南海北部湾表层悬浮体分布规律

李珏, 乔璐璐, LeDucCuong, 薛文静, 杨宏达, 王勇智, 姚志刚. 南海北部湾表层悬浮体分布规律[J]. 海洋地质与第四纪地质, 2020, 40(2): 10-18. doi: 10.16562/j.cnki.0256-1492.2019021301
引用本文: 李珏, 乔璐璐, LeDucCuong, 薛文静, 杨宏达, 王勇智, 姚志刚. 南海北部湾表层悬浮体分布规律[J]. 海洋地质与第四纪地质, 2020, 40(2): 10-18. doi: 10.16562/j.cnki.0256-1492.2019021301
LI Jue, QIAO Lulu, LE DucCuong, XUE Wenjing, YANG Hongda, WANG Yongzhi, YAO Zhigang. Surficial distribution of suspended sediment in Beibu Gulf of the South China Sea[J]. Marine Geology & Quaternary Geology, 2020, 40(2): 10-18. doi: 10.16562/j.cnki.0256-1492.2019021301
Citation: LI Jue, QIAO Lulu, LE DucCuong, XUE Wenjing, YANG Hongda, WANG Yongzhi, YAO Zhigang. Surficial distribution of suspended sediment in Beibu Gulf of the South China Sea[J]. Marine Geology & Quaternary Geology, 2020, 40(2): 10-18. doi: 10.16562/j.cnki.0256-1492.2019021301

南海北部湾表层悬浮体分布规律

  • 基金项目: 国家自然科学基金“浙闽沿岸泥质带冬季悬浮体的沉积机制”(41476030),“黄海暖流的沉积动力机制研究”(40906025);中国东盟海上合作基金“长江三角洲与红河三角洲全新世沉积演化对比研究”;泰山学者建设工程专项项目;国家重点研发计划“大型水库调控下河口沉积动力过程及其生物地球化学效应”(2016YFA060093)
详细信息
    作者简介: 李珏(1997—),女,硕士研究生,主要从事沉积动力学研究,E-mail:lijue1019@163.com
  • 中图分类号: P736.21

Surficial distribution of suspended sediment in Beibu Gulf of the South China Sea

  • 受实测数据海域位置的限制,目前基于遥感手段对北部湾表层悬浮体的研究,在部分海域如海湾西部精度不高,且缺乏对悬浮体浓度(suspended sediment concentration,SSC)季节变化的研究。基于2003—2017年MODIS-Aqua卫星L1B数据,结合海南岛西部、广西沿岸和越南沿岸实测数据,建立表层SSC的反演模型,获得北部湾海域2003—2017年月均表层SSC分布,并对其影响因素进行初步探讨。结果显示:北部湾表层SSC存在3个终年高值区,包括广西沿岸、海南岛西侧和红河三角洲沿岸;受河流输沙和海洋动力季节变化影响,SSC表现为冬季和夏季较高、春季最低的季节变化特征;热带气旋过境导致北部湾海域SSC增高,其中热带风暴“贝碧嘉”过境时位于路径右侧的雷州半岛西部SSC较多年平均值增幅达75%。

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  • 图 1  北部湾区域图

    Figure 1. 

    图 2  北部湾实测表层SSC与遥感反演结果对比图

    Figure 2. 

    图 3  北部湾2003—2017年年均表层悬浮体分布

    Figure 3. 

    图 4  北部湾2003—2017年多年平均各月SSC分布图

    Figure 4. 

    图 5  北部湾主要断面表层SSC(a,b,c,d)及北部湾区域平均风场(e)随时间变化

    Figure 5. 

    图 6  2013年6月北部湾表层悬浮体分布(a)及其与多年平均6月的差值(b)

    Figure 6. 

    图 7  2009年各月15日Balat河口含沙量及a点处多年月平均SSC分布

    Figure 7. 

    图 8  昌化江下游水体多年月平均含沙量[25]及b站处多年月平均SSC分布

    Figure 8. 

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出版历程
收稿日期:  2019-02-13
修回日期:  2019-08-28
刊出日期:  2020-04-25

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