首页> 外文会议>International archives of the photogrammetry, remote sensing and spatial information sciences conference >A DEM CONSTRUCTION METHOD FOR INCONSTANT INTER-TIDAL ZONE BASE ON SHORT-INTERVAL, HIGH FREQUENCY MODIS DATA SET: A CASE STUDY IN THE DONGSHA SANDBANK OF THE JIANGSU RADIAL TIDAL SAND-RIDGES
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A DEM CONSTRUCTION METHOD FOR INCONSTANT INTER-TIDAL ZONE BASE ON SHORT-INTERVAL, HIGH FREQUENCY MODIS DATA SET: A CASE STUDY IN THE DONGSHA SANDBANK OF THE JIANGSU RADIAL TIDAL SAND-RIDGES

机译:江苏东沙砂浆近距离潮汐区的第一次潮汐区底座的DEM施工方法 - 以江苏径向潮汐散砂砂浆为例

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Surface elevation is a critical data for geo-science study. As far as some regions with rapidly-changing in landform, analyzing the surface elevation of different periods help provide scientific basis for regional economic & social sustained development. Jiangsu coast is force tide zone, and the complicated sediment dynamical environment, gently rolling tidal-flat landform, huge spatial difference in tidal-flat moisture content changing with the time, geomorphic type and tidal condition, sediment concentration differing in sea area, season and tidal period. It is difficult to retrieve tidal-flat elevation information from RS imageries. Massive, high frequency and complete in temporal series of MODIS imageries on the study area since 2000 have been accumulated. The study takes Dongsha Sandbank as a case study area, and attempts to formulate a construction method for historical DEM based on short-interval, high frequency MODIS RS imageries data set. Starting point of the study is: shorelines of exposed tidal flat changes period with time because the tidal regime of research area is semi-diurnal tide. Contours of the sandbank in different RS imagery differ from each other due to the following factors: 1) Difference caused by spatial and temporal evolution of the sandbank itself. 2) Difference caused by the huge difference of tidal-level between different imaging moments. If the time interval is short enough, the factor of sandbank evolution can be ignored, and the leading difference of the sandbank shoreline in the two RS imageries reflects the influence of tidal-level difference. For this reason, DEM of the inter-tidal zone construction framework was discussed.
机译:表面高度是地质科学研究的关键数据。至于具有迅速变化的地貌,分析不同时期的表面高度有助于为区域经济和社会持续发展提供科学依据。江苏海岸是强制潮汐区,复杂的沉积物动态环境,轻轻滚动潮汐地貌,潮汐型水分含量巨大的空间差异,随着时间的推移,地貌型和潮汐条件,海域沉积物浓度不同。潮汐期。难以从RS成像检索潮汐平面信息。自2000年以来,累积了大规模的,高频和临时系列Modis Imageries,自2000年累积。该研究将Dongsha Sandbank视为案例研究区,并试图根据短期间,高频MODIS RS Imageries数据集制定历史DEM的施工方法。研究的起点是:暴露的潮汐平面变化周期随着时间的推移,因为研究区域的潮汐制度是半昼夜潮。由于以下因素的以下因素,不同的RS图像中的沙袋的轮廓彼此不同:1)砂银的空间和时间演化引起的差异。 2)不同成像时刻之间的潮汐级巨大差异引起的差异。如果时间间隔足够短,则可以忽略砂银进化的因素,两种RS成像中的砂银海岸线的主要差异反映了潮汐级别的影响。因此,讨论了互相互连区施工框架的DEM。

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