The Water Area of Sawa Lake as Derived from Land Surface Temperature and Remote Sensing Data

Haidar A. Radeef, I. Abdulameer
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Abstract

Sawa Lake is one of the unique lakes in Iraq. It is located in the southwestern part of Iraq. It is one of the closed lakes, as no surface water source works to feed the lake. The lake feeds on groundwater. The source of this groundwater is the Dammam Basin. During the past ten years, The lake has had many changes, which led to a decrease in water levels. This also led attention to study of the causes of these changes. Many types of research were presented in the study of the state of the lake. This research used remote sensing images from Landsat 8 OLI to monitor the changes during 2020-2021 by applying the NDWI equation to extract water area from image data. The results of the areas were obtained from a special report by Normalized Difference Water Index (NDWI). Then, the lake surface water temperature was derived from Landsat 8 thermal bands (TIRS). The lake water area and temperatures increased in summer and decreased in winter and autumn. Then, it is not the main reason for the change in the lake water area. The levels of the lake water rise during the dry period and decrease during the rainy period. The natural factors have little influence in reducing the lake water. It is attributed to human factors, groundwater depletion, and a reduction in water supply from the Dammam Basin, which feeds the lake.
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基于地表温度和遥感数据的萨瓦湖水域面积
萨瓦湖是伊拉克独特的湖泊之一。它位于伊拉克西南部。它是一个封闭的湖泊,因为没有地表水的来源工程来喂养湖泊。这个湖以地下水为水源。地下水的来源是达曼盆地。在过去的十年里,这个湖发生了许多变化,导致水位下降。这也引起了人们对这些变化原因的研究。在对湖泊状况的研究中,提出了许多类型的研究。本研究利用Landsat 8 OLI遥感影像,应用NDWI方程从影像数据中提取水域面积,监测2020-2021年的变化。这些地区的结果来自一份特别报告,采用归一化差水指数(NDWI)。然后利用Landsat 8热带(TIRS)反演湖泊地表水温。湖水面积和温度夏季呈上升趋势,冬季和秋季呈下降趋势。因此,它不是湖泊水域变化的主要原因。枯水期湖水水位上升,雨季水位下降。自然因素对湖泊水量的减少影响不大。这是由于人为因素、地下水枯竭以及达曼盆地供水量减少造成的。达曼盆地是该湖泊的水源。
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发文量
67
审稿时长
18 weeks
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