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Water level, areal extent and volume change of Lake Tanganyika, Lake Turkana, Lake Tonle Sap and Lake Constance: Multi-year time series from satellite altimetry and remote sensing

机译:坦噶尼喀湖,图尔卡纳湖,洞里萨湖和康斯坦茨湖的水位,面积和体积变化:卫星测高和遥感的多年时间序列

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摘要

This dataset contains time series of the water level, the areal extent and the volume change of the four large lakes Tanganyika, Turkana, Tonle Sap and Constance. For each lake, the time series cover a time-span of many years at a variable temporal resolution between several days and approximately one month: Lake Tanganyika: October 1992 - February 2015 Lake Turkana: October 1992 - September 2017 Lake Tonle Sap: June 2002 - September 2017 Lake Constance: July 2002 - May 2016 The data are based on satellite observations. Lake levels have been estimated from multi-mission satellite altimetry within DGFI-TUM's Database for Hydrological Time Series of Inland Waters (DAHITI; Schwatke et al., 2015). The areal extent of the water bodies has been derived from optical remote sensing data (Landsat 7/8 images with land/water classification). The relation between water level, areal extent and water volume change has been analyzed for these four lakes in the frame of the related DFG-project WLDYN (Assessing the spatiotemporal dynamics of water volumes in large wetlands and lakes by combining remote sensing with macro-scale hydrological modelling; grant No. SE 1916/4-1). Except for Lake Constance, where the change in areal extent was not mensurable in Landsat images, a linear relationship between water level and areal extent was found for the lakes in this data set. Based on this linear relationship, the areal extent of the lakes Tanganyika, Turkana and Tonle Saphas been interpolated to unobserved epochs. Changed in water volume were subsequently computed from combining water level and areal extent via the so-called truncated pyramid approach.
机译:该数据集包含四个大型湖泊坦any尼喀,图尔卡纳,洞里萨湖和康斯坦斯的水位,面积和体积变化的时间序列。对于每个湖泊,时间序列涵盖了数年至一个月之间不同时间分辨率的多年时间跨度:坦any尼喀湖:1992年10月至2015年2月图尔卡纳湖:1992年10月至2017年9月洞里萨湖(2002年6月) -2017年9月博登湖:2002年7月-2016年5月数据基于卫星观测值。湖泊水位是根据DGFI-TUM内陆水文时间序列数据库中的多任务卫星测高法估算的(DAHITI; Schwatke等人,2015)。水体的面积范围已从光学遥感数据(具有陆地/水分类的Landsat 7/8图像)得出。在相关的DFG项目WLDYN(通过结合遥感与宏观尺度评估大型湿地和湖泊中水量的时空动态)的框架内,分析了这四个湖泊的水位,面积范围和水量变化之间的关系。水文模型;授权号SE 1916 / 4-1)。除了康斯坦茨湖以外,在Landsat影像中无法确定面积的变化,在此数据集中发现了湖泊的水位与面积之间的线性关系。基于这种线性关系,将坦any尼喀湖,图尔卡纳湖和洞里萨法斯湖的面积范围内插到未观测到的时代。随后通过所谓的截顶金字塔方法,通过结合水位和面积来计算水量的变化。

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