A method for estimating boundary exchanges in the East China Sea based on satellite drifter trajectories
WU Ze-zhou1,2,ZHOU Feng*1,2,3
Author information+
1. State Key Laboratory of Satellite Ocean Environment Dynamics, Hangzhou 310012,China; 2. Second Institute of Oceanography, SOA, Hangzhou 310012,China; 3. Ocean College, Zhejiang University, Zhoushan 316021, China
The shelf slope and the Taiwan Strait are two main boundaries of the East China Sea, which obtain considerable heat and salinity as well as nutrients from the northwestern Pacific and the South China Sea. In this paper, based on the satellite drifter trajectories, a reliable method is established for estimating the cross-boundary exchanges by mapping the irregularly-distributed trajectories to the regular homogeneous grid. With this method, the calculated density of trajectories reveals the location of the Kuroshio main axis, and further indicates significant cross-slope exchanges. The statistical results reveal the remarkable region feature of water exchanges along the shelf slope of the East China Sea, showing seven dynamic exchange zones, i.e., three inflow (shoreward) zones and four outflow (offshore) zones. The study also shows that the cross-slope exchange has prominent seasonality. The most significant exchange and the most distinctive inflow occurs in autumn while the weakest in spring. The exchange through the Taiwan Strait is mainly northward and the most intense exchange occurs in the eastern side of the strait. The exchange through the Taiwan Strait reaches the strongest in summer but the weakest in spring and in winter.
WU Ze-zhou,ZHOU Feng.
A method for estimating boundary exchanges in the East China Sea based on satellite drifter trajectories[J]. Journal of Marine Sciences. 2018, 36(1): 27-34 https://doi.org/10.3969/j.issn.1001-909X.2018.01.003
中图分类号:
P731
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参考文献
[1] ZHOU Feng, XUE Hui-jie, HUANG Da-ji, et al. Cross-shelf exchange in the shelf of the East China Sea[J]. Journal of Geophysical Research: Oceans, 2015,120(3):1 545-1 572. [2] DING Rui-bing, HUANG Da-ji, XUAN Ji-liang, et al. Cross-shelf water exchange in the East China Sea as estimated by satellite altimetry and in situ hydrographic measurement[J]. Journal of Geophysical Research: Oceans, 2016,121(9):7 192-7 211. [3] CHEN Chen-tung, WANG Shu-lun. Carbon, alkalinity and nutrient budgets on the East China Sea continental shelf[J]. Journal of Geophysical Research: Oceans, 1999,104(C9):20 675-20 686. [4] ZHANG Jing, LIU Su-mei, REN Jing-ling, et al. Nutrient gradients from the eutrophic Changjiang (Yangtze River) Estuary to the oligotrophic Kuroshio waters and re-evaluation of budgets for the East China Sea Shelf[J]. Progress in Oceanography, 2007,74(4):449-478. [5] CHUANG W. A note on the driving mechanisms of current in the Taiwan Strait[J]. Journal of Oceanography, 1986,42(5):355-361. [6] TEAGUE W J, JACOBS G A, KO D S, et al. Connectivity of the Taiwan, Cheju, and Korea straits[J]. Continental Shelf Research, 2003,23(1):63-77. [7] NITANI H. Beginning of the Kuroshio[M]//STOMMEL H, YOSHIDA K. Kuroshio: Its physical aspects.Tokyo: University of Tokyo Press, 1972: 129-163 [8] GUO Xin-yu, MIYAZAWA Y, YAMAGATA T. The Kuroshio Onshore Intrusion along the Shelf Break of the East China Sea: The origin of the Tsushima Warm Current[J]. Journal of Physical Oceanography, 2006,36(12):2 205-2 231. [9] ISOBE A. Recent advances in ocean-circulation research on the Yellow Sea and East China Sea shelves[J]. Journal of Oceanography, 2008,64(4):569-584. [10] SONG Jun, XUE Hui-jie, BAO Xian-wen, et al. A spectral mixture model analysis of the Kuroshio variability and the water exchange between the Kuroshio and the East China Sea[J]. Chinese Journal of Oceanology and Limnology, 2011,29(2):446-459. [11] VELEZ-BELCHI P, CENTURIONI L R, LEE D, et al. Eddy induced Kuroshio intrusions onto the continental shelf of the East China Sea[J]. Journal of Marine Research, 2013,71(1-2):83-107. [12] LIU Xiao-hui, DONG Chang-ming, CHEN Da-ke, et al. The pattern and variability of winter Kuroshio intrusion northeast of Taiwan[J]. Journal of Geophysical Research: Oceans, 2014,119(8):5 380-5 394. [13] UCHIDA H, IMAWAKI S. Eulerian mean surface velocity field derived by combining drifter and satellite altimeter data[J]. Geophysical Research Letters, 2003,30(5):doi:10.1029/2002GL016445. [14] YU Long, XIONG Xue-jun, GUO Yan-liang, et al. Analysis of the path and axis features of the Kuroshio at the depth of 15 m based on drifting buoy data[J].Advances in Marine Science, 2014,32(3):316-323. 于龙, 熊学军, 郭延良, 等. 根据漂流浮标资料对黑潮15m层流路及流轴特征的分析[J]. 海洋科学进展, 2014,32(3):316-323. [15] LIE H J, CHO C H, LEE J H, et al. Separation of the Kuroshio water and its penetration onto the continental shelf west of Kyushu[J]. Journal of Geophysical Research: Oceans, 1998,103(C2):2 963-2 976. [16] YU Fei, ZANG Jia-ye, GUO Bing-huo, et al. Some phenomena of the Kuroshio intrusion into shelf area and the shelf circulation of the East China Sea[J]. Advances in Marine Science,2002,20(3):21-28. 于非, 臧家业, 郭炳火, 等. 黑潮水入侵东海陆架及陆架环流的若干现象[J]. 海洋科学进展, 2002,20(3):21-28. [17] HU Xiao-min, XIONG Xue-jun, QIAO Fang-li, et al. Surface current field and seasonal variability in the Kuroshio and adjacent regions derived from satellite-tracked drifter data[J]. Acta Oceanologica Sinica, 2008,30(6):1-16. 胡筱敏, 熊学军, 乔方利, 等. 利用漂流浮标资料对黑潮及其邻近海域表层流场及其季节分布特征的分析研究[J]. 海洋学报, 2008, 30(6):1-16. [18] LIU Z, GAN J. Variability of the Kuroshio in the East China Sea derived from satellite altimetry data[J]. Deep Sea Research Part I: Oceanographic Research Papers, 2012,59(3):25-36. [19] LIN Kui, TANG Yu-xiang, GUO Bing-huo. An analysis on observational surface and upper layer current in the Huanghai Sea and the East China Sea[J]. Acta Oceanologica Sinica, 2002,24(2):9-19. 林葵, 汤毓祥, 郭炳火. 黄海、东海表、上层实测流分析[J]. 海洋学报, 2002,24(2):9-19. [20] ZHAO Rui-xiang, LIU Zhi-liang. The seasonal variability of the Kuroshio surface water intrusion onto the East China Sea continental shelf derived from Argos drifter data[J]. Acta Oceanologica Sinica, 2014,36(1):20-27. 赵瑞祥, 刘志亮. 台湾东北部黑潮次表层水入侵的季节变化规律[J]. 海洋学报, 2014,36(1):20-27. [21] HANSEN D V, POULAIN P M. Quality control and interpolations of WOCE-TOGA drifter data[J]. Journal of Atmospheric and Oceanic Technology, 1996,13(4):900-909. [22] GUO Bing-huo, LIE H J, LEE J H. Interaction of Kuroshio water and shelf water in the Tsushima Current region in summer[J]. Acta Oceanologica Sinica, 1998,20(5):1-12. 郭炳火, 李兴宰, 李载学. 夏季对马暖流区黑潮水与陆架水的相互作用──兼论对马暖流的起源[J]. 海洋学报, 1998,20(5):1-12. [23] SU Ji-lan. A review of circulation dynamics of the coastal oceans near China[J]. Acta Oceanologica Sinica, 2001,23(4):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(4):1-16. [24] LEE J, MATSUNO T. Intrusion of Kuroshio water onto the continental shelf of the East China Sea[J]. Journal of Oceanography, 2007,63(2):309-325. [25] GUO B, HU X, XIONG X, et al. Study on interaction between the coastal water, shelf water and Kuroshio water in the Huanghai Sea and East China Sea[J]. Acta Oceanologica Sinica, 2003,22(3):351-367. [26] CHANG P H, ISOBE A. A numerical study on the Changjiang diluted water in the Yellow and East China Sea[J]. Journal of Geophysical Research Atmospheres, 2003,108(C9):11-15. [27] LIE H J, CHO C H, LEE J H, et al. Structure and eastward extension of the Changjiang River plume in the East China Sea[J]. Journal of Geophysical Research Oceans, 2003,108(C3):209.