| 沙埕港湾口断面潮流及余流特征分析 |
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| 引用本文： | 万 凯,鲍献文,姚志刚,万修全,夏颖颖.沙埕港湾口断面潮流及余流特征分析[J].海洋与湖沼,2014,45(4):669-675. |
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| 作者姓名： | 万 凯 鲍献文 姚志刚 万修全 夏颖颖 |
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| 作者单位： | 中国海洋大学海洋环境学院,中国海洋大学海洋环境学院;中国海洋大学物理海洋教育部重点实验室,中国海洋大学海洋环境学院；中国海洋大学物理海洋教育部重点实验室,中国海洋大学海洋环境学院；中国海洋大学物理海洋教育部重点实验室,中国海洋大学海洋环境学院 |
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| 基金项目： | 福建主要海湾海洋环境与数模研究，国家自然科学基金项目（41006004、41276013、41206013) ，高等学校博士学科点专项科研基金 （2011013213000）,国家海洋局青年科学基金重点项目(2012202). |
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| 摘 要： | 基于对沙埕港湾口断面的连续走航观测资料,成功构建了沿走航断面的10个站点的连续海流序列,并分析了潮流、余流、潮通量等水文要素。分析结果表明,沙埕港湾口水道潮流类型为正规半日潮流,涨潮最先出现在中下层而落潮最先出现在上层,涨(落)潮转流相差约为30min。水道内潮流为往复流,M2和S2分潮流流速较大,倾角基本沿水道主轴方向。沙埕港湾口断面余流呈2层结构,10m以浅基本为东南向余流流出湾口,核心位于湾口断面南侧。10m以深多为西北向流入湾内,入流核心位于湾口断面中部的底层区域。对潮通量的计算表明,通过湾口进入沙埕港的潮通量约为1.63×108m3。
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| 关 键 词： | 潮流 余流 纳潮量 走航ADCP |
| 收稿时间： | 2013/3/15 0:00:00 |
| 修稿时间： | 2013/11/28 0:00:00 |
TIDAL AND RESIDUAL CURRENT CHARACTERISTICS AT MOUTH OF SHANGCHENGGANG CHANNEL |
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| WAN Kai,BAO Xian-Wen,YAO Zhi-Gang,WAN Xiu-Quan and XIA Ying-Ying.TIDAL AND RESIDUAL CURRENT CHARACTERISTICS AT MOUTH OF SHANGCHENGGANG CHANNEL[J].Oceanologia Et Limnologia Sinica,2014,45(4):669-675. |
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| Authors: | WAN Kai BAO Xian-Wen YAO Zhi-Gang WAN Xiu-Quan and XIA Ying-Ying |
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| Institution: | College of Physical and Environmental Oceanography, Ocean University of China,College of Physical and Environmental Oceanography, Ocean University of China;Physical Oceanography Laboratory , Ocean University of China,College of Physical and Environmental Oceanography, Ocean University of China;Physical Oceanography Laboratory , Ocean University of China,College of Physical and Environmental Oceanography, Ocean University of China;Physical Oceanography Laboratory , Ocean University of China,College of Physical and Environmental Oceanography, Ocean University of China |
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| Abstract: | Based on shipboard ADCP measurements at the mouth of Shachenggang Channel, time series of tidal current at 10 sites along the transection are constructed. The hydrological factors such as tidal current, residual current and tidal transport are analyzed to increase our understanding of tidal and residual current characteristics in this region. The tidal currents are identified as regular semidiurnal tidal flows. Tidal flood currents first appear in lower layers about 30 minutes ahead to upper layers currents in flood phase , while ebb currents first show up in upper layers about 30 minutes ahead in ebb phase. The tidal currents in the channel are alternating currents, in which M2 and S2 constituents have relatively stronger speed and mainly flow along the principal axis of Shachenggang Channel. A two-layer structure is found for residual currents of the transection, with southeastward outflows centered at the south section in the upper 10m and northwestward inflows centered at the middle section blow the 10m depth, The approximate tidal transports between the Shachenggang Channel and outer sea through the transection are 1.63 x108 m3. |
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| Keywords: | tidal currents residual current tidal transport shipboard ADCP |
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