黄海溶解无机氮时空变化及其水团对DIN总量的影响

金春洁; 张传松; 王丽莎; 石晓勇; 韩秀荣; 唐洪杰

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中国环境科学 ›› 2021, Vol. 41 ›› Issue (4) : 1642-1654.

水污染与控制

黄海溶解无机氮时空变化及其水团对DIN总量的影响

金春洁^1,2, 张传松^1,2, 王丽莎^1,2, 石晓勇^1,2,3, 韩秀荣^1,2, 唐洪杰^1,2

作者信息 +

Spatial-temporal variation of dissolved inorganic nitrogen (DIN) and impacts of water mass on the reserves estimation of the total DIN content in the Yellow Sea

JIN Chun-jie^1,2, ZHANG Chuan-song^1,2, WANG Li-sha^1,2, SHI Xiao-yong^1,2,3, HAN Xiu-rong^1,2, TANG Hong-jie^1,2

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摘要

本文根据2013~2016年4个航次调查资料，研究了黄海水体中溶解无机氮（DIN）的时空变化及其总量影响因素.结果表明：春、夏、秋和冬季黄海调查海域DIN平均浓度分别为（5.43±4.02），（4.47±3.16），（7.46±3.56）和（5.09±2.59）μmol/L.其中，秋季浓度最高，夏季最低；黄海调查海域各季节DIN的分布呈现近岸高、外海低的变化规律，近岸高值点多集中在长江口以北、山东半岛和辽东半岛等处.春~秋季影响DIN分布的因素主要是陆源输入和浮游植物的生长繁殖，冬季则主要是河流输入和沉积物再悬浮作用.四季在中央海域底层还存在一个高值区（>6μmol/L），主要受黄海冷水团和黄海暖流等共同影响；通过聚类分析法对黄海四季水团进行了基本划分，调查海域主要包括5个水团：黄海混合水团、黄海冷水团、黄海暖流水、沿岸水团和黄东海混合水团，除黄海混合水团终年存在外，其他水团均为季节性存在；调查海域DIN总量四季差异不大，整体含量介于1.0×10⁶~1.5×10⁶t，春、夏、秋和冬季DIN总量分别约为1.2×10⁶，1.0×10⁶，1.5×10⁶和1.3×10⁶t.春季和夏季受浮游植物吸收影响，DIN总量略低，从水团对DIN总量的贡献上来看，春季以黄海暖流为主，夏季以黄海冷水团为主，秋、冬季以黄海混合水团为主.

Abstract

Based on the data of 4 curies in 2013~2016, the distribution of DIN in the Yellow Sea、nitrogen pool and its influencing factors have been studied. Results showed that the average concentrations of DIN in the Yellow Sea were (5.43±4.02) μmol/L in spring, (4.47±3.16) μmol/L in summer, (7.46±3.56) μmol/L in autumn, and (5.09±2.59) μmol/L in winter, among which DIN contents reached maximum in autumn and minimum in summer, respectively. DIN concentrations declined from coastal zones to the offshore area. The DIN-rich sites near the coast were mostly centralized in the north of the Yangtze River estuary, Shandong Peninsula and Liaodong Peninsula. The main affecting factors all the year except winter were terrigenous input and the growth of phytoplankton, as the resuspension of the riverine input and sediment were the main factors affecting the distribution of DIN in winter. There was an area with high concentration of DIN(>6μmol/L) in the central area, which was co-influenced by the Yellow Sea warm current and the Yellow Sea Cold Water Mass. Cluster analysis has been used to classified the Yellow Sea water into 5 water masses, including the Yellow Sea water masses (Y), Yellow Sea cold water mass (YC), Yellow Sea warm current water (YW), Coastal water mass (CW) and Yellow Sea-East China Sea mixed water mass (YE), which was the main water mass in the researching sea area. All these water masses except for Y were seasonal. The total DIN content in the research field showed no obvious difference in all year, and their range was 1.0×10⁶~1.5×10⁶t. The DIN content was slightly lower in spring and summer under the influence of phytoplankton assimilation. The total DIN contents were about 1.2×10⁶t in spring, 1.0×10⁶t in summer, 1.5×10⁶t in autumn, and 1.3×10⁶t in winter, respectively. The contributions of water masses to the total DIN content were different in the varying season. In autumn and winter, Y was dominant, while in summer and spring, YW and YC played the dominant roles, respectively.

导出引用

金春洁, 张传松, 王丽莎, 石晓勇, 韩秀荣, 唐洪杰. 黄海溶解无机氮时空变化及其水团对DIN总量的影响[J]. 中国环境科学. 2021, 41(4): 1642-1654

JIN Chun-jie, ZHANG Chuan-song, WANG Li-sha, SHI Xiao-yong, HAN Xiu-rong, TANG Hong-jie. Spatial-temporal variation of dissolved inorganic nitrogen (DIN) and impacts of water mass on the reserves estimation of the total DIN content in the Yellow Sea[J]. China Environmental Science. 2021, 41(4): 1642-1654

中图分类号： X55

参考文献

[1] 米铁柱,姚庆祯,孟佳,等.2011年春、夏季黄海、东海营养盐分布特征研究[J]. 海洋与湖沼, 2012,43(3):678-688. Mi T Z, Yao Q Z, Meng J, et al. Distributions of nutrients in the Southern Yellow Sea and East China Sea in spring and summer 2011[J]. Oceanologia et Limnologia Sinica, 2012,43(3):678-688.
[2] Wei Q S, Yu Z G, Wang B D, et al, Coupling of the spatial-temporal distributions of nutrients and physical conditions in the southern Yellow Sea[J]. Journal of Marine Systems, 2016,156:30-45.
[3] 王保栋,王桂云,郑昌洙,等.南黄海营养盐的平面分布及横向输运[J]. 海洋学报, 1999,21(6):124-129. Wang B D, Wang G Y, Zheng C Z, et al. Horizontal distributions and transportation of nutrients in the southern Huanghai Sea[J]. Haiyang Xuebao, 1999,21(6):124-129.
[4] 王保栋.黄海和东海营养盐分布及其对浮游植物的限制[J]. 应用生态学报, 2003,14(7):1122-1126. Wang B D. Nutrient distributions and their limitation on phytoplankton in the Yellow Sea and the East China Sea[J]. Chinese Journal of Applied Ecology, 2003,14(7):1122-1126.
[5] Liu S M, Hong G H, Zhang J, et al. Nutrient budgets for large Chinese estuaries[J]. Biogeosciences, 2009,6(10):2245-2263.
[6] 韦钦胜,于志刚,冉祥滨,等.黄海西部沿岸流系特征分析及其对物质输运的影响[J]. 地球科学进展, 2011,26(2):145-156. Wei Q S, Yu Z G, Ran X B, et al. Characteristics of the Western Coastal Current of the Yellow Sea and its impacts on material transportation[J]. Advances in Earth Science, 2011,26(2):145-156.
[7] 韦钦胜,臧家业,魏修华,等.秋季南黄海西部营养盐的分布及其与环流场的关系[J]. 海洋学报, 2011,33(1):74-82. Wei Q S, Zang J Y, Wei X H, et al. The distribution of nutrients and the relationship of them with the circulation condition in the western southern Huanghai Sea in autumn[J]. Haiyang Xuebao, 2011,33(1):74-82.
[8] Zheng L W, Zhai W D, Wang L F, et al. Improving the understanding of central Bohai Sea eutrophication based on wintertime dissolved inorganic nutrient budgets:Roles of North Yellow Sea water intrusion and atmospheric nitrogen deposition[J]. Environmental Pollution, 2020,267:115626.
[9] Abal E G, Bunn S E, Dennison W C. Healthy waterways healthy catchments:Making the connection in South East Queensland[M]. Moreton Bay Waterways and Catchments Partnership, Brisbane, Australia, 2005:240.
[10] Wang J J, Yu Z G, Wei Q S, et al. Long-term nutrient variations in the Bohai Sea over the past 40years[J]. Journal of Geophysical Research:Oceans, 2018,124(1):703-722.
[11] Wei Q S, Wang B D, Yao Q Z, et al. Hydro-biogeochemical processes and their implications for Ulva prolifera blooms and expansion in the world's largest green tide occurrence region (Yellow Sea, China)[J]. The Science of the Total Environment, 2018,645(DEC.15):257-266.
[12] Gilbert P M. Eutrophication, harmful algae and biodiversity-Challenging paradigms in a world of complex nutrient changes[J]. Marine Pollution Bulletin, 2017,124(2):591-606.
[13] Ferreira J G, Bricker S B, Simas T C. Application and sensitivity testing of a eutrophication assessment method on coastal systems in the United States and European Union[J]. Journal of Environmental Management, 2007,82(4):433-445.
[14] Jackson C, Preston N, Thompson P J, et al. Nitrogen budget and effluent nitrogen components at an intensive shrimp farm[J]. Aquaculture, 2003,218(1-4):397-411.
[15] Naylor R L, Goldburg R J, Mooney H. Natures subsidies to shrimp and salmon farming[J]. Science, 1998,282:883-884.
[16] 王俊杰,于志刚,韦钦胜,等.2017年春、夏季南黄海西部营养盐的分布特征及其与浒苔暴发的关系[J]. 海洋与湖沼, 2018,49(5):1045-1053. Wang J J, Yu Z G, Wei Q S, et al. Distributions of nutrients in the Western South Yellow Sea in spring and summer of 2017 and their relationship with Ulva prolifera outbreaks[J]. Oceanologia et Limnologia Sinica, 2018,49(5):1045-1053.
[17] 李绪录,张军晓,史华明,等.深圳湾及邻近沿岸水域总溶解氮的分布、组成和来源及氮形态的转化[J]. 环境科学学报, 2014,34(8):2027-2034. Li X L, Zhang J X, Shi 11M, et al. Transformation of nitrogenous forms, and composition, sources and distributions of total dissolved nitrogen in the Shenzhen Bay and adjacent coastal waters[J]. Acta Scientiae Circumstantiae, 2014,34(8):2027-2034.
[18] Lin A, Shen S, Wang G, et al. Comparison of chlorophyll and photosynthesis parameters of floating and attached Ulva prolifera[J]. Journal of integrative plant biology, 2011,53(1):25-34.
[19] Keesing J K, Liu D, Fearns P, et al. Inter-and intra-annual patterns of Ulva prolifera green tides in the Yellow Sea during 2007~2009, their origin and relationship to the expansion of coastal seaweed aquaculture in China[J]. Marine Pollution Bulletin, 2011,62(6):1169-1182.
[20] Li H M, Zhang C S, Han X R, et al. Changes in concentrations of oxygen, issolved nitrogen, phosphate, and silicate in the southern Yellow Sea, 1980~2012:sources and seaward gradients[J]. Estuarine Coastal and Shelf Science, 2015,163(20):44-55.
[21] Perrot T, Rossi N, Ménesguen A, et al. Modelling green macroalgae blooms on the coasts of Brittany, France to enhance water quality management[J]. Journal of Marine Systems, 2014,132(4):38-53.
[22] Liu D Y, Keesing J K, Dong Z, et al. Recurrence of Yellow Sea green tide in June 2009 confirms coastal seaweed aquaculture provides nursery for generation of macroalgae blooms[J]. Marine Pollution Bulletin, 2010,60(9):1423-1432.
[23] Liu D Y, Keesing J K, Xing Q, et al. World's largest macroalgal bloom caused by expansion of seaweed aquaculture in China[J]. Marine Pollution Bulletin, 2009,58(6):888-895.
[24] Nelson T A, Nelson A V, Tjoelker M. Seasonal and spatial patterns of Green Tides (ulvoid algal blooms) and related water quality parameters in the coastal waters of Washington State, USA[J]. Botanica Marina, 2003,46(3):263-275.
[25] Li H M, Zhang Y Y, Chen J, et al. Nitrogen uptake and assimilation preferences of the main green tide alga Ulva prolifera in the Yellow Sea, China[J]. Journal of Applied Phycology, 2019,31(1):625-635.
[26] 吴老五,韩秀荣,吴婷,等.重金属对浒苔吸收硝酸盐的动力学特性影响[J]. 中国环境科学, 2016,36(4):1173-1180. Wu L W, Han X R, Wu T, et al. Effects of heavy metals on the uptake of nitrate by Ulva prolifera.[J]. China Environmental Science, 2016, 36(4):1173-1180.
[27] 张海波,王爽,尹航,等.2018年南黄海浒苔绿潮发展规律及氮组分的作用探究[J]. 海洋学报, 2020,42(8):40-49. Zhang H B, Wang S, Yin H, et al. The development of Ulva prolifera green tide and the roles of nitrogen nutrients in it in the southern Yellow Sea in 2018[J]. Haiyang Xuebao, 2020,42(8):40-49.
[28] Shi X Y, Qi M Y, Tang H J, et al. Spatial and temporal nutrient variations in the Yellow Sea and their effects on Ulva prolifera blooms[J]. Estuarine, Coastal and Shelf Science, 2015,163:36-43.
[29] Morand P, Merceron M. Coastal eutrophication and excessive growth of macroalgae[J]. Recent Research Developments in Environmental Biology, 2004,1:395-449.
[30] Teichberg M, Fox S E, Olsen Y S, et al. Eutrophication and macroalgae blooms in temperate and tropical coastal waters:nutrient enrichment experiments with Ulva spp[J]. Global Change Biology, 2010,16:2624-2637.
[31] Liu D Y, Keesing J K, He P M, et al. The world's largest macroalgae bloom in the Yellow Sea, China:formation and implications. Estuarine[J]. Coastal and Shelf Science, 2013,129:2-10.
[32] Chen L, Li C, Zhou K, Shi Y, et al. Effects of nutrient limitations on three species of zooplankton[J]. Haiyang Xuebao, 2018,37:58-68.
[33] Li H M, Zhang Y Y, Tang H J, et al. Spatiotemporal variations of inorganic nutrients along the Jiangsu coast, China, and the occurrence of macroalgal blooms (green tides) in the southern Yellow Sea[J]. Harmful Algae, 2017,63:164-172.
[34] GB/T. 12763.3-2007海洋调查规范[S]. GB/T. 12763.3-2007 Specification of oceanographic investigation[S].
[35] 邱道立,周诗赉,李昌明.应用聚类分析法划分黄海水团的初步研究[J]. 海洋学报(中文版), 1984,(3):281-292. Qiu D L, Zhou S L, Li C M. Application of cluster analysis method in determining water mass of the Huanghai Sea[J]. Haiyang Xuebao, 1984,(3):281-292.
[36] 李凤岐,苏育嵩,喻祖祥.聚类分析在浅海变性水团分析中的试验[J]. 海洋学报, 1983,(6):675-686. Li F Q, Su Y S, Yu Z X. Application of cluster analysis method to modified water masses in the shallow sea[J]. Haiyang Xuebao, 1983,(6):675-686.
[37] 李凤岐,苏育嵩,王凤钦,等.用模糊集合观点讨论水团的有关概念[J]. 海洋与湖沼, 1986,17(2):102-110. Li F Q, Su Y S, Wang F Q, et al. Discussion of some concepts of the water mass by the theory of fuzzy sets[J]. Oceanologia et Limnologia Sinica, 1986,17(2):102-110.
[38] 臧璐.北黄海生源要素的季节特征及冷水团对其影响的研究[D]. 山东:中国海洋大学, 2009. Zang L. The Research of biogenic elements' seasonal characteristics in the North Yellow Sea and the contribution of the North Yellow Sea Cold water mass[D]. Shandong:Ocean University of China, 2009.
[39] Wang J J, Yu Z G, Wei Q S, et al. Intra-and inter-seasonal variations in the hydrological characteristics and nutrient conditions in the southwestern Yellow Sea during spring to summer[J]. Marine Pollution Bulletin, 2020,156(111139):1-15.
[40] 赵晨英,臧家业,刘军,等.黄渤海氮磷营养盐的分布,收支与生态环境效应[J]. 中国环境科学, 2016,36(7):2115-2127. Zhao C Y, Zang J Y, Liu J, et al. Distribution and budget of nitrogen and phosphorus and their influence on the ecosystem in the Bohai Sea and Yellow Sea[J]. China Environmental Science, 2016,36(7):2115-2127.
[41] 王丽莎,张传松,王颢,等.夏季黄渤海生源要素的平面分布特征[J]. 海洋环境科学, 2015,34(3):361-366,383. Wang L S, Zhang C S, Wang H, et al. Horizontal distribution features of biogenic elements in Bohai Sea and the Yellow Sea in summer[J]. Marine Environmental Science, 2015,34(3):361-366,383.
[42] 殷京玉,金春洁,石晓勇,等.2013年夏秋季黄海溶解无机氮的分布及季节变化特征[J]. 海洋通报, 2017,36(1):74-81. Yin J Y, Jin C J, Shi X Y, et al. Distribution and seasonal variation in dissolved inorganic nitrogen of the Yellow Sea in summer and autumn of 2013[J]. Marine Science Bulletin, 2017,36(1):74-81.
[43] 唐永,孙语嫣,石晓勇,等.黄渤海海域秋季营养盐及有色溶解有机物分布特征[J]. 环境科学, 2017,38(11):4501-4512. Tang Y, Sun Y Y, Shi X Y, et al. Distribution Characteristics of Chromophoric Dissolved Organic Matter and Nutrients from the Yellow Sea and Bohai Sea in Autumn[J]. Environmental Science, 2017,38(11):4501-4512.
[44] Jin J, Liu S M, Ren J L, et al. Nutrient dynamics and coupling with phytoplankton species composition during the spring blooms in the Yellow Sea[J]. Deep Sea Research Part Ⅱ:Topical Studies in Oceanography, 2013,97:16-32.
[45] 王婷,石晓勇,张传松,等.2008年黄海浒苔绿潮爆发区营养盐浓度变化及分布特征[J]. 海洋通报, 2011,30(5):578-582. Wang T, Shi X Y, Zhang C S, et al. Variations in nutrient concentration and distribution for green tide of Enteromorpha prolifera occurrence areas of the Yellow Sea in 2008[J]. Marine Science Bulletin, 2011, 30(5):578-582.
[46] Fu M, Wang Z, Li Y, et al. Phytoplankton biomass size structure and its regulation in the Southern Yellow Sea (China):Seasonal variability[J]. Continental Shelf Research, 2009,29(18):2178-2194.
[47] Wang B D, Wang X L, Zhan R. Nutrient conditions in the Yellow Sea and the East China Sea[J]. Estuarine Coastal and Shelf Science, 2003,58(1):127-136.
[48] Li H M, Tang H J, Shi X Y, et al. Increased nutrient loads from the Changjiang (Yangtze) River have led to increased Harmful Algal Blooms[J]. Harmful Algae, 2014,39:92-101.
[49] 江蓓洁,鲍献文,吴德星,等.北黄海冷水团温、盐多年变化特征及影响因素[J]. 海洋学报, 2007,29(4):1-10. Jiang B J, Bao X W, Wu D X, et al. Interannual variation of temperature and salinity of northern Huanghai Sea Cold Water Mass and its probable cause[J]. Haiyang Xuebao, 2007,29(4):1-10.
[50] 张传松.长江口及邻近海域赤潮生消过程特征及其营养盐效应分析[D]. 山东:中国海洋大学, 2008. Zhang C S. The Characteristic and Effects of Nutrient during the Process of HAB in Changjiang River Estuary and its Adjacent Area[D]. Shandong:Ocean University of China, 2008.
[51] Zhang H B, Su R G, Shi X Y, et al. Role of nutrients in the development of floating green tides in the Southern Yellow Sea, China, in 2017[J]. Marine Pollution Bulletin, 2020,156:111197.
[52] Yang F X, Wei Q S, Chen H T, et al. Long-term variations and influence factors of nutrients in the western North Yellow Sea, China[J]. Marine Pollution Bulletin, 2018,135:1026-1034.
[53] 蒋昊,赵亮,张晶.黄海溶解无机氮及颗粒有机氮收支与转化模型[J]. 中国环境科学, 2020,40(9):3981-3991. Jiang H, Zhao L, Zhang J. Budgets and transformation of dissolved inorganic and particulate organic nitrogen in the Yellow Sea:A model study[J]. China Environmental Science, 2020,40(9):3981-3991.
[54] 韦钦胜,刘璐,战闰,等.夏季南黄海海水化学要素的分布特征及影响因素[J]. 中国海洋大学学报(自然科学版), 2010,40(1):82-88. Wei Q S, Liu L, Zhan R, et al. Distribution Features of the Chemical Parameters in the Southern Yellow Sea in Summer[J]. Journal of Ocean University of China, 2010,40(1):82-88.
[55] Flynn K J. Algal carbon-nitrogen metabolism:a biochemical basis for modelling the interactions between nitrate and ammonium uptake[J]. Journal of Plankton Research, 1991,(2):373-387.
[56] Hanisak M D. The Nitrogen Relationships of Marine Macroalgae[J]. Nitrogen in the Marine Environment, 1983:699-730.
[57] Maestrini S Y, Robert J M, Leftley J W, et al. Ammonium thresholds for simultaneous uptake of ammonium and nitrate by oyster-pond algae[J]. Journal of Experimental Marine Biology & Ecology, 1986, 102(1):75-98.
[58] 田千桃,霍元子,王阳阳,等.浒苔对NH₄⁺-N与NO₃^--N吸收的相互作用[J]. 海洋科学, 2010,(7):41-45. Tian Q T, Huo Y Z, Wang Y Y, et al. The interaction between NH₄⁺-N and NO₃^--N in nitrogen uptaking by Ulva prolifera[J]. Marine Sciences, 2010,(7):41-45.
[59] 何洁,刘瑀,张立勇,等.三种大型海藻吸收营养盐的动力学研究[J]. 渔业现代化, 2010,37(1):1-5. He J, Liu Y, Zhang L Y, et al. Study on the nutrient uptake kinetics of three kinds of macro_alga[J]. Fishery Modernization, 2010,37(1):1-5.
[60] 吴婷,田小亭,刘召辉,等.浒苔对不同氮源吸收特性的初步研究[J]. 海洋科学, 2011,35(4):51-54. Wu T, Tian X T, Liu Z H, et al. Absorption of different nitrogen species by Enteromorpha prolifera [J]. Marine Sciences, 2011,35(4):51-54.
[61] 李俭平.浒苔对氮营养盐的响应及其氮营养盐吸收动力学和生理生态研究[D]. 北京:中国科学院研究生院(海洋研究所), 2011. Li J P. The response to nitrogen nutrient, and the uptake kinetics mechanism of nitrogen and ecophysiaiagical analysis of Enteromorpha prolifera [D]. Beijing:University of Chinese Academy of Sciences, 2011.
[62] 海洋化学图集编委会.渤海黄海东海海洋图集——化学卷[M].北京:海洋出版社, 1991:99-103. Editorial board for the atlas of marine chemistry. Marine atlas of Bohai Sea Yellow Sea East Sea-Chemistry[M]. Beijing:China Ocean Press, 1991:99-103.
[63] 高生泉,林以安,金明明,等.春、秋季东、黄海营养盐的分布变化特征及营养结构[J]. 东海海洋, 2004,22(4):38-50. Gao S Q, Lin Y A, Jin M M, et al. Distribution features of nutrients and nutrient structure in the East China Sea and the Yellow Sea in spring and autumn[J]. Donghai Marine Science, 2004,22(4):38-50.
[64] 李瑞香,吴晓文,韦钦胜,等.不同营养盐条件下浒苔的生长[J]. 海洋科学进展, 2009,(2):211-216. Li R X, Wu X W, Wei Q S, et al. Growth of Enteromorpha Prolifera under different nutrient conditions[J]. Advances in Marine Science, 2009,(2):211-216.
[65] 李俭平,赵卫红,付敏,等.氮磷营养盐对浒苔生长影响的初步探讨[J]. 海洋科学, 2010,34(4):45-48. Li J P, Zhao W H, Fu M, et al. Preliminary study on the effects of nitrogen and phosphorus on the growth of Enteromorpha prolifera [J]. Marine Sciences, 2010,34(4):45-48.
[66] 国家海洋局.2009年中国海洋灾害公报[J]. 海洋开发与管理, 2010,(2):70. State Oceanic Administration (SOA). 2009 China marine disaster bulletin[J]. Ocean Development and Management, 2010,(2):70.
[67] 刘树勋,沈新强,王幼琴,等.渤、黄、东海水团多年月平均分布与变化的初步分析[J]. 海洋学报(中文版), 1993,15(4):1-11. Liu S X, Shen X Q, Wang Y Q, et al. Preliminary analysis on the monthly mean distribution and variation of water masses in the Bohai Sea, Yellow Sea and East China Sea over the years[J]. Haiyang Xuebao, 1993,15(4):1-11.
[68] 张启龙,翁学传,杨玉玲.南黄海春季水团分析[J]. 海洋与湖沼, 1996,(4):421-428. Zhang Q L, Weng X C, Yang Y L. Analysis of water masses in the South Yellow Sea in spring[J]. Oceanologia et Limnologia Sinica, 1996,(4):421-428.
[69] Nakao T. Oceanic Variability in Relation to Fisheries in the East China Sea and the Yellow Sea[J]. Journal of the Faculty of Marine Science and Technology, 1977,1:199-367.
[70] Zhong Y, Qiao L, Song D, et al. Impact of cold water mass on suspended sediment transport in the South Yellow Sea[J]. Marine Geology, 2020,106244:1-20.
[71] Wang B, Hirose N, Kang B, et al. Seasonal migration of the Yellow Sea Bottom Cold Water[J]. Journal of Geophysical Research:Oceans, 2014,119(7):4430-4443.
[72] Yuan D L, Hsueh Y. Dynamics of the cross-shelf circulation in the Yellow and East China Seas in winter[J]. Deep-Sea Research Part Ⅱ:Topical Studies in Oceanography, 2010,57(19/20):1745-1761.
[73] Tak Y J, Cho Y K, Seo G H, et al. Evolution of wind-driven flows in the Yellow Sea during winter[J]. Journal of Geophysical Research Oceans, 2016,121(3):1970-1983.
[74] Teague, G. A. Jacobs. Current observations on the development of the Yellow Sea Warm Current[J]. Journal of Geophysical Research:Oceans, 2000,105:3401-3411.
[75] Hsueh Y, Pang I C. Coastally Trapped Long Waves in the Yellow Sea[J]. Journal of Physical Oceanography, 1989,19(5):612-625.
[76] Hsueh Y. Recent current observations in the eastern Yellow Sea[J]. Journal of Geophysical Research:Oceans, 1988,93(C6):6875-6884.
[77] Park Y H. A simple theoretical model for the upwind flow in the southern Yellow Sea[J]. Oceanological Society Korea, 1986,21:203-210.
[78] Guo C C, Zhang G C, Sun J, et al. Seasonal responses of nutrient to hydrology and biology in the southern Yellow Sea[J]. Continental Shelf Research, 2020,206:104207.
[79] Wang F, Liu C Y, Meng Q J. Effect of the Yellow Sea warm current fronts on the westward shift of the Yellow Sea warm tongue in winter[J]. Continental Shelf Research, 2012,45:98-107.
[80] Mei X, Li R H, Zhang X H, et al. Evolution of the Yellow Sea Warm Current and the Yellow Sea Cold Water Mass since the Middle Pleistocene[J]. Palaeogeography Palaeoclimatology Palaeoecology, 2016,442:48-60.
[81] Ding Y, Bao X W, Yao Z G, et al. Effect of coastal-trapped waves on the synoptic variations of the Yellow Sea Warm Current during winter[J]. Continental Shelf Research, 2018,167:14-31.
[82] 邹娥梅,郭炳火,汤毓祥,等.1996年春季南黄海水文特征和水团分析[J]. 海洋学报(中文版), 2000,(1):17-26. Zou E M, Guo B H, Tang Y X, et al. The hydrographic features and water masses analyses of the southern Huanghai Sea in the spring of 1996[J]. Haiyang Xuebao, 2000,(1):17-26.
[83] 于非,张志欣,刁新源,等.黄海冷水团演变过程及其与邻近水团关系的分析[J]. 海洋学报(中文版), 2006,(5):26-34. Yu F, Zhang Z X, Diao X Y, et al. Analysis of evolution of the Huanghai Sea Cold Water Mass and its relationship with adjacent water masses[J]. Haiyang Xuebao, 2006,(5):26-34.
[84] 王辉武.黄海暖流季节和年际变化研究[D]. 山东:国家海洋局第一海洋研究所, 2008. Wang H W. Study on Seasonal and inter-annual variations of the Yellow Sea Warm Current[D]. Shandong:First Institute of Oceanography, State Oceanic Administration, 2008