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2003 - 2018年波弗特环流淡水含量分析

Analysis of the Beaufort Gyre Freshwater Content in 2003-2018.

作者信息

Proshutinsky A, Krishfield R, Toole J M, Timmermans M-L, Williams W, Zimmermann S, Yamamoto-Kawai M, Armitage T W K, Dukhovskoy D, Golubeva E, Manucharyan G E, Platov G, Watanabe E, Kikuchi T, Nishino S, Itoh M, Kang S-H, Cho K-H, Tateyama K, Zhao J

机构信息

Woods Hole Oceanographic Institution Woods Hole MA USA.

Geology and Geophysics department Yale University New Haven CT USA.

出版信息

J Geophys Res Oceans. 2019 Dec;124(12):9658-9689. doi: 10.1029/2019JC015281. Epub 2019 Dec 28.

DOI:10.1029/2019JC015281
PMID:32055432
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7003849/
Abstract

Hydrographic data collected from research cruises, bottom-anchored moorings, drifting Ice-Tethered Profilers, and satellite altimetry in the Beaufort Gyre region of the Arctic Ocean document an increase of more than 6,400 km of liquid freshwater content from 2003 to 2018: a 40% growth relative to the climatology of the 1970s. This fresh water accumulation is shown to result from persistent anticyclonic atmospheric wind forcing (1997-2018) accompanied by sea ice melt, a wind-forced redirection of Mackenzie River discharge from predominantly eastward to westward flow, and a contribution of low salinity waters of Pacific Ocean origin via Bering Strait. Despite significant uncertainties in the different observations, this study has demonstrated the synergistic value of having multiple diverse datasets to obtain a more comprehensive understanding of Beaufort Gyre freshwater content variability. For example, Beaufort Gyre Observational System (BGOS) surveys clearly show the interannual increase in freshwater content, but without satellite or Ice-Tethered Profiler measurements, it is not possible to resolve the seasonal cycle of freshwater content, which in fact is larger than the year-to-year variability, or the more subtle interannual variations.

摘要

从北冰洋波弗特环流区的科研航次、海底锚定系泊设备、漂流冰系剖面仪以及卫星测高仪收集的水文数据表明,2003年至2018年期间,液态淡水含量增加了6400多公里:相对于20世纪70年代的气候平均值增长了40%。这种淡水积累被证明是由持续的反气旋大气风强迫(1997 - 2018年)伴随着海冰融化、麦肯齐河径流因风强迫从主要向东流重新定向为向西流,以及太平洋源低盐度水体经白令海峡的贡献所导致的。尽管不同观测数据存在显著不确定性,但本研究证明了拥有多个不同数据集以更全面了解波弗特环流淡水含量变化的协同价值。例如,波弗特环流观测系统(BGOS)调查清楚地显示了淡水含量的年际增加,但如果没有卫星或冰系剖面仪测量,就无法解析淡水含量的季节周期,而实际上该季节周期大于年际变化,也无法解析更细微的年际变化。

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