Abstract
During the 3rd Chinese National Arctic Research Expedition cruise in the summer of 2008, nutrients (NO3, NO2, SiO23 , and PO34 ) and dissolved oxygen were measured in the western Arctic Ocean, to derive the vertical distribution of nutrient tracers and its relationship to water structure and biogeochemical processes. The nutrient data show that surface waters had the lowest NO3/PO34 (mean of 0.5) and SiO23 /PO3 (mean of 2.8) values in the water column, suggesting an excess of phosphate. Winter Bering Shelf water (wBSW) had high Si* (16.7 µmol/L; Si*=[Si(OH)4]-[NO3]) with negative N* (−11.7 µmol/L; N*=[PO34 ]-16[PO34 ]+3.5 µmol/L) in the water column, indicating nitrate deficiency. The warm Atlantic layer had positive N* (0.8 µmol/L) and negative Si* (−5.4 µmol/L) compared with Pacific source water. The vertical distribution of nutrients indicates that wBSW can be characterized by N* minimum and Si* maximum. In contrast, minima of Si* and SiO23 /PO34 below 200 m indicate the distribution of Atlantic warm water.
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The National Natural Science Foundation of China under contract Nos 41941013, 41776205, 41976226 and 41806228; the Scientific Research Funds of Second Institute of Oceanography, Ministry of Natural Resources, under contract No. QNYC2003; the Chinese Polar Environment Comprehensive Investigation & Assessment Programs under contract Nos 0304 and 0402.
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We thank the crew members of the Xuelong icebreaker during Chinese Arctic Expeditions. CTD data were provided by Jinping Zhao from the Ocean University of China and issued through a polar scientific data sharing platform maintained by the Chinese National Arctic and Antarctic Data Center (CN-AADC: (http://www.chinare.org.cn). Thanks are also given to Zhengbing Han from the Second Institute of Oceanography for help with fieldwork.
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Zhuang, Y., Li, H., Jin, H. et al. Vertical distribution of nutrient tracers in the western Arctic Ocean and its relationship to water structure and biogeochemical processes. Acta Oceanol. Sin. 39, 109–114 (2020). https://doi.org/10.1007/s13131-020-1651-8
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DOI: https://doi.org/10.1007/s13131-020-1651-8