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科学通报  2011 

2008与2010年黄海浒苔漂移输运特征对比

, PP. 1470-1476

Keywords: 黄海,浒苔,漂移路径,模拟,预测

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Abstract:

利用中国近海三维海浪-潮流-环流耦合数值模式,分别对2008年6~7月(青岛奥帆赛前期)和2010年6~7月黄海浒苔的漂移开展了模拟和预测,研究了黄海漂浮浒苔在青岛聚集的动力学成因.揭示了2008年6月浒苔之所以在青岛近岸大量聚集,是因为该海区月平均表层流向向岸且与岸线几乎垂直;相比之下,2008年7月上旬表层流场与岸线大致平行,因而海上浒苔的漂移对奥帆赛场的压力明显减缓.利用数值模式预测2010年6月下旬浒苔主体不会在青岛登陆,该预测与其后的观测事实相吻合.研究发现,风场驱动下的海洋表层流场年际变化是浒苔漂移路径变异的主要原因,提出区域气候变化是影响海洋生态系统的一种途径.

References

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[3]  Hu C M, He M X. Origin and offshore extent of floating algae in Olympic sailing area. Eos Trans AGU, 2008, 89: 302–303
[4]  Hu C M. A novel ocean color index to detect floating algae in the global oceans. Remote Sens Environ, 2009, 113: 2118–2129
[5]  Qiao F L, Dai D J, Simpson J, et al. Banded structure of drifting macroalgae. Mar Pollut Bull, 2009, 58: 1792–1795
[6]  Langmuir I. Surface motion of water induced by wind. Science, 1938, 87: 119–123
[7]  Thorpe S A. Spreading of floating particles by Langmuir circulation. Mar Pollut Bull, 2009, 58: 1787–1791
[8]  Hu C M, Li D Q, Chen C S, et al. On the recurrent Ulva prolifera blooms in the Yellow Sea and East China Sea. J Geophys Res, 2010, 115: C05017
[9]  Wang X H, Qiao F L, Lu J, et al. The turbidity maxima of the northern Jiangsu Shoal-water in the Yellow Sea, China. Estuar Coast Shelf Sci, 2010, doi: 10.1016/j.ecss.2010.10.020
[10]  Lü X G, Qiao F L, Xia C S, et al. Upwelling and surface cold patches in the Yellow Sea in summer: Effects of tidal mixing on the vertical circulation. Cont Shelf Res, 2010, 30: 620–632
[11]  Wang X H, Li L, Bao X, et al. Economic cost of an algae bloom cleanup in China’s 2008 Olympic Sailing Venue. Eos Amer Geophys Union Trans, 2009, 90: 238–239
[12]  Lü X G, Qiao F L. Distribution of sunken macroalgae against the background of tidal circulation in the coastal waters of Qingdao, China, in summer 2008[J].Geophys Res Lett.2008, 35:23614-
[13]  Blumberg A F, Mellor G L. A description of a three-dimensional coastal ocean circulation model. In: Heaps N S, ed. Three Dimensional Coastal Ocean Models, Vol 4. Washington D C: American Geophysical Union, 2010. 1–16
[14]  Xia C S, Qiao F L, Zhang Q H, et al. Numerical modeling of the quasi-global ocean circulation based on POM. J Hydrodyn Ser B, 2004, 16: 537–543
[15]  Yuan Y L, Pan Z D, Hua F, et al. LAGFD-WAM numerical wave model-I . Basic physical model. Acta Oceanol Sin, 1991, 10: 483–488
[16]  杨永增, 乔方利, 赵伟, 等. 球坐标系下MASNUM 海浪数值模式的建立及其应用. 海洋学报, 2005, 27: 1–7
[17]  Xia C S, Qiao F L, Yang Y Z, et al. Three-dimensional structure of the summertime circulation in the Yellow Sea from a wave-tide-circulation coupled model. J Geophys Res, 2006, 111: C11S03
[18]  Wang G S, Qiao F L, Xia C S. Parallelization of a coupled wave-circulation model and its application. Ocean Dyn, 2010, 60: 331–339
[19]  Qiao F L, Yuan Y L, Yang Y Z, et al. Wave-induced mixing in the upper ocean: Distribution and application in a global ocean circulation model. Geophys Res Lett, 2004, 31: L11303
[20]  Grell G A, Dudhia J, Stauffed D R. A description of the fifth-generation Penn State/NCAR mesoscale model (MM5). NCAR Technical Note, 1995
[21]  凌铁军, 张蕴斐, 杨学联, 等. 中尺度数值预报模式(MM5)在海面风场预报中的应用. 海洋预报, 2004, 21: 1–9
[22]  李尧. 中国东部近海夏季环流特征及其动力机制. 博士学位论文. 青岛: 中国科学院海洋研究所, 2010. 1–114
[23]  郭炳火, 许建平. 中国近海环流. 见: 苏纪兰, 袁业立, 编. 中国近海水文. 北京: 海洋出版社, 2005. 174–181
[24]  刘志亮, 胡敦欣. 黄海夏季近岸海区环流的初步分析及其与风速的关系. 海洋学报, 2009, 31: 1–7
[25]  吕新刚. 黄东海上升流机制数值研究. 博士学位论文. 青岛: 中国科学院海洋研究所, 2010. 1–147

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