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Arctic Ocean outflow shelves in the changing Arctic: A review and perspectives

机译:在变化的北极地区,北冰洋流出货架:回顾与展望

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摘要

Over the past decade or so, international research efforts, many of which were part of the International Polar Year, have accrued our understanding of the Arctic outflow shelves. The Arctic outflow shelves, namely the East Greenland Shelf (EGS) and the Canadian Arctic Archipelago (CAA), serve as conduits through which Arctic sea ice and waters and their properties are exported to the North Atlantic. These shelves play an important role in thermohaline circulation and global circulation patterns, while being influenced by basin-scale and regional changes taking place in the Arctic. Here, we synthesize the current knowledge on key forcings of primary production and ecosystem processes on the outflow shelves, as they influence their structure and functionalities and, consequently their role in Arctic Ocean productivity and global biogeochemical cycles. For the CAA, a fresh outlook on interannual and decadal physical and biological time-series reveals recent changes in productivity patterns, while an extensive analysis of sea ice conditions over the past 33 years (1980–2012) demonstrates significant declines in multi-year ice and a redistribution of ice types. For the EGS, our analysis shows that sea ice export strongly contributes to structuring spatially diverse productivity regimes. Despite the large heterogeneity in physical and biological processes within and between the outflow shelves, a conceptual model of productivity regimes is proposed, helping identify general productivity patterns and key forcings. The different productivity regimes are expected to respond differently to current and future Arctic change, providing a useful basis upon which to develop predictive scenarios of future productivity states. Current primary production estimates for both outflow shelves very likely underestimate their contribution to total Arctic production.
机译:在过去的十年左右的时间里,国际研究工作(其中很多是国际极地年的一部分)使我们对北极流出架的了解加深了。北极流出架,即东格陵兰大陆架(EGS)和加拿大北极群岛(CAA),充当北极海冰和海水及其财产出口到北大西洋的管道。这些架子在热盐环流和全球环流模式中起着重要作用,同时受北极流域规模和区域变化的影响。在这里,我们综合了关于流出架上初级生产和生态系统过程的主要强迫因素的当前知识,因为它们影响了它们的结构和功能,因此影响了它们在北冰洋生产力和全球生物地球化学循环中的作用。对于CAA,对年际和年代际物理和生物时间序列的新展望揭示了生产力模式的最新变化,而对过去33年(1980-2012年)海冰状况的广泛分析表明,多年期冰的显着下降并重新分配冰种。对于EGS,我们的分析表明,海冰出口在很大程度上有助于构建空间上不同的生产力制度。尽管流出架子内部和之间的物理和生物过程存在很大的异质性,但仍提出了生产率制度的概念模型,以帮助确定总体生产率模式和关键强迫因素。预期不同的生产率制度对当前和未来的北极变化有不同的反应,为发展未来生产率状态的预测方案提供了有用的基础。目前对这两个流出架子的初步产量估算很可能低估了它们对北极总产量的贡献。

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