Mooring-based (YS06) data collected in the period May-June 2014 in Young Sound, Greenland

Time series of currents were obtained in the period May- June 2014 by use of an ice-tethered mooring in Young Sound, Greenland. At YS06 (74.245o N, 20.229o W) the mooring consisted of a 600 kHz downward-looking Nortek Aquadopp ADCP. Velocities were corrected for magnetic deviation (18.5o). The water column sampling spanned between 1.5 and 30 m depth every 30 min. The ADCP was set to sample 80 bins (bin size of 0.5 m) and each bin consisted of a 1 min ensamble average of 60 pings. The first and last bins were centred at 1m and 41 m depth. Only bins between 2.5 and 30 m were adequately measured. For further details see Boone et al., 2017 (Circulation and fjord-shelf exchange during the ice-covered period in Young Sound-Tyrolerfjord, Northwest Greenland (74o N). Estuar. Coast. Shelf Sci., 15, 194-205. https://doi.org/10.1016/j.ecss.2017.06.021).2014年5月至6月期间，研究团队于格陵兰扬松德（Young Sound）海域，借助冰系锚系装置获取了海流时间序列数据。该锚系布设于YS06站点（北纬74.245°，西经20.229°），搭载一台600 kHz向下观测的Nortek Aquadopp型声学多普勒流速剖面仪（Acoustic Doppler Current Profiler，ADCP）。海流流速数据已完成磁偏角校正（磁偏角为18.5°）。水柱采样覆盖1.5米至30米水深范围，采样间隔为30分钟。该ADCP设置为采集80个采样分层（分层厚度0.5米），每个分层取60次声脉冲的1分钟集合平均结果。首个与最末采样分层分别以1米和41米水深为中心，仅2.5米至30米水深范围内的分层数据测量质量达标。更多细节可参见Boone等人2017年的研究成果：《西北格陵兰扬松德-蒂罗勒峡湾冰期的环流与峡陆架交换》，刊载于《河口、海岸与陆架科学》（*Estuar. Coast. Shelf Sci.*）第15卷，第194-205页，DOI: 10.1016/j.ecss.2017.06.021。