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高频地波雷达观测的苏北辐射沙洲南部海域夏季表层海流特征

杨华 吉会峰 高清清 张春琳 杨波 马润美 丁言者

杨华, 吉会峰, 高清清, 张春琳, 杨波, 马润美, 丁言者. 高频地波雷达观测的苏北辐射沙洲南部海域夏季表层海流特征[J]. 海洋学报, 2019, 41(5): 1-11. doi: 10.3969/j.issn.0253-4193.2019.05.001
引用本文: 杨华, 吉会峰, 高清清, 张春琳, 杨波, 马润美, 丁言者. 高频地波雷达观测的苏北辐射沙洲南部海域夏季表层海流特征[J]. 海洋学报, 2019, 41(5): 1-11. doi: 10.3969/j.issn.0253-4193.2019.05.001
Yang Hua, Ji Huifeng, Gao Qingqing, Zhang Chunlin, Yang Bo, Ma Runmei, Ding Yanzhe. Summertime surface current characteristics in the southern region of Subei radial sand ridges detected by HF surface wave radar[J]. Haiyang Xuebao, 2019, 41(5): 1-11. doi: 10.3969/j.issn.0253-4193.2019.05.001
Citation: Yang Hua, Ji Huifeng, Gao Qingqing, Zhang Chunlin, Yang Bo, Ma Runmei, Ding Yanzhe. Summertime surface current characteristics in the southern region of Subei radial sand ridges detected by HF surface wave radar[J]. Haiyang Xuebao, 2019, 41(5): 1-11. doi: 10.3969/j.issn.0253-4193.2019.05.001

高频地波雷达观测的苏北辐射沙洲南部海域夏季表层海流特征

doi: 10.3969/j.issn.0253-4193.2019.05.001
基金项目: 国家海洋局东海分局青年科技基金(201624)。

Summertime surface current characteristics in the southern region of Subei radial sand ridges detected by HF surface wave radar

  • 摘要: 本文利用高频地波雷达获得的江苏如东海域大范围长期海流观测资料对苏北辐射沙洲南部烂沙洋海域夏季表层海流特征进行了分析。分析结果表明:研究海域表层海流靠近近岸一侧为往复流,流向总体上呈西北-东南向,靠近外海一侧为旋转流;海域潮流动力较为强劲,夏季表层海流实测最大流速达1.47 m/s,涨潮平均流速介于0.44~0.55 m/s,落潮平均流速介于0.38~0.52 m/s,海域西北部区域涨落潮平均流速明显大于其他区域;表层潮流为正规半日潮流,M2分潮为最主要分潮,其潮流椭圆长轴范围为0.57~0.71 m/s,远大于其他分潮,其次为S2分潮;该海域夏季表层余流呈现近岸大离岸小的分布趋势,余流流向基本指向近岸方向,从离岸到近岸余流流向呈现逆时针偏转。
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