MAPPING OF SPATIO-TEMPORAL LANDUSE AND LAND SURFACE TEMPERATURE USING SATELLITE DATA- A CASE STUDY OF SUKKUR-KOTRI INDUS REACH

Tayyaba Suhail, Sadia Allah Ditta, A. A. Siyal, K. Ansari
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Abstract

The riparian zone is an ecological corridor for the rivers, forests, and lakes where the transition of water occurs between flora, fauna, and alluvial soil. It functions as a barrier to protect the riparian cities from floods, a retainer to hold the sediments transported in the water body, and a purifier in an order to adsorb the harmful dissolved solids present in the river flow. At some rivers, where the riparian zone has been degraded, the natural vegetation is observed to be under-functioning, consequently decreasing the water quality. The anthropogenic activities on river beds e.g agriculture are a reason for riparian degradation. In this study, the riparian zone of River Indus’s reach between the Sukkur and Kotri barrages is observed to identify the varying land covers and land temperature ranges due to agricultural invasion that could threaten the river ecosystem and sustainability. In a low flood period, less moisture on the river bed facilitates the detection of mature Rabi crops through the Landsat satellite. Acquired Imageries were classified for natural vegetation and agricultural area using the Visible bands. Land Surface Temperature (LST) was calculated from the pixels of the Thermal band. The images for 1999, 2003, 2010, 2015, 2018, and 2019 for February were utilized for the processing. Results demonstrated that in 1999, the 45.4% area of the Sukkur-Kotri reach was under the natural vegetation cover and decreased up to 14.2% area in 2019. In 1999, 22.5% of the reach area was under agricultural farming and increased up to 60% of the area in 2019. Analysis of surface temperature demonstrated that the areas having high temperatures are under natural vegetation cover, which is being reduced. And the areas having low temperatures are under agricultural farming, which is being increased inside the riparian zone.
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基于卫星数据的土地利用与地表温度时空制图——以苏库尔-科特里印度河河段为例
河岸带是河流、森林和湖泊的生态走廊,在这里,水在植物、动物和冲积土壤之间发生过渡。它的功能是保护河岸城市免受洪水侵袭的屏障,保留在水体中运输的沉积物,以及吸附河流中存在的有害溶解固体的净化器。在一些河流中,河岸带已经退化,自然植被功能不足,从而导致水质下降。河床上的人为活动(如农业)是导致河岸退化的一个原因。在本研究中,我们观察了苏库尔河和科特里河流域之间的印度河河段河岸带,以确定由于农业入侵而导致的土地覆盖和土地温度变化,这些变化可能威胁到河流生态系统和可持续性。在低潮期,河床上较少的水分有利于通过Landsat卫星探测成熟的Rabi作物。利用可见光波段对自然植被区和农区进行分类。利用热波段像元计算地表温度(LST)。利用1999年、2003年、2010年、2015年、2018年和2019年2月的图像进行处理。结果表明:1999年苏库尔—科特里河段自然植被覆盖面积为45.4%,2019年下降至14.2%;1999年,该流域22.5%的面积为农业,2019年这一比例增加到60%。地表温度分析表明,高温地区处于自然植被覆盖之下,植被覆盖正在减少。气温较低的地区正在进行农业耕作,在河岸地带,农业耕作正在增加。
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