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Lake Chad Total Surface Water Area as Derived from Land Surface Temperature and Radar Remote Sensing Data

机译:湖乍得湖总面积水域源自陆地温度和雷达遥感数据

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摘要

Lake Chad, located in the middle of the African Sahel belt, underwent dramatic decreases in the 1970s and 1980s leaving less than ten percent of its 1960s surface water extent as open water. In this paper, we present an extended record (dry seasons 1988–2016) of the total surface water area of the lake (including both open water and flooded vegetation) derived using Land Surface Temperature (LST) data (dry seasons 2000–2016) from the NASA Terra MODIS sensor and EUMETSAT Meteosat-based LST measurements (dry seasons 1988–2001) from an earlier study. We also examine the total surface water area for Lake Chad using radar data (dry seasons 2015–2016) from the ESA Sentinel-1a mission. For the limited number of radar data sets available to us (18 data sets), we find on average a close match between the estimates from these data and the corresponding estimates from LST, though we find spatial differences in the estimates using the two types of data. We use these spatial differences to adjust the record (dry seasons 2000–2016) from MODIS LST. Then we use the adjusted record to remove the bias of the existing LST record (dry seasons 1988–2001) derived from Meteosat measurements and combine the two records. From this composite, extended record, we plot the total surface water area of the lake for the dry seasons of 1988–1989 through 2016–2017. We find for the dry seasons of 1988–1989 to 2016–2017 that the maximum total surface water area of the lake was approximately 16,800 sq. km (February and May, 2000), the minimum total surface water area of the lake was approximately 6400 sq. km (November, 1990), and the average was approximately 12,700 sq. km. Further, we find the total surface water area of the lake to be highly variable during this period, with an average rate of increase of approximately 143 km2 per year.
机译:乍得湖湖位于非洲萨赫尔腰带中部,在20世纪70年代和20世纪80年代的剧烈减少下降,占20世纪60年代地表水范围的百分之不到10%的百分比。在本文中,我们展示了使用土地表面温度(LST)数据的湖泊(包括开放水和泛滥植被的湖泊)总表面水域的延长记录(干燥季节1988-2016)(干燥季节2000-2016)从NASA Terra Modis传感器和基于Eumetsat Meteosat的LST测量(1988-2001的干燥季节)从早期的研究中。我们还使用雷达数据(2015-2016)从ESA Sentinel-1A任务中检查乍得湖的总面积水域。对于您(18个数据集)可用的有限数量的雷达数据集,我们在这些数据的估计和LST的估计之间的平均差异相匹配,尽管我们在使用这两种类型的估计中找到了空间差异数据。我们使用这些空间差异来调整Modis LST的记录(2000-2016)。然后我们使用调整的记录来消除来自Meteosat测量的现有LST记录(1988-2001的干燥季节)的偏置,并结合两个记录。从这个综合,延长记录,我们绘制了1988-1989至2016-2017的干燥季节的湖泊总面积水域。我们发现1988-1989至2016-2017的干燥季节,最大的湖泊总面积水域大约是16,800平方公里,km(2月和5月,2000年),湖泊的最低总面积水域约为6400 SQ.km(1990年11月),平均约为12,700平方公里..此外,在此期间,我们发现湖的总面积水域在这段时间内变化,平均每年增加约143平方公里。

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