首页> 外文期刊>Arabian journal of geosciences >Estimation of dune celerity and sand flux in part of West Rajasthan, Gadra area of the Thar Desert using temporal remote sensing data
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Estimation of dune celerity and sand flux in part of West Rajasthan, Gadra area of the Thar Desert using temporal remote sensing data

机译:使用时间遥感数据估算塔尔沙漠加德拉地区西拉贾斯坦邦部分地区的沙丘速度和沙通量

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The main objectives of this study were to estimate the dune celerity and sand flux in an arid environment (Gadra in Barmer District in Thar Desert, Rajasthan, India) using multi-temporal remote sensing data. Dunal shift estimation and interdunal space estimation, which are crucial for calculating sand flux, were also performed. We applied this method to two Cartosat-1 scenes (stereopairs) of years 2010 and 2011. Co-registration of Optically Sensed Images and Correlation was utilized to meet the above mentioned objectives. The mean dune shift for the study area for a year was estimated to be 1.25 m. Mean dune celerity was estimated as 0.0034 m/day or 1.24 m/year. Mean sand flux was estimated to be 0.0156 or 5.69 m(3)/m/year. Based on the results of the dune migration pattern, the co-registration accuracy was found to be 0.70 pixels, wherein the pixel resolution of input data was 2.50 m. This indicates that the root mean square error (RMSE) is about 1.60 m. However, our results demonstrated that dune celerity is 1.24 m per annum, which is within the RMSE level of the analysis. Therefore, this corroborates with the results that during the approximately 1-year time period, there is no apparent movement of the sand dunes in the study area.
机译:这项研究的主要目的是使用多时相遥感数据估算干旱环境(印度拉贾斯坦邦塔尔沙漠巴默区加德拉的加德拉)中的沙丘速度和沙通量。还进行了沙丘位移估计和跨界空间估计,这对于计算砂通量至关重要。我们将此方法应用于2010年和2011年的两个Cartosat-1场景(立体对)。利用光学图像和相关性的共配准来实现上述目标。研究区域一年的平均沙丘偏移量估计为1.25 m。平均沙丘速度估计为0.0034 m /天或1.24 m /年。平均砂通量估计为0.0156或5.69 m(3)/ m /年。根据沙丘迁移模式的结果,共配准精度为0.70像素,其中输入数据的像素分辨率为2.50 m。这表明均方根误差(RMSE)约为1.60 m。但是,我们的结果表明,沙丘速度为每年1.24 m,在分析的RMSE水平之内。因此,这与以下结果相吻合:在大约1年的时间段内,研究区域内沙丘没有明显的运动。

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