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Changes in sea ice conditions along the Arctic Northeast Passage from 1979 to 2012

机译:1979年至2012年沿北极东北航道的海冰状况变化

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Sea ice conditions in the Arctic Northeast Passage (NEP) have changed dramatically in the last four decades, with important impacts on the environment and navigability. In the present study, multisource remote sensing data for 1979-2012 were analyzed to quantify seasonal, interannual, and spatial changes in sea ice conditions along the NEP. Data for October-November showed that spatially averaged ice thickness in the NEP decreased from 1.2-1.3 m in 2003-2006 to 0.2-0.6 m in 2011-2012. From 1979 to 2012, the fastest decreasing trend in monthly ice concentration occurred in October (-1.76% per year, P < 0.001), when the ice cover starts to increase. As a result of decreasing multiyear sea ice, thinning ice and delayed freeze-up, the spatially averaged length of open period (ice concentration < 50%) increased from 84 days in the 1980s to 114 days in the 2000s and reached 146 days in 2012. The Kara, Laptev, and East Siberian sectors were relatively inaccessible, especially the sector of 90-110 degrees E around the Vilkitsky Strait. However, because of the thinning sea ice prior to the melt season and the enhanced positive polarity of the summer Arctic Dipole Anomaly, these sectors have become more accessible in recent years. The summer sea ice along the high-latitude sea route (HSR) north of the eastern Arctic islands, with a route distance comparable to the NEP, has also decreased during the last decade with the ice-free period reaching 42 days in 2012. The HSR avoids shallow waters along the coast, improving access to the Arctic sea route for deeper-draft vessels. (C) 2015 Elsevier B.V. All rights reserved.
机译:过去四十年来,北极东北航道(NEP)中的海冰条件发生了巨大变化,对环境和通航性产生了重要影响。在本研究中,分析了1979-2012年的多源遥感数据,以量化NEP沿线海冰条件的季节性,年际和空间变化。 10月至11月的数据显示,NEP的空间平均冰厚度从2003-2006年的1.2-1.3 m下降到2011-2012年的0.2-0.6 m。从1979年到2012年,当冰盖开始增加时,月冰浓度的下降趋势最快(10月为-1.76%,P <0.001)。由于多年海冰减少,冰层变薄和冻结时间延迟,开放期的空间平均长度(冰浓度<50%)从1980年代的84天增加到2000年代的114天,到2012年达到146天卡拉,拉普捷夫和西伯利亚东部地区相对较难进入,尤其是在维尔吉茨基海峡周围东经90-110度的地区。但是,由于融化季节之前的海冰变薄以及夏季北极偶极子异常的正极性增强,因此近年来这些区域变得更加容易获得。过去十年中,北极东部岛屿以北的高纬度海上航线(HSR)上的夏季海冰在过去十年中也有所减少,2012年的无冰期达到了42天。高铁避免了沿海岸的浅水区,为更深的船只提供了通往北极海路的通道。 (C)2015 Elsevier B.V.保留所有权利。

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