Current conditions in summer in the Zhejiang offshore

LI Peng, WANG Si-jian, LI Yan-gang, QIN Wei-hua

Journal of Marine Sciences ›› 2014, Vol. 32 ›› Issue (3) : 16-25.

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Journal of Marine Sciences ›› 2014, Vol. 32 ›› Issue (3) : 16-25. DOI: 10.3969/j.issn.1001-909X.2014.03.003

Current conditions in summer in the Zhejiang offshore

  • LI Peng, WANG Si-jian, LI Yan-gang, QIN Wei-hua
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Abstract

To research the current character, variation and pattern in vertical profile, current speed and direction were observed using ADCP at 3 fixed sites along the Zhejiang offshore in summer of 2006 and 2009. The results showed that: (1) In central and north of Zhejiang offshore (A and B sites), the current was rotating flow and it rotated in clockwise direction. In the south area(C site), the flood tidal current was north,while it was north by east in ebb period. In vertical profile, the current direction was unanimous. (2) The vertical average speed was similar in the three observation sites (44.4~51.1 cm/s), but significant difference presented in average speed of vertical profile. The biggest speeds in the three sites were all bigger than 110 cm/s, which all occurred in the flood period in spring tide. (3) During observation period, the average residual flow speed at A, B and C site was 21.9, 12.3 and 22.3 cm/s, respectively. Influenced by the Yangtze diluted water, at A and B sites the residual current directions in the upper layers were southwest. From the middle to the bottom layers the residual currents were veering in counter clockwise direction with the southeast direction in lower layers, which may be caused by the Taiwan Warm Current traction. At C site residual current flow was more consistent in vertical, which was mainly affected by the northeast monsoon.(4)In summer, along the Zhejiang offshore from south to north, the current direction turned to east gradually at central area (between B and C site).(5)During the low water discharge of Yangtze, the south costal current existed in the central and north of Zhejiang offshore. The current adjacent to Zhejiang was controlling by monsoon, the Yangtze diluted water and the Taiwan Warm Current together, but the role of them varied significant spatially.

Key words

current / summer / spatial variability / Zhejiang offshore

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LI Peng, WANG Si-jian, LI Yan-gang, QIN Wei-hua. Current conditions in summer in the Zhejiang offshore[J]. Journal of Marine Sciences. 2014, 32(3): 16-25 https://doi.org/10.3969/j.issn.1001-909X.2014.03.003

References

[1] MILLIMAN J D, SHEN Huan-ting, YANG Zuo-sheng, et al. Transport and deposition of river sediment in the Changjiang Estuary and adjacent continental shelf[J].Continental Shelf Research,1985,4(1-2):37-45.
[2] YANG Shi-lun, BELKIN I M, BELKINA A I, et al. Delta response to decline in sediment supply from the Yangtze River: Evidence of the recent four decades and expectations for the next half-century[J]. Estuarine Coastal Shelf Science,2003,57:689-699.
[3] TANG Jun, SHEN Yong-ming, QIU Da-hong. Numerical simulation of longshore currents and pollutant movement in waves and currents in coastal zone[J]. Acta Oceanologica Sinica,2008,30(1):148-155.
唐军,沈永明,邱大洪.近岸沿岸流及污染物运动的数值模拟[J].海洋学报,2008,30(1):148-155.
[4] LIU J P, LI An-chun, XU K H, et al. Sedimentary features of the Yangtze River-derived along-shelf clinoform deposit in the East China Sea[J]. Continental Shelf Research,2006,26(17-18):2 141-2 156.
[5] LIU J P, XU K H, LI An-chun, et al. Flux and fate of Yangtze River sediment delivered to the East China Sea [J]. Geomorphology,2007,85:208-224.
[6] SU Ji-lan, PAN Yu-qiu. A primarily study of circulation dynamics of the continental shelf in the north of Taiwan in China Sea[J]. Acta Oceanologica Sinica,1989,11(1):1-14.
苏纪兰,潘玉球.台湾以北陆架环流动力学初步研究[J].海洋学报,1989,11(1):1-14.
[7] SU Ji-lan. A review of circulation dynamics of the coastal oceans near China [J]. Acta Oceanologica Sinica,2001,23(3):1-16.
苏纪兰.中国近海的环流动力机制研究[J].海洋学报,2001,23(3):1-16.
[8] GU Guo-chuan,HU Fang-xi,ZHANG Zheng-ti. The sediment sources and shaping mechanism of muddy coast in the east Zhejiang Province[J]. Donghai Marine Science,1997,15(3):1-12.
谷国传,胡方西,张正惕.浙东淤泥质海岸的泥沙来源和塑造机理[J].东海海洋,1997,15(3):1-12.
[9] ZHANG Cai-yun, SHANG Shao-ling, CHEN De-wen, et al. Short-term variability of the distribution of Zhe-Min Coastal Water and wind forcing during winter monsoon in the Taiwan Strait[J]. Journal of Remote Sensing,2005,9(4):452-458.
张彩云,商少凌,陈德文,等.冬季浙闽沿岸水分布的短期变动与风的关系初探[J].遥感学报,2005,9(4):452-458.
[10] LI Guang-xue, HAN Xin-bin, YUE Shu-hong, et al. Monthly variations of water masses in the East China Seas[J]. Continental Shelf Research,2006,26:1 954-1 970.
[11] XU Ke-hui, LI An-chun, LIU J P, et al. Provenance, structure, and formation of the mud wedge along inner continental shelf of the East China Sea: A synthesis of the Yangtze dispersal system [J]. Marine Geology,2012,291-294:176-191.
[12] XU Fang-jian, LI An-chun, HUANG Jing-li. Research progress in the mud deposits along the Zhe-Min coast of the East Sea continental shelf[J]. Marine Science Bulletin,2012,31(1):97-104.
徐方建,李安春,黄敬利.东海陆架浙闽沿岸泥质沉积研究进展[J].海洋通报,2012,31(1):97-104.
[13] LIU Bao-chao, LI Jian-ping, FENG Li-cheng. A modeling study of the effect of wind on Changjiang (Yangtze) River diluted water in summer[J]. Acta Oceanologica Sinic,2013,35(1):25-37.
刘宝超,李建平,冯立成.风影响夏季长江冲淡水扩展的数值模拟研究[J].海洋学报,2013,35(1):25-37.
[14] BEARDSLEY R C, LIMEBURNER R, YU Hong-hua, et al. Discharge of the Changjiang(Yangtze River) into the East China Sea[J]. Continental Shelf Research,1985,4(1-2):57-76.
[15] ZHU Jian-rong, DING Ping-xing, HU Dun-xin. Observation of the diluted water and plume from the Changjiang River estuary during August 2000[J]. Oceanologia et Limnologia Sinica,2003,34(3):249-255.
朱建荣,丁平兴,胡敦欣.2000年8月长江口外海区冲淡水和羽状锋的观测[J].海洋与湖沼,2003,34(3):249-255.
[16] ZHOU Feng, XUAN Ji-liang, NI Xiao-bo, et al. A preliminary study on variations of the Changjiang Diluted Water between August 1999 and 2006[J]. Acta Oceanologica Sinica,2009,31(4):1-12.
周锋,宣基亮,倪晓波,等.1999年与2006年间夏季长江冲淡水变化动力因素的初步分析[J].海洋学报,2009,31(4):1-12.
[17] BAO Xian-wen, GAO Guo-ping, YAN Ju. Three dimensional simulation of tide and tidal current characteristics in the East China Sea[J]. Oceanologica Acta,2001,24(2):135-149.
[18] WEI Ze-xun. Numerical simulation of the China adjacent sea circulation and its seasonal variation[D]. Qingdao: Institute of Oceanology, Chinese Academy of Sciences,2004:151.
魏泽勋.中国近海环流及其季节变化的数值模拟[D].青岛:中国科学研究院海洋研究所,2004:151.
[19] CHEN Qian, HUANG Da-ji, ZHANG Ben-zhao, et al. Characteristics of the tidal current and residual current in the seas adjacent to Zhejiang[J]. Donghai Marine Sciences,2003,21(4):1-14.
陈倩,黄大吉,章本照,等.浙江近海潮流和余流的特征[J].东海海洋,2003,21(4):1-14.
[20] ZENG Ding-yong, NI Xiao-bo, HUANG Da-ji. Temporal and spatial variability of the Zhe-Min Coastal Current and the Taiwan Warm Current in winter in the southern Zhejiang coastal sea (in Chinese)[J]. Sci Sin Terrae,2012,42(7):1 123-1 134.
曾定勇,倪晓波,黄大吉.冬季浙闽沿岸流与台湾暖流在浙南海域的时空变化[J].中国科学:地球科学,2012,42(7):1 123-1 134.
[21] ZHAO Bao-ren. Mechanism of expansion trend of the Yangtze diluted water[J]. Acta Oceanologica Sinica,1991,13(5):600-610.
赵保仁.长江冲淡水的转向机制问题[J].海洋学报,1991,13(5):600-610.
[22] PU Yong-xiu, SU Yu-fen, XU Xiao-yun. Characteristics of currents in the southern east China sea[C]∥Thesis of Kuroshio investigation. Beijing: Ocean Press,1987:33-44.
浦泳修,苏玉芬,许小云.东海南部流场的若干特征[C]∥黑潮调查研究论文集.北京:海洋出版社,1987:33-44.
[23] GUAN Bing-xian. A sketch of the current structures and eddy characteristics in the East China Sea[J]. Studia Marina Sinica,1986,27:1-23.
管秉贤.东海海流结构及涡旋特征概述[J].海洋科学集刊,1986,27:1-23.
[24] GUAN Bing-xian. A summary of current system in the East China sea[C]∥Thesis of continental shelf in East China. Qingdao: Institute of Oceanology, Chinese Academy of Sciences,1978:126-183.
管秉贤.东海海流系统概述[C]∥东海大陆架论文集.青岛:中国科学研究院海洋研究所,1978:126-183.
[25] CHEN Ji-yu, WANG Bao-can, YU Zhi-ying. Development and evolution of China's coast[M]. Shanghai: Shanghai Scientific and Technical Publishers,1989:393-402.
陈吉余,王宝灿,虞志英.中国海岸发育过程和演变规律[M].上海:上海科学技术出版社,1989:393-402.
[26] BAI Xue-zhi, WANG Fan, HU Dun-xin. Numerical simulation of the seasonal circulation in the Huanghai sea and East China sea[J]. Studia Marina Sinica,2003,45:77-85.
白学志,王凡,胡敦欣.东中国海环流及其季节变化的数值模拟[J].海洋科学集刊,2003,45:77-85.
[27] LE Ken-tang. A preliminary study of the path of the Yangtze diluted water[J]. Oceanologia et Limnologia Sinica,1984,15(2):157-167.
乐肯堂.长江冲淡水路径问题的初步研究[J].海洋与湖沼,1984,15(2):157-167.
[28] ZHAN Peng, CHEN Xue-en,HU Xue-jun, et al. Analysis of the summertime current observations outside of the Yangtze Estuary in Donghai[J]. Periodical of Ocean University of China,2010,40(8):34-42.
展鹏,陈学恩,胡学军,等. 夏季长江口外东海海域实测海流资料分析[J]. 中国海洋大学学报,2010,40(8):34-42.
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