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Soil Moisture And Drought Monitoring In Casablanca-Settat Region, Morocco By The Use Of Gis And Remote Sensing

机译:地理信息系统和遥感技术在摩洛哥卡萨布兰卡-塞塔特地区的土壤水分和干旱监测

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Soil moisture (SM) is a key factor in climate, hydrology, and agronomy. Its assessment is therefore important and constitutes an alert parameter for desertification. It impacts the heat and mass transfers between soil and atmosphere. However, information access in the regional or global scale is very complicated which usually leads to a rough estimate, or completely disregard of this parameter. Today, remote sensing offers a solution to this problem by providing access to this information through the satellite images. The use of geospatial data to generate adequate information on droughts, we applied the remote sensing method based on the use of the Soil Moisture Index (SMI), which in its algorithm uses the data obtained from satellite sensors. As reported by Hunt et al., The index is based on actual water content (), water capacity and wilting point. The multispectral satellite images from the visible (red band) and infrared (near-infrared and thermal band) bands are essential for the calculation of the index, which is why we used Landsat 8 OLI/TIRS in this context, then SMOS disaggregated data is chosen to be compared with SMI and MI (Moisture Index) used in this work. On the other side, drought monitoring in Morocco faces complexity in the evidence that it depends on a lot of parameters including the SM. Thus, the aim of this paper is firstly to analyze the spatiotemporal variation of SM from SMOS in Casablanca-Settat region of Morocco site during five successive years 2013 to 2017. For that, the first temporal SM values mapping of the study area is established for each year of 2013 to 2017. Next, for each year we will compare SM from SMOS with SMI by drawing the graph line of SM variability in this period and generating differences maps. Secondly, we will evaluate the effect and the impact of Soil Moisture Index (SMI) in Drought monitoring by calculation of Land Surface Temperature (LST) from Landsat 8 OLI/TIRS, and define which indexes are more indicated for assessing soil conditions.
机译:土壤水分(SM)是气候,水文学和农学的关键因素。因此,对它的评估很重要,并构成了荒漠化的预警参数。它影响土壤与大气之间的热量和质量传递。但是,区域或全球范围内的信息访问非常复杂,这通常会导致粗略估计或完全忽略此参数。如今,遥感通过提供通过卫星图像访问此信息的方式,为解决这一问题提供了解决方案。利用地理空间数据生成有关干旱的足够信息,我们基于土壤水分指数(SMI)应用了遥感方法,该算法在其算法中使用了从卫星传感器获得的数据。正如Hunt等人所报道的那样,该指数基于实际含水量(),水容量和萎点。来自可见(红色波段)和红外(近红外和热波段)波段的多光谱卫星图像对于指数的计算至关重要,这就是为什么我们在这种情况下使用Landsat 8 OLI / TIRS,然后将SMOS分解后的数据选择与本工作中使用的SMI和MI(湿度指数)进行比较。另一方面,摩洛哥的干旱监测面临复杂性,因为它取决于包括SM在内的许多参数。因此,本文的目的是首先分析2013年至2017年连续5年摩洛哥站点卡萨布兰卡-塞塔特地区SMOS的SM的时空变化。为此,建立了该研究区域的第一个时间SM值图。 2013年至2017年的每一年。接下来,我们将通过绘制此期间SM变异性的图形线并生成差异图,比较SMOS和SMI的SM。其次,我们将通过根据Landsat 8 OLI / TIRS计算地表温度(LST)来评估土壤水分指数(SMI)在干旱监测中的作用和影响,并确定哪些指数更适合用于评估土壤条件。

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