗抗抗抗抗性结构。基于三个陆上雷达站(RS)(Cape Levenstern,Bay Odoptu,Village Komrvo)的冰漂的同步观察允许在东北萨哈林架近岸区改变冰区岩覆盖冰覆盖分配变化。

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