| 2012年南海西北陆架冬季水文特征的观测分析 |
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| 引用本文： | 郑曼立,李明明,谢玲玲,洪颖彬,何云开,宗晓龙.2012年南海西北陆架冬季水文特征的观测分析[J].海洋与湖沼,2018,49(4):734-745. |
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| 作者姓名： | 郑曼立 李明明 谢玲玲 洪颖彬 何云开 宗晓龙 |
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| 作者单位： | 广东海洋大学海洋与气象学院广东省近海海洋变化与灾害预警重点实验室 湛江 524088,广东海洋大学海洋与气象学院广东省近海海洋变化与灾害预警重点实验室 湛江 524088,广东海洋大学海洋与气象学院广东省近海海洋变化与灾害预警重点实验室 湛江 524088,国家海洋局南海分局 湛江环境监测站 湛江 524074,中国科学院南海海洋研究所热带海洋环境国家重点实验室 广州 510301,中国海洋大学物理海洋教育部重点实验室 青岛 266100 |
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| 基金项目： | 国家自然科学基金项目，41776034号，41476009号；广东省高等学校优秀青年教师项目，YQ2015088号；广东海洋大学创新强校项目，GDOU2016050240号。 |
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| 摘 要： | 本文基于2012年12月南海西北部陆架海区的温盐和流速实测资料，分析了粤西和琼东陆架海区冬季三维温、盐结构和流场特征，给出沿陆架和跨陆架方向的水体和热盐通量。结果表明：（1）在50m以浅，粤西和琼东海区温度均由近岸向外海递增，深层则相反；冬季近岸海区混合层较深，外海密度跃层位于60—120m深度且层结较强，浮力频率大于10–2/s；（2）海流大致沿等深线向西南流动，30m以深流速大小在0.03—0.40m/s之间，且随着深度增加而略有减小；琼东海区100m等深线附近在60m以浅水层观测到水体辐聚并有明显温度锋面存在；（3）沿陆架方向的水体和热盐输送均大于跨陆架方向，其中粤西单位面积沿/跨陆架水体通量平均值为0.13×10–6/0.03×10–6Sv/m2，低于琼东海区的0.91×10–6/0.56×10–6Sv/m2。
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| 关 键 词： | 南海 水文特征 流速分布 跨陆架输送 锋面 |
| 收稿时间： | 2017/10/23 0:00:00 |
| 修稿时间： | 2018/3/30 0:00:00 |
OBSERVATION OF HYDROGRAPHIC CHARACTERISTICS OF NORTHWESTERN SHELF OF THE SOUTH CHINA SEA IN WINTER 2012 |
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| ZHENG Man-Li,LI Ming-Ming,XIE Ling-Ling,HONG Ying-Bin,HE Yun-Kai and ZONG Xiao-Long.OBSERVATION OF HYDROGRAPHIC CHARACTERISTICS OF NORTHWESTERN SHELF OF THE SOUTH CHINA SEA IN WINTER 2012[J].Oceanologia Et Limnologia Sinica,2018,49(4):734-745. |
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| Authors: | ZHENG Man-Li LI Ming-Ming XIE Ling-Ling HONG Ying-Bin HE Yun-Kai and ZONG Xiao-Long |
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| Institution: | College of Ocean and Meteorology, Guangdong Ocean University, Guangdong Key Laboratory of Coastal Ocean Variation and Disaster Prediction, Zhanjiang 524088, China,College of Ocean and Meteorology, Guangdong Ocean University, Guangdong Key Laboratory of Coastal Ocean Variation and Disaster Prediction, Zhanjiang 524088, China,College of Ocean and Meteorology, Guangdong Ocean University, Guangdong Key Laboratory of Coastal Ocean Variation and Disaster Prediction, Zhanjiang 524088, China,Zhanjiang Environmental Monitor Station, South Chian Sea Branch, State Oceanic Administration, Zhanjiang 524074, China,South China Sea Institute of Oceanology, Chinese Academy of Sciences, State Key Laboratory of Tropical Oceanography, Guangzhou 510301, China and OceanUniversity of China, Physical Oceanography Laboratory, Qingdao 266100, China |
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| Abstract: | In-situ conductivity-temperature-depth (CTD) and Acoustic Doppler Current Profiler (ADCP) observations were conducted on the northwestern continental shelf of the South China Sea in December 2012. The 3-D structures of hydrographic and current properties, and alongshore and cross-shelf transports in the west Guangdong (WG) and east Hainan (EH) in winter were analyzed. The results show that the seawater temperature increased in the offshore direction in the upper layer above 50 m but decreased in deeper layers. The waters inshore were well mixed to bottom near WG coast, and the pycnocline deepened to 60-120m with stratification larger than 10-2/s in deep water offshore. The currents flowed generally southwestward along the isobaths in the magnitudes of 0.03-0.40m/s. The velocities decreased generally with depth. In the EH area, the currents above 60m converged along the 100-m isobath and formed a thermal front. The alongshore transports of water mass, heat, and salinity were larger than those of the cross-shelf. The average alongshore and cross-shelf fluxes in the WG area were 0.13×10-6 and 0.03×10-6Sv/m2, respectively, lower than those of the EH area for 0.91×10-6 and 0.56×10-6Sv/m2. |
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| Keywords: | South China Sea hydrographic characteristics current cross-shelf transport front |
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