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Real time drought monitoring using Remote Sensing approaches A Case Study :Western desert of Kharga and Dakhla Regions

机译:遥感方法进行干旱实时监测案例研究:喀尔加和达克拉地区西部沙漠

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A new? drought index? was developed using Soil moisture(SM)? and Land Surface temperature (LST) reflectance data, which deduced from Landsat images, called ( LST/SM). This new index was examined beside other effective existing drought index named Perpendicular Drought Index( PDI), which consider? as useful indicator for? monitoring drought condition . These indices were applied on the middle of? western desert of Egypt ( Kharga and Dakhla regions ) as study areas. Red ,blue, and near- infrared? wavelengths of? landsat 8 (2014) and TM 5(2003) images were preprocessed First geo-registed then converted to TOA Reflectance for SM , PDI indices determination? Thermal? infrared bands were processed? using different algorithms? to deduce LST data . 800 random? points were well distributed? on each? resulted index? raster image to analyze? the drought condition. The results demonstrated? that for Kharga region the? mean? value for LST/SM index was slightly increased from 16.770 in 2003 to 16.807 in 2014,? and for PDI index ,the mean value increase? from 0.583 in 2003, to 0.6171 in 2014.For? Dakhla? region mean value? of LST/SM index? increase from 17.589 in 2003 to 20.820 in 2014 , while for? PDI? index , the mean value? increase? from 0.5676 in 2003? to 0.6021 in 2014. Standard deviation (SD )? for LST/SM index were? increased from 2.5933 in 2003 to 2.9775 in 2014? for Kharga region , and? SD increase from? 2.9996 in 2003?? to? 3.0756 in 2014 for? Dakhla region .? Analyzing the drought indices proof significant correlation? between LST/SM , PDI(r =.457). The results proof slightly increasing in drought condition? in the two study areas and this was agree with other previous field study. Finally These? indices? LST/SM and PDI have? the potential to provide? a effective, simple and real time monitoring method in the remote estimation of drought? phenomena.
机译:一个新的?干旱指数?是用土壤水分(SM)开发的?由Landsat影像得出的陆面温度(LST)反射率数据称为(LST / SM)。除了其他有效的现有干旱指数(垂直干旱指数(PDI))以外,还检查了该新指数,该考虑哪些因素?作为有用的指标?监测干旱状况。这些指标被应用在中间吗?埃及西部沙漠(哈尔加和达赫拉地区)为研究区域。红色,蓝色和近红外?波长是多少?对Landsat 8(2014)和TM 5(2003)图像进行了预处理,然后进行地理定位,然后转换为TOA反射率,用于SM,PDI指数测定?热的?红外波段被处理了吗?使用不同的算法?推断LST数据。 800随机?点分布均匀吗?在每一个上?结果索引?栅格图像进行分析?干旱条件。结果证明了吗?那对于喀尔加地区呢?意思? LST / SM指数的值从2003年的16.770略微增加到2014年的16.807,对于PDI指数,平均值增加了吗?从2003年的0.583,到2014年的0.6171。达赫拉?区域平均值? LST / SM指数?从2003年的17.589增加到2014年的20.820,为什么? PDI?指标,平均值?增加?从2003年的0.5676开始?到2014年的0.6021。标准差(SD)? LST / SM指数是多少?从2003年的2.5933增加到2014年的2.9775?喀尔加地区? SD从哪里增加? 2.9996在2003年??至? 2014年的3.0756?达赫拉地区。?分析干旱指数证明显着相关?在LST / SM之间,PDI(r = .457)。结果证明在干旱条件下略有增加?在这两个研究领域中,这与之前的其他实地研究一致。最后这些?指数? LST / SM和PDI有?提供的潜力?一种有效,简单且实时的远程干旱监测方法?现象。

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