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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Seasonal and inter-annual dynamics of suspended sediment at the mouth of the Amazon river: The role of continental and oceanic forcing, and implications for coastal geomorphology and mud bank formation
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Seasonal and inter-annual dynamics of suspended sediment at the mouth of the Amazon river: The role of continental and oceanic forcing, and implications for coastal geomorphology and mud bank formation

机译:亚马逊河河口悬浮泥沙的季节和年际动态:大陆和海洋强迫的作用,及其对海岸地貌和泥滩形成的影响

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Fine-grained sediments supplied to the Ocean by the Amazon River and their transport under the influence of continental and oceanic forcing drives the geomorphic change along the 1500 km-long coast northward to the Orinoco River delta. The aim of this study is to give an encompassing view of the sediment dynamics in the shallow coastal waters from the Amazon River mouth to the Capes region (northern part of the Amapa region of Brazil and eastern part of French Guiana), where large mud banks are formed. Mud banks are the overarching features in the dynamics of the Amazon-Orinoco coast. They start migrating northward in the Capes region. Suspended Particulate Matter (SPM) concentrations were calculated from satellite products (MODIS Aqua and Terra) acquired over the period 2000-2013. The Census-X11 decomposition method used to discriminate short-term, seasonal and long-term time components of the SPM variability has rendered possible a robust analysis of the impact of continental and oceanic forcing. Continental forcing agents considered are the Amazon River water discharge, SPM concentration and sediment discharge. Oceanic forcing comprises modelled data of wind speed and direction, wave height and direction, and currents. A 150 km-long area of accretion is detected at Cabo Norte that may be linked with a reported increase in the river's sediment discharge concurrent with the satellite data study period. We also assess the rate of mud bank migration north of Cabo Norte, and highlight its variability. Although we confirm a 2 km y(-1) migration rate, in agreement with other authors, we show that this velocity may be up to 5 km y(-1) along the Cabo Orange region, and we highlight the effect of water discharge by major rivers debouching on this coastal mud belt in modulating such rates. Finally, we propose a refined sediment transport pattern map of the region based on our results and of previous studies in the area such as the AMASSEDS programme, and discuss the relationship between sediment transport and accumulation patterns and the coastal geomorphology of this region. (C) 2016 Elsevier Ltd. All rights reserved.
机译:亚马逊河向海洋提供的细颗粒沉积物及其在大陆和海洋强迫作用下的运移,驱使沿北向奥里诺科河三角洲的1500公里长海岸的地貌变化。这项研究的目的是提供从亚马逊河河口到Capes地区(巴西的Amapa地区的北部和法属圭亚那的东部)的沿海浅水区沉积物动力学的全貌。形成。泥浆库是亚马逊-奥里诺科海岸动态的主要特征。他们开始在Capes地区向北迁移。悬浮颗粒物(SPM)浓度是根据2000-2013年期间获取的卫星产品(MODIS Aqua和Terra)计算得出的。用于区分SPM变异性的短期,季节性和长期时间成分的人口普查X11分解方法使得对大陆和海洋强迫影响的稳健分析成为可能。被考虑的大陆强迫因素是亚马逊河的水排放,SPM浓度和沉积物排放。海洋强迫包括风速和风向,波高和风向以及洋流的建模数据。在北卡波(Cabo Norte)发现了一个150公里长的积聚区域,这可能与所报告的河流沉积物增加以及卫星数据研究期有关。我们还评估了北卡波北部泥浆库的迁移速度,并突出了其可变性。尽管我们确定了2 km y(-1)的迁移速率,但与其他作者一致,我们表明沿卡波奥兰治地区该速度可能高达5 km y(-1),并且我们强调了排水的影响主要河流在调节这些流量的过程中在这条沿海淤泥带上开凿。最后,我们根据研究结果和该地区以前的研究(例如AMASSEDS计划),提出了该地区的精细泥沙迁移模式图,并讨论了该地区的泥沙迁移和累积模式与沿海地貌之间的关系。 (C)2016 Elsevier Ltd.保留所有权利。

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