Key Laboratory of Watershed Geographic Sciences, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China.
University of Chinese Academy of Sciences, Beijing 100049, China.
Sensors (Basel). 2019 Sep 30;19(19):4247. doi: 10.3390/s19194247.
Inland lakes are essential components of hydrological and biogeochemical water cycles, as well as indispensable water resources for human beings. To derive the long-term and continuous trajectory of lake inundation area changes is increasingly significant. Since it helps to understand how they function in the global water cycle and how they are impacted by climate change and human activities. Employing optical satellite images, as an important means of lake mapping, has been widely used in the monitoring of lakes. It is well known that one of the obvious difficulties of traditional remote sensing-based mapping methods lies in the tremendous labor and computing costs for delineating the large lakes (e.g., Caspian Sea). In this study, a novel approach of reconstructing long-term and high-frequency time series of inundation areas of large lakes is proposed. The general idea of this method is to obtain the lake inundation area at any specific observation date by referring to the mapping relationship of the water occurrence frequency (WOF) of the selected shoreline segment at relatively slight terrains and lake areas based on the pre-established lookup table. The lookup table to map the links of the WOF and lake areas is derived from the Joint Research Centre (JRC)Global Surface Water (GSW) dataset accessed in Google Earth Engine (GEE). We select five large lakes worldwide to reconstruct their long time series (1984-2018) of inundation areas using this method. The time series of lake volume variation are analyzed, and the qualitative investigations of these lake changes are eventually discussed by referring to previous studies. The results based on the case of North Aral Sea show that the mean relative error between estimated area and actually mapped value is about 0.85%. The mean R of all the five lakes is 0.746, which indicates that the proposed method can produce the robust estimates of area time series for these large lakes. This research sheds new light on mapping large lakes at considerably deducted time and labor costs, and be effectively applicable in other large lakes in regional and global scales.
内陆湖泊是水文和生物地球化学水循环的重要组成部分,也是人类不可或缺的水资源。推求湖泊淹没区的长期连续变化轨迹,对于了解它们在全球水循环中的功能以及它们如何受到气候变化和人类活动的影响越来越重要。利用光学卫星图像作为湖泊测绘的重要手段,已广泛应用于湖泊监测。众所周知,传统基于遥感的测绘方法的一个明显难点在于描绘大型湖泊(如里海)的巨大劳动力和计算成本。在本研究中,提出了一种新的大型湖泊长期高频淹没区时间序列重建方法。该方法的基本思想是通过参考基于 Google Earth Engine (GEE) 中访问的联合研究中心(JRC)全球地表水(GSW)数据集建立的预设定查找表,根据所选岸线段的水出现频率(WOF)的测绘关系,获得任意特定观测日期的湖泊淹没区。该查找表用于映射 WOF 和湖泊区域的链接。我们选择了全球的五个大型湖泊,用这种方法来重建它们的长时间序列(1984-2018 年)的淹没区。分析了湖泊体积变化的时间序列,并通过参考以前的研究,最终讨论了这些湖泊变化的定性研究。基于咸海北部的案例研究结果表明,估计面积与实际测绘值之间的平均相对误差约为 0.85%。五个湖泊的平均 R 值为 0.746,这表明该方法可以为这些大型湖泊的面积时间序列提供稳健的估计。本研究为在大大减少时间和劳动力成本的情况下测绘大型湖泊提供了新的思路,并可在区域和全球范围内有效地应用于其他大型湖泊。