首页> 外文会议>第21届国际摄影测量与遥感大会(ISPRS 2008)论文集 >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:基于短间隔,高频率MODIS数据集的不连续潮间带DEM构造方法-以江苏省放射状潮河带东沙砂库为例

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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:地表高程是地球科学研究的关键数据。对于某些地貌变化迅速的地区,分析不同时期的地表高度有助于为区域经济社会的可持续发展提供科学依据。江苏沿海为潮汐带,复杂的泥沙动力环境,潮滩地貌平缓滚动,潮滩含水量的空间差异随时间,地貌类型和潮汐条件变化而变化,海域,季节和海底泥沙浓度不同。潮期。很难从RS影像中检索潮汐平面高程信息。自2000年以来,该研究区域的MODIS影像在时间序列上具有大量,高频率和完整的特征。本研究以东沙沙洲为例,尝试建立基于短间隔,高频MODIS RS影像数据集的历史DEM构造方法。研究的出发点是:由于研究区的潮汐为半日潮,因此裸露的滩涂海岸线随时间而变化。由于以下因素,不同RS影像中沙丘的轮廓彼此不同:1)沙丘本身的时空演变引起的差异。 2)差异是由于不同成像时刻之间的潮汐水平差异巨大所致。如果时间间隔足够短,则可以忽略沙岸演变的因素,并且两个RS影像中沙岸海岸线的前导差异反映了潮位差异的影响。因此,讨论了潮间带建设框架的DEM。

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