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Mid-winter freeze experiment in the Arctic Ocean: Norwegian Young sea ICE cruise (N-ICE2015)

机译:北冰洋中冬冻结实验:挪威年轻海冰巡游(N-ICE2015)

摘要

In mid-January 2015, RV Lance will freeze into the ice north of Svalbard, Arctic Ocean at around 83.25°N 30°E, and passively drift with the ice as part of the Norwegian Young sea ICE cruise (N-ICE2015). Judging from historic sea ice drift trajectories, it is likely that RV Lance will drift in a SW direction and the ship will probably be freed from the ice in mid spring after about two to three months of drift. Thereafter, RV Lance will return to her starting position and start a new drift. Under all circumstances, the ice drift project will end in late June 2015. Throughout the cruise the focus will be on the interaction of the atmosphere-ice-ocean system and the response of the marine ecosystem to the thinner ice regime. The overall goal of the project team is to improve our understanding of the role of the younger ice pack in the Arctic on greenhouse gas fluxes and to ultimately assess whether the Arctic Ocean is a sink or source of greenhouse gases. We plan to conduct long-term synchronous observations of Arctic snow and sea ice biogeochemistry and physics and fluxes of carbon dioxide, methane, nitrous oxide and bromoform. This work targets at filling a crucial gap in our understanding of the role of Arctic sea ice in the climate system. This is done by conducting state of the art observations on Arctic sea ice in the polar night, when observations are basically non-existent. Further we are focusing on the new thinner ice regime, which is even less documented. We aim to understand how the thinner sea ice in the Arctic basin contributes (i) to important greenhouse gas exchange between the atmosphere and ocean and (ii) to aerosol formation, that contribute to the radiative balance of the planet. This work will increase direct collaboration between Japanese and European scientists in the Arctic, and combines complimentary expertise and experience from several international partners to carry out the interdisciplinary work proposed.
机译:在2015年1月中旬,RV Lance将在北冰洋北冰洋以83.25°N 30°E的速度冻结到冰层中,并随冰层被动漂移,这是挪威青年海冰巡游的一部分(N-ICE2015)。从历史上的海冰漂移轨迹来看,RV Lance可能会沿SW方向漂移,并且在漂移约2至3个月后的春季中,船舶可能会脱离冰层。此后,RV Lance将返回到她的起始位置并开始新的漂移。在任何情况下,冰漂项目都将在2015年6月下旬结束。在整个航行过程中,重点将放在大气-冰-海洋系统的相互作用以及海洋生态系统对更薄的冰层制度的响应上。该项目小组的总体目标是增进我们对北极地区年轻冰袋对温室气体通量的作用的了解,并最终评估北冰洋是否是温室气体的汇或源。我们计划对北极雪和海冰的生物地球化学和物理学以及二氧化碳,甲烷,一氧化二氮和溴仿的通量进行长期同步观测。这项工作旨在填补我们对北极海冰在气候系统中的作用的认识上的关键空白。当根本不存在观测时,可以通过在极地夜晚对北极海冰进行最先进的观测来完成此操作。此外,我们将重点放在新的更薄的冰层机制上,该机制的文献资料更少。我们旨在了解北极盆地中较薄的海冰如何(i)促进大气与海洋之间重要的温室气体交换,以及(ii)促进地球辐射平衡的气溶胶形成。这项工作将增进日本和欧洲科学家在北极的直接合作,并结合一些国际合作伙伴提供的专业知识和经验,以开展拟议的跨学科工作。

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