首页> 外文会议>20 years of Progress in Radar Altimetry >VARIATIONAL DATA ASSIMILATION OF AIRSWOT AND SWOT DATA INTO THE 2D SHALLOW WATER MODEL DASSFLOW. METHOD AND TEST CASE ON GARONNE RIVER (FRANCE)
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VARIATIONAL DATA ASSIMILATION OF AIRSWOT AND SWOT DATA INTO THE 2D SHALLOW WATER MODEL DASSFLOW. METHOD AND TEST CASE ON GARONNE RIVER (FRANCE)

机译:AIRSWOT和SWOT数据的变化数据同化到2D浅水模型DASSFLOW中。加伦河(法国)的方法和试验案例

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摘要

For continental water bodies and riverrnhydraulic studies, water level measurements arernfundamental information, yet they are currently mostlyrnprovided by punctual gauging stations located on thernmain river channel. That is why they are sparselyrndistributed in space and can have gaps in their timernseries (e.g. sensors failures). These issues can berncompensated by remote sensing data, which havernconsiderably contributed to improve the observation andrnunderstanding of physical processes in hydrology andrnhydraulics in general. Satellites such as SWOT (SurfacernWater and Ocean Topography) would give spatiallyrndistributed information on water elevations at anrnunprecedented resolution. Gathering pre-mission datarnover specific and varied science targets is the purpose ofrnthe AirSWOT airborne campaign in order to implementrnand test SWOT products retrieval algorithms. A reachrnof the Garonne River, downstream of Toulousern(FRANCE), is a proposed study area for AirSWOTrnflights. This choice is motivated by previous studiesrnalready performed on this section of 100km reach of thernriver. Moreover, on this highly instrumented and studiedrnportion of river many typical free surface flowrnmodelling issue has been encountered, and this riverrnreach represents the limit of SWOT observationrncapability. The 2D hydrodynamic model DassFlowrnespecially designed for variational data assimilation willrnbe used on this portion of the Garonne River withrncartographic sensitivity analysis. An identificationrnstrategy would allow retrieving spatial roughness alongrnthe main channel, variation of the local topographicrnslope or else temporal evolution of the streamflow.rnAddressing such problems and studying horizontal andrnvertical river sinuosity would improve fine scalernhydraulics representation and understanding, whichrncould additionally help to improve global dischargernalgorithms with different scales and complexity levels.
机译:对于大陆水体和河流水力研究而言,水位测量是基础信息,但目前大多由位于主河道上的准时测量站提供。这就是为什么它们在空间上稀疏分布并且在时间序列上可能会有间隔(例如传感器故障)的原因。这些问题可以通过遥感数据来弥补,这对于改善对水文学和液压力学中的物理过程的观察和理解有很大贡献。诸如SWOT(地表水和海洋地形)之类的卫星将以前所未有的分辨率提供有关水位的空间分布信息。收集飞行任务特定目标和各种科学目标的数据是AirSWOT空降战役的目的,目的是实施和测试SWOT产品检索算法。图卢兹(FRANCE)下游的加龙河(Garonne River)河段是拟议的AirSWOTrnflights研究区域。这种选择是受先前对热河100公里范围的这一部分已经进行的研究的启发。此外,在这种高度仪器化和研究的河流中,遇到了许多典型的自由表面流建模问题,而该河流的延伸代表了SWOT观测能力的极限。专门为变化数据同化设计的二维水动力模型DassFlowr将用于加隆河的这一部分,并具有制图敏感性分析。识别策略可以检索沿主要通道的空间粗糙度,局部地形的坡度变化或河流的时间演变。解决此类问题并研究水平和垂直河流的正弦度将改善精细比例的水力表示和理解,这还可以帮助改善不同形式的全球排放算法规模和复杂程度。

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  • 会议地点 Venice(IT)
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    Université de Toulouse INSA IMT F-31400 Toulouse, France. pierre-andre.garambois@imft.fr;

    CNRS/LEGOS FR sylvain.biancamria@legos.obs-mip.fr;

    Université de Toulouse INSA IMT F-31400 Toulouse, Francejerome.monnier@insa-toulouse.fr;

    Université de Toulouse INP IMFT F-31400 Toulouse, France. hroux@imft.fr;

    Université de Toulouse INP IMFT F-31400 Toulouse, France dartus@imft.fr;

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