调水调沙期间黄河口羽状流的逐时变化

于永贵, 石学法, 迟万清, 胡子峰, 乔淑卿. 调水调沙期间黄河口羽状流的逐时变化[J]. 海洋地质与第四纪地质, 2018, 38(5): 41-51. doi: 10.16562/j.cnki.0256-1492.2018.05.004
引用本文: 于永贵, 石学法, 迟万清, 胡子峰, 乔淑卿. 调水调沙期间黄河口羽状流的逐时变化[J]. 海洋地质与第四纪地质, 2018, 38(5): 41-51. doi: 10.16562/j.cnki.0256-1492.2018.05.004
YU Yonggui, SHI Xuefa, CHI Wanqing, HU Zifeng, QIAO Shuqing. Hourly change in sediment plume at the Yellow River mouth during the water-sediment regulation[J]. Marine Geology & Quaternary Geology, 2018, 38(5): 41-51. doi: 10.16562/j.cnki.0256-1492.2018.05.004
Citation: YU Yonggui, SHI Xuefa, CHI Wanqing, HU Zifeng, QIAO Shuqing. Hourly change in sediment plume at the Yellow River mouth during the water-sediment regulation[J]. Marine Geology & Quaternary Geology, 2018, 38(5): 41-51. doi: 10.16562/j.cnki.0256-1492.2018.05.004

调水调沙期间黄河口羽状流的逐时变化

  • 基金项目:
    国家海洋局第一海洋研究所基本科研业务费专项资金项目“黄河调水调沙的沉积记录”(GY0215SG07)
详细信息
    作者简介: 于永贵(1982—),男,助理研究员,主要从事河口沉积动力过程研究,E-mail:yuyonggui@fio.org.cn
  • 中图分类号: X145

  • 文凤英编辑

Hourly change in sediment plume at the Yellow River mouth during the water-sediment regulation

  • 2002年黄河实施调水调沙以来,黄河入海泥沙普遍以异轻羽状流的形式在河口附近的有限区域内堆积下来。采用2011年、2012年以及2013年调水调沙期间3期静止轨道海洋水色卫星(GOCI)数据对黄河口附近海域进行悬浮物浓度反演,提取了黄河口羽状流的逐时变化信息;通过黄河口水动力数值模拟以及风场、潮汐等实测数据分析,阐明了羽状流逐时变化的驱动机制。研究结果表明:黄河调水调沙前后黄河口羽状流表现出单向变化和往复变化两种不同的变化过程;而悬浮物浓度的逐时变化显示:河口附近不同站位的悬浮物浓度逐时变化过程差异较大,同一站位的悬浮物浓度可在1小时之内升高或降低约100mg/L。单向变化型羽状流主要受单向潮流的控制,且GOCI观测时段位于一个落潮或者涨潮过程,河流动力较弱;往复变化型羽状流受涨、落潮往复潮流的控制,涨、落潮流向的转换驱使羽状流向相反的方向运动,而且羽状流位于潮流切变带以内,切变锋对羽状流的形态、分布范围具有明显的切变效应。

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  • 图 1  区域位置图

    Figure 1. 

    图 2  2011年7月9日黄河口羽状流3小时彩色合成图(a, b, c)及逐时运动轨迹(d)

    Figure 2. 

    图 3  2012年7月16日羽状流8个小时的彩色合成图(a, b, c, d, e, f, g, h)及逐时运动轨迹(i)

    Figure 3. 

    图 4  2013年6月14日羽状流8个小时的彩色合成图(a, b, c, d, e, f, g, h)及逐时运动轨迹(i)

    Figure 4. 

    图 5  黄河口羽状流典型站位位置图

    Figure 5. 

    图 6  2012年7月16日P1-P6站悬浮物浓度逐时变化

    Figure 6. 

    图 7  2011年7月9日孤东站潮位逐时变化

    Figure 7. 

    图 8  2011年7月9日10时至13时(a, b, c, d)黄河三角洲附近海域逐时流场图

    Figure 8. 

    图 9  2011年7月9日10时至13时(a, b, c, d)黄河口附逐时近悬沙浓度及流场示意图

    Figure 9. 

    图 10  (a) 外涨内落型切变带; (b)外落内涨型切变带;(c)外落内涨型切变带;(d)无流场切变带(据李广雪等(1994)修改)

    Figure 10. 

    表 1  2011年7月9日孤东站逐时风场信息

    Table 1.  Hourly-recorded wind field data at Gudong station on July 9, 2011

    时间(h) 风向 风速(m/s)
    01时 西南 3.1
    02时 西南 4.3
    03时 西南 3.3
    04时 西南 3.5
    05时 西南 3.2
    06时 西南 0.7
    07时 西南 1.4
    08时 西北 1.2
    09时 西北 1.2
    10时 西北 1.0
    11时 西北 1.4
    12时 西北 1.4
    13时 西北 1.8
    14时 西北 1.6
    15时 西北 1.7
    16时 西北 1.8
    17时 西北 3.3
    18时 西北 2.8
    19时 西北 2.8
    20时 西北 3.4
    21时 东南 3.4
    22时 东南 4.7
    23时 东南 3.9
    24时 东南 2.7
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  • [1]

    Milliman J D, Syvitski J. Geomorphic/Tectonic control of sediment discharge to the ocean: The importance of small mountainous rivers [J]. Journal of Geology, 1992, 100(5): 525-544. doi: 10.1086/629606

    [2]

    YANG Z, Milliman J, Galler J, et al. Yellow River's water and sediment discharge decreasing steadily [J]. EOS, Transaction, American Geophysical Union, 1998, 79: 589-592. http://d.old.wanfangdata.com.cn/NSTLQK/10.1029-98EO00428/

    [3]

    Wang H, Yang Z, Saito Y, et al. Interannual and seasonal variation of the Huanghe (Yellow River) water discharge over the past 50 years: Connections to impacts from ENSO events and dams [J]. Global and Planetary Change, 2006, 50 (3-4): 212-225. doi: 10.1016/j.gloplacha.2006.01.005

    [4]

    Wang H, Yang Z, Saito Y, et al. Stepwise decreases of the Huanghe (Yellow River) sediment load (1950-2005): impacts of climate changes and human activities [J]. Global and Planetary Change, 2007, 57, 331-354. doi: 10.1016/j.gloplacha.2007.01.003

    [5]

    杨作升, 李国刚, 王厚杰, 等. 55年来黄河下游逐日水沙过程变化及其对干流建库的响应[J].海洋地质与第四纪地质, 2008, 28 (6): 9-18. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ200806002.htm

    YANG Zuosheng, LI Guogang, WANG Houjie, et al. Variation of daily water and sediment discharge in the Yellow River lower reaches in the past 55 years and its response to the dam operation on its main stream[J]. Marine Geology & Quaternary Geology, 2008, 28 (6): 9-18. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ200806002.htm

    [6]

    Wang H, Bi N, Saito Y, et al. Recent changes in sediment delivery by the Huanghe (Yellow River) to the sea: Causes and environmental implications in its estuary [J]. Journal of Hydrology, 2010, 31: 302-313. http://d.old.wanfangdata.com.cn/NSTLQK/10.1016-j.jhydrol.2010.07.030/

    [7]

    Yu Y G, Wang H J, Shi X F, et al. New discharge regime of the Huanghe (Yellow River): Causes and implications [J]. Continental Shelf Research, 2013, 69: 62-72. doi: 10.1016/j.csr.2013.09.013

    [8]

    于帅, 毕乃双, 王厚杰, 等.黄河调水调沙影响下河口入海泥沙扩散及沉积效应[J].海洋湖沼通报, 2015, 2:155-163. http://d.old.wanfangdata.com.cn/Periodical/hyhztb201502022

    YU Shuai, BI Naishuang, WANG Houjie, et al. Suspended sediment dispersal off The Huanghe (Yellow River) River mouth and its sedimentary effects under impact of the water-sediment regulation scheme[J]. Transactions of Oceanology and Limnology. 2015, 2:155-163. http://d.old.wanfangdata.com.cn/Periodical/hyhztb201502022

    [9]

    Wu X, Bi N S, Yuan P, et al. Sediment dispersal and accumulation off the present Huanghe (Yellow River) delta as impacted by the Water-Sediment Regulation Scheme [J]. Continental Shelf Research, 2015, 111:126-138. doi: 10.1016/j.csr.2015.11.003

    [10]

    刘锋, 陈沈良, 周永东, 等.黄河2009年调水调沙期间河口水动力及悬沙输移变化特征[J].泥沙研究, 2009, 12(6): 1-8. http://d.old.wanfangdata.com.cn/Periodical/nsyj201006001

    LIU Feng, CHEN Shenliang., ZHOU Yongdong, et al. Effect of water-sediment regulation in the Yellow River on hydrodynamics and suspended sediment transport in the Estuary[J]. Journal of Sediment Research, 2009, 12(6): 1-8. http://d.old.wanfangdata.com.cn/Periodical/nsyj201006001

    [11]

    于帅.黄河调水调沙影响下河口入海泥沙扩散及沉积效应[D].青岛: 中国海洋大学, 2014.

    YU Shuai. Sediment dispersal and accumulation at the Huanghe River mouth as impacted by the Water-Sediment Regulation [D]. Qingdao, Ocean University of China, 2014.

    [12]

    Wiseman W J, Yang Z S, Bornhold B D, et al. Suspended sediment advection by tidal currents off the Huanghe (Yellow River) delta [J]. Geo-Marine Letters, 1986, 6: 107-113. doi: 10.1007/BF02281646

    [13]

    庞重光, 杨作升, 张军, 等.黄河口最大浑浊带特征及其时空演变[J].黄渤海海洋, 2000, 18(3): 1-6. http://d.old.wanfangdata.com.cn/Periodical/hbhhy200003007

    PANG Chongguang, YANG Zuosheng., ZHANG Jun, et al. Characteristics and evolution of turbidity maximum at the Yellow River estuary [J]. Journal of Oceanography of Huanghai & Bohai Seas, 2000, 18(3): 1-6. http://d.old.wanfangdata.com.cn/Periodical/hbhhy200003007

    [14]

    Chao S Y. River-forced estuarine plumes [J]. Journal of Physical Oceanography, 1987, 18: 72-88.

    [15]

    Chao S Y. Wind-driven motion of estuarine plumes [J]. Journal of Physical Oceanography, 1988, 18: 1144-1166. doi: 10.1175/1520-0485(1988)018<1144:WDMOEP>2.0.CO;2

    [16]

    李广雪, 成国栋, 魏合龙, 等.现代黄河口区流场切变带[J].科学通报, 1994, 39(10): 928-932. http://d.old.wanfangdata.com.cn/Thesis/D548442

    LI Guangxue, CHENG Guodong, WEI Helong, et al. Tidal shear front at the modern Yellow River mouth[J]. Chinese Science Bulletin, 1994, 39(10): 928-932. http://d.old.wanfangdata.com.cn/Thesis/D548442

    [17]

    李广雪.黄河入海泥沙扩散与河海相互作用[J].海洋地质与第四纪地质, 1999, 19(3): 1-10. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ200403021.htm

    LI Guangxue. Suspended sediment dispersal and interaction of river-sea off the Yellow River mouth[J]. Marine Geology and Quaternary Geology, 1999, 19(3): 1-10. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ200403021.htm

    [18]

    Walker N. Satellite assessment of Mississippi River plume variability: causes and predictability [J]. Remote Sensing of Environment, 1996, 58 (1): 21-35.

    [19]

    Dagg M, Benner R, Lohrenz S, et al. Transformation of dissolved and particulate materials on continental shelves influenced by large rivers: plume processes [J]. Continental Shelf Research, 2004, 24 (7-8): 833-858. doi: 10.1016/j.csr.2004.02.003

    [20]

    Wang H, Yang Z, Li Y, et al. Dispersal pattern of suspended sediment in the shear frontal zone off the Huanghe (Yellow River) mouth [J]. Continental Shelf Research, 2007, 27: 854-871. doi: 10.1016/j.csr.2006.12.002

    [21]

    Wang Q, Guo X, Takeoka H. Seasonal variations of the Yellow River plume in the Bohai Sea: A model study [J]. Journal of Geophysical Research, 2008, 113, C08046, doi: 10.1029/2007JC004555.

    [22]

    毕乃双, 杨作升, 王厚杰, 等.黄河调水调沙期间黄河入海水沙的扩散及通量[J].海洋地质与第四纪地质, 2010, 2:27-34. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ201305009.htm

    BI Naishuang, YANG Zuosheng, WANG Houjie, et al. Characteristics of dispersal of the Yellow River Water and sediment to the sea during water-sediment regulation period of the Yellow River and its dynamic mechanism [J]. Marine Geology & Quaternary Geology, 2010, 2:27-34. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ201305009.htm

    [23]

    郝艳玲.黄河口水体生物光学性质逐时变化的静止海洋水色卫星遥感探测研究[D].青岛: 中国海洋大学, 2012.

    HAO Yanling. Detection of hourly variability of bio-optical properties in the Yellow River estuary by Geostationary Satellite Ocean Color Images [D]. Qingdaoo, Ocean University of China, 2012.

    [24]

    王厚杰, 杨作升, 毕乃双, 等. 2005年黄河调水调沙期间河口入海主流的快速摆动[J].科学通报, 2005, 50(23): 2656-2662. http://d.old.wanfangdata.com.cn/Periodical/kxtb200523016

    WANG Houjie, YANG Zuosheng, BI Naishuang, et al. Rapid shifts of the river plume pathway off the Huanghe mouth during water-sediment regulation scheme in 2005[J]. Chinese Science Bulletin, 2005, 50(23): 2656-2662. http://d.old.wanfangdata.com.cn/Periodical/kxtb200523016

    [25]

    潘德炉, 王迪峰.我国海洋光学遥感应用科学研究的新进展[J].地球科学进展, 2004, 19(4): 506-512. http://d.old.wanfangdata.com.cn/Periodical/dqkxjz200404003

    PAN Delu, WANG Difeng. Advances in the science of marine optical remote sensing application in China[J]. Advances in Earth Science, 2004, 19(4): 506-512. http://d.old.wanfangdata.com.cn/Periodical/dqkxjz200404003

    [26]

    Thomas A, Weatherbee R. Satellite-measured temporal variability of the Columbia River plume [J]. Remote Sensing of Environment, 2006, 100: 167-178. doi: 10.1016/j.rse.2005.10.018

    [27]

    周为峰.静止卫星的海洋水色观测计划[J].世界科技研究与发展, 2008, 30(2):180-184. http://d.old.wanfangdata.com.cn/Periodical/sjkjyjyfz200802019

    ZHOU Weifeng. The introduction of international plans in monitoring ocean color on the geostationary satellites[J]. World Sci-Tech R&D, 2008, 30(2):180-184. http://d.old.wanfangdata.com.cn/Periodical/sjkjyjyfz200802019

    [28]

    Hu Z F, Pan D L, He X Q, et al. Diurnal variability of turbidity fronts observed by geostationary satellite ocean color remote sensing [J]. Remote Sensing, 2016, 8, 147, doi:10.3390/rs8020147.

    [29]

    王厚杰, 杨作升, 毕乃双.黄河口泥沙输运三维数值模拟I-黄河口切变锋[J].泥沙研究, 2006, 2:1-9.

    WANG Houjie, YANG Zuosheng, BI Naishuang. 3-D simulation of the suspended sediment transport in the Yellow River mouth I: Shear front off the Yellow River mouth[J]. Journal of Sediment Research, 2006, 2:1-9.

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出版历程
收稿日期:  2017-11-16
修回日期:  2018-04-17
刊出日期:  2018-10-28

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