OU Suying, YANG Qingshu, LUO Xiangxin, ZHU Fan, LUO Kaiwen, YANG Hao. The influence of runoff and wind on the dispersion patterns of suspended sediment in the Zhujiang (Pearl) River Estuary based on MODIS data[J]. Acta Oceanologica Sinica, 2019, 38(3): 26-35. doi: 10.1007/s13131-019-1396-4
Citation: OU Suying, YANG Qingshu, LUO Xiangxin, ZHU Fan, LUO Kaiwen, YANG Hao. The influence of runoff and wind on the dispersion patterns of suspended sediment in the Zhujiang (Pearl) River Estuary based on MODIS data[J]. Acta Oceanologica Sinica, 2019, 38(3): 26-35. doi: 10.1007/s13131-019-1396-4

The influence of runoff and wind on the dispersion patterns of suspended sediment in the Zhujiang (Pearl) River Estuary based on MODIS data

doi: 10.1007/s13131-019-1396-4
  • Received Date: 2017-11-23
  • Cloud-free moderate-resolution imaging spectroradiometer (MODIS) images of the Zhujiang (Pearl) River Estuary (ZRE) taken between 2002 and 2012 are retrieved and used to study the spatial and temporal patterns of suspended sediment concentrations (SSCs) across the estuary under runoff, wind, and tropical storm conditions. Five typical dispersal patterns of suspended sediments in the estuary are defined:Case I shows generally low SSCs under low dynamics; Case Ⅱ shows a river-dominant dispersal pattern of suspended sediments from the outlets, particularly from Modaomen, Jiaomen, Hengmen, and others; Case Ⅲ shows wind-dominant dispersal of high SSCs derived from the west shoal and southwesterly transport under a strong NE wind; Case IV is the combination of relatively large runoff and wind; and Case V is caused by a strong tropical storm with high river discharge and wind, which is characterized by the high SSCs across the entire estuary that are transported eastward by wind-driven and buoyancy currents outside the estuary. Runoff is a dominant factor that controls seasonal and annual SSC variations in the ZRE, with the area of high SSCs being largest in the summer and smallest in the spring. The correlation coefficients between the monthly averaged river-suspended sediment discharge and the area of the high SSCs are approximately 0.6. The wind power over the west shoal increases with a wind speed, which induces more sediment resuspension and shows a close relationship between the wind speed and high SSC area.
  • loading
  • Alvarez, Gomez-Gesteira M, Decastro M, et al. 2014. Comparison of different wind products and buoy wind data with seasonality and interannual climate variability in the southern Bay of Biscay (2000-2009). Deep-Sea Research Part Ⅱ-Topical Studies in Oceanography, 106:38-48, doi: 10.1016/j.dsr2.2013.09.028
    Bourrin F, Friend P L, Amos C L, et al. 2008. Sediment dispersal from a typical Mediterranean flood:The Têt River, Gulf of Lions. Continental Shelf Research, 28(15):1895-1910, doi: 10.1016/j.csr.2008.06.005
    Chen Shuisen, Huang Wenrui, Chen Weiqi, et al. 2011. Remote sensing analysis of rainstorm effects on sediment concentrations in Apalachicola Bay, USA. Ecological Informatics, 6(2):147-155, doi: 10.1016/j.ecoinf.2010.12.001
    Chen Shuisen, Huang Wenrui, Wang Hongqing, et al. 2012. Remote sensing assessment of sediment re-suspension during Hurricane Frances in Apalachicola Bay, USA. Remote Sensing of Environment, 113(12):2670-2681
    Chen Weibo, Liu Wencheng, Hsu M H, et al. 2015. Modeling investigation of suspended sediment transport in a tidal estuary using a three-dimensional model. Applied Mathematical Modelling, 39(9):2570-2586, doi: 10.1016/j.apm.2014.11.006
    Cuvilliez A, Lafite R, Deloffre J, et al. 2015. River flow control on intertidal mudflat sedimentation in the mouth of a macrotidal estuary. Geomorphology, 239:174-181, doi: 10.1016/j.geomorph.2015.03.020
    Doxaran D, Froidefond J M, Castaing P, et al. 2012. Dynamics of the turbidity maximum zone in a macrotidal estuary (the Gironde, France):Observations from field and MODIS satellite data. Estuarine, Coastal and Shelf Science, 81(3):321-332
    Fagherazzi S, Mariotti G, Banks A T, et al. 2014. The relationships among hydrodynamics, sediment distribution, and chlorophyll in a mesotidal estuary. Estuarine, Coastal and Shelf Science, 144:54-64, doi: 10.1016/j.ecss.2014.04.003
    Feng Lian, Hu Chuanmin, Chen Xiaoling, et al. 2014. Influence of the Three Gorges Dam on total suspended matters in the Yangtze Estuary and its adjacent coastal waters:Observations from MODIS. Remote Sensing of Environment, 140:779-788, doi: 10.1016/j.rse.2013.10.002
    Fernández-Nóvoa D, Mendes R, deCastro M, et al. 2015. Analysis of the influence of river discharge and wind on the Ebro turbid plume using MODIS-Aqua and MODIS-Terra data. Journal of Marine Systems, 142:40-46, doi: 10.1016/j.jmarsys.2014.09.009
    Freeman Freeman A M, Jose F, Roberts H H, et al. 2015. Storm induced hydrodynamics and sediment transport in a coastal Louisiana lake. Estuarine, Coastal and Shelf Science, 161:65-75, doi: 10.1016/j.ecss.2015.04.011
    Gong Wenping, Jia Liangwen, Shen Jian, et al. 2014. Sediment transport in response to changes in river discharge and tidal mixing in a funnel-shaped micro-tidal estuary. Continental Shelf Research, 76:89-107, doi: 10.1016/j.csr.2014.01.006
    Gong Wenping, Shen Jian. 2012. Response of sediment dynamics in the York River Estuary, USA to tropical cyclone Isabel of 2003. Estuarine, Coastal and Shelf Science, 84(1):61-74
    Green M O, Coco G. 2014. Review of wave-driven sediment resuspension and transport in estuaries. Reviews of Geophysics, 52(1):77-117, doi: 10.1002/rog.v52.1
    Lahet F, Stramski D. 2010. MODIS imagery of turbid plumes in San Diego coastal waters during rainstorm events. Remote Sensing of Environment, 114(2):332-344, doi: 10.1016/j.rse.2009.09.017
    Lawson S E, Wiberg P L, Mcglathery K J, et al. 2007. Wind-driven sediment suspension controls light availability in a shallow coastal lagoon. Estuaries and Coasts, 30(1):102-112, doi: 10.1007/BF02782971
    Li Zhanhai, Li M Z, Dai Zhijun, et al. 2015. Intratidal and neap-spring variations of suspended sediment concentrations and sediment transport processes in the North Branch of the Changjiang Estuary. Acta Oceanologica Sinica, 34(1):137-147, doi: 10.1007/s13131-015-0605-z
    Li P, Yang S L, Milliman J D, et al. 2012. Spatial, temporal, and human-induced variations in suspended sediment concentration in the surface waters of the Yangtze Estuary and adjacent coastal areas. Estuaries and Coasts, 35(5):1316-1327, doi: 10.1007/s12237-012-9523-x
    Lihan T, Saitoh S I, Iida T. 2008. Satellite-measured temporal and spatial variability of the Tokachi River plume. Estuarine, Coastal and Shelf Science, 78(2):237-249, doi: 10.1016/j.ecss.2007.12.001
    Liu Xiaohai, Huang Wenrui. 2012. Modeling sediment resuspension and transport induced by storm wind in Apalachicola Bay, USA. Environmental Modelling & Software, 24(11):1302-1313
    Liu Xiaoming, Wang Menghua. 2014. River runoff effect on the suspended sediment property in the upper Chesapeake Bay using MODIS observations and ROMS simulations. Journal of Geophysical Research:Oceans, 119(12):8646-8661, doi: 10.1002/2014JC010081
    Mao Q W, Shi P, Yin K D, et al. 2004. Tides and tidal currents in the Pearl River Estuary. Continental Shelf Research, 24:1797-1808, doi: 10.1016/j.csr.2004.06.008
    Moreira D, Simionato C G, Gohin F, et al. 2013. Suspended matter mean distribution and seasonal cycle in the Río de La Plata estuary and the adjacent shelf from ocean color satellite (MODIS) and in-situ observations. Continental Shelf Research, 68:51-66, doi: 10.1016/j.csr.2013.08.015
    Nezlin N P, DiGiacomo P M, Diehl D W, et al. 2008. Stormwater plume detection by MODIS imagery in the southern California coastal ocean. Estuarine, Coastal and Shelf Science, 80(1):141-152, doi: 10.1016/j.ecss.2008.07.012
    Ou Suying, Zhang Hong, Wang Dongxiao. 2009. Dynamics of the buoyant plume off the Pearl River Estuary in summer. Environmental Fluid Mechanics, 9(5):471-492, doi: 10.1007/s10652-009-9146-3
    Percuoco V P, Kalnejais L H, Officer L V. 2015. Nutrient release from the sediments of the Great Bay Estuary, N. H. USA. Estuarine, Coastal and Shelf Science, 161:76-87, doi: 10.1016/j.ecss.2015.04.006
    Petus C, Chust G, Gohin F, et al. 2010. Estimating turbidity and total suspended matter in the Adour River plume (South Bay of Biscay) using MODIS 250-m imagery. Continental Shelf Research, 30(5):379-392, doi: 10.1016/j.csr.2009.12.007
    Petus C, Marieu V, Novoa S, et al. 2014. Monitoring spatio-temporal variability of the Adour River turbid plume (Bay of Biscay, France) with MODIS 250-m imagery. Continental Shelf Research, 74:35-49, doi: 10.1016/j.csr.2013.11.011
    Wu Guofeng, Liu Liangjie, Chen Fangyuan, et al. 2014. Developing MODIS-based retrieval models of suspended particulate matter concentration in Dongting Lake, China. International Journal of Applied Earth Observation and Geoinformation, 32:46-53, doi: 10.1016/j.jag.2014.03.025
    Xing Qianguo, Lou Mingjing, Chen Chuqun, et al. 2013. Using in situ and satellite hyperspectral data to estimate the surface suspended sediments concentrations in the Pearl River Estuary. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 6(2):731-738, doi: 10.1109/JSTARS.2013.2238659
    Yang Ganran, Chen Lianggui. 1987. Wave characteristics and calculation of typhoon wave in Mawan harbour. Tropic Oceanology (in Chinese), 6(1):66-72
    Zhang Wei, Xu Zheng, Dong Xue, et al. 2010. Analysis on characteristics of temporal and spatial variation of suspended sediment in the Lingding Bay. Journal of Sediment Research (in Chinese), (4):22-28
    Zu Tingting, Wang Dongxiao, Gan Jianping, et al. 2014. On the role of wind and tide in generating variability of Pearl River plume during summer in a coupled wide estuary and shelf system. Journal of Marine Systems, 136:65-79, doi: 10.1016/j.jmarsys.2014.03.005
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Article Metrics

    Article views (630) PDF downloads(418) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return