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Airborne Observations of the Distribution, Thickness, and Drift of Different Sea Ice Types and Extreme Ice Features in the Canadian Beaufort Sea

机译:空中观察不同海冰类型的分布,厚度和漂移和加拿大博福特海的极端冰功能

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Extensive airborne electromagnetic (EM) ice thickness surveys have been performed in April 2009, 2011, and 2012 over the Canadian Beaufort Sea with a long-range airplane. These are contributing to the Beaufort Regional Environmental Assessment (BREA) project which gathers ice information in preparation of a regulatory framework for safe and environmental responsible oil and gas production. Results show that the location of the multiyear ice edge can be very variable from year to year. Multiyear ice modal thicknesses ranged between 3.0 and 3.7 m. The seasonal ice zone had very variable ice thicknesses depending on the amount and age of ice formed in coastal polynyas and leads throughout the winter. However, we gathered enough data to show that modal first-year ice thicknesses of 2.0 to 2.2 m emerge if profiles are long enough, which can be considered the most representative first-year ice thickness estimate in the Canadian Beaufort Sea in April. However, in the seasonal ice zone also regions with heavily deformed ice thicker than 10 m, and occasional multiyear hummock fields of similar thicknesses occur. Results suggest that multiyear hummock fields may not comprise the thickest ice as they are affected by melt during the summer. Two ice islands had thicknesses between 20 and 30 m. Our results suggest a melt rate of ice islands of 10 m per year in the Southern Beaufort Sea. Ice thickness surveys were complemented by the analysis of satellite radar data and tracking of ice features by means of GPS beacons. We demonstrate that all these activities combined comprise a powerful tool for a future Arctic sea ice environmental observatory.
机译:广泛的空中电磁(EM)冰厚检验已在2009年4月,2011年,长程飞机执行,和2012年在加拿大波弗特海。这些都有助于对所采集的信息冰在准备安全环保负责石油和天然气生产的监管框架的博福特区域环境评估(阿欧)项目。结果表明,多年冰边缘的位置可以有很大变化,从每年。多年冰模态厚度3.0到3.7米之间的范围内。季节性冰冻带了根据形成沿海polynyas和导线整个冬季的冰量和年龄的变化非常大冰的厚度。然而,我们收集了足够的数据来显示的2.0至2.2米情态第一年的冰厚度出现,如果配置文件是足够长的时间,这可以被认为是在加拿大波弗特海最具代表性的第一年的冰层厚度估计在四月。然而,在季节性冰区也有重变形冰厚于10μm时,和类似的厚度的偶然多年小丘字段区域发生。结果表明,多年小丘字段可能不包括最厚的冰,因为它们是通过熔体在夏季影响。两个冰岛20和30米之间有厚度。我们的研究结果表明,在南波弗特海每年10米冰岛的熔化速率。冰厚调查由卫星雷达数据的分析和补充冰跟踪由GPS信标的装置的功能。我们表明,所有这些活动总共包括为未来的北极海冰环境观测站的有力工具。

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