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DRIFT DIRECTION CHANGES AND IMPLICATIONS FOR SEA ICE MANAGEMENT

机译:海冰管理的方向变化及含义

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As the focus on hydrocarbon exploration and production in high Arctic environments increases, there is a need to develop and assess operational ice management procedures applicable to these areas. Particularly in water depths exceeding 100 m, bottom-founded structures are not a viable option and stationary floating vessels will likely be used. Ice management in the form of icebreakers is a key component for station-keeping by reducing floe sizes upstream to decrease subsequent loads on the floating vessel. Drift changes in the Beaufort Sea can be frequent and complete drift reversals can occur in only a few hours. The highly dynamic nature of ice drift can be problematic when maintaining a managed ice channel for a station-keeping vessel. This paper assesses ice drift characteristics based on an analysis of Acoustic Doppler Current Profiler and Ice Profiling Sonar data collected in the Beaufort Sea from 1990 to 2003 and identifies quantitative measures of drift direction change.
机译:随着在北极高海拔环境中对油气勘探和生产的关注日益增加,有必要制定和评估适用于这些地区的冰管理程序。特别是在水深超过100 m的情况下,基于底部的结构不是可行的选择,并且可能会使用固定式浮船。破冰船形式的制冰管理是保持站位的关键组成部分,它可以减少上游的絮凝物尺寸,从而减少后续在浮船上的负荷。博福特海的漂流变化可能很频繁,而完全的漂流逆转仅在几个小时内就会发生。当为固定站的船只维护可管理的冰道时,冰漂移的高度动态性可能会带来问题。本文基于对1990年至2003年在波弗特海收集的声学多普勒电流剖面仪和冰剖面声纳数据的分析,评估了冰的漂移特征,并确定了漂移方向变化的定量度量。

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