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Variation in Water Masses on Shelf of Northern Bering Sea in September 2016-2018
Authors:Yingjie Wang  Na Liu  Lina Lin  Yan He  Bin Kong  Zhanhai Zhang
Institution:1. College of Oceanic and Atmospheric, Ocean University of China, Qingdao, China;2. Key Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, Minsitry of Natural Resources, Qingdao, China;3. Laboratory for Regional Oceanography and Numerical Modeling, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China;4. wangyj@fio.org.cn;6. Key Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, Minsitry of Natural Resources, Qingdao, China;7. Ministry of Natural Resources of the People’s Republic of China, Beijing, China
Abstract:Abstract

Based on hydrological data obtained during the 7th to 9th Chinese National Arctic Research Expeditions in the summers of 2016–2018, the main water structure on the shelf of the northern Bering Sea and the volume and heat fluxes of the Bering Strait throughflow were analyzed. Distinct variability was identified in the three Pacific water masses feeding the strait - Anadyr Water (AW), Bering Shelf Water (BSW) and Alaskan coastal water (ACW). Overall, the temperature and salinity of the entire section increased each year, with 2018 showing significant anomalies, i.e., a temperature anomaly of up to 1?°C and a maximum salinity anomaly of 2. From 2016 to 2018, the extent of the ACW gradually narrowed in the eastern part of this section, while the AW expanded eastward each year. The net volume transport through each of the three sections increased poleward from 1.65?Sv to 2.76?Sv, with the AW increasing from 0?Sv to 1.03?Sv, the BSW varying between 0.52–1.65?Sv, and the ACW gradually decreasing from 1.04?Sv to disappearing completely. The net heat fluxes were also poleward, varying between 25.77 TW and 61.50 TW, and showing a significant increase. Significant variations in magnitude and extent were observed in each water mass of the Bering Strait throughflow, which could produce widespread effects in the Arctic Ocean and the global ocean beyond.
Keywords:Heat fluxes  interannual variations  Northern Bering Sea shelf  volume transports  water properties
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