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High-temporal-resolution water level and storage change data sets for lakes on the Tibetan Plateau during 2000–2017 using multiple altimetric missions and Landsat-derived lake shoreline positions

机译:使用多个测高任务和Landsat派生的湖岸线位置,在2000–2017年期间青藏高原湖泊的高分辨率水位和存储变化数据集

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Abstract. The Tibetan Plateau (TP), known as Asia's water tower, isquite sensitive to climate change, which is reflected by changes in hydrologic statevariables such as lake water storage. Given the extremely limited groundobservations on the TP due to the harsh environment and complex terrain, weexploited multiple altimetric missions and Landsat satellite data to createhigh-temporal-resolution lake water level and storage change time series atweekly to monthly timescales for 52 large lakes (50 lakes larger than 150 km~(2) and 2 lakes larger than 100 km~(2)) on the TP during 2000–2017. The data sets are available online at https://doi.org/10.1594/PANGAEA.898411 (Li et al., 2019). WithLandsat archives and altimetry data, we developed water levels from lakeshoreline positions (i.e., Landsat-derived water levels) that cover thestudy period and serve as an ideal reference for merging multisource lakewater levels with systematic biases being removed. To validate theLandsat-derived water levels, field experiments were carried out in twotypical lakes, and theoretical uncertainty analysis was performed based onhigh-resolution optical images (0.8 m) as well. The RMSE of theLandsat-derived water levels is 0.11 m compared with the in situmeasurements, consistent with the magnitude from theoretical analysis(0.1–0.2 m). The accuracy of the Landsat-derived water levels that can bederived in relatively small lakes is comparable with most altimetry data.The resulting merged Landsat-derived and altimetric lake water levels canprovide accurate information on multiyear and short-term monitoring of lakewater levels and storage changes on the TP, and critical information on lake overflow flood monitoring and prediction as the expansion of some TP lakesbecomes a serious threat to surrounding residents and infrastructure.
机译:抽象。青藏高原(TP)被称为亚洲的水塔,对气候变化相当敏感,这反映在诸如湖泊蓄水等水文状态变量的变化上。鉴于恶劣的环境和复杂的地形导致TP的地面观测极其有限,我们利用多个测高任务和Landsat卫星数据来创建每周52个大型湖泊(50个湖泊)的高时间分辨率湖水位和储量变化时间序列,从每周到每月在2000–2017年期间,TP上大于150 km〜(2)和2个大于100 km〜(2)的湖泊。数据集可在线访问https://doi.org/10.1594/PANGAEA.898411(Li等,2019)。借助Landsat档案和测高仪数据,我们从涵盖研究期间的湖岸线位置(即Landsat得出的水位)得出了水位,并为合并多源湖水位并消除了系统偏差提供了理想的参考。为了验证陆地卫星水位,在两个典型的湖泊中进行了野外实验,并基于高分辨率的光学图像(0.8 m)进行了理论不确定性分析。与实地测量相比,陆地卫星水位的均方根误差(RMSE)为0.11 m,与理论分析得出的幅度(0.1–0.2 m)一致。可以在相对较小的湖泊中得出的Landsat得出的水位精度与大多数测高仪的数据相当,由此得出的合并的Landsat得出的和高出的湖泊水位可以提供有关湖泊水位和储量变化的多年期和短期监测的准确信息TP上的信息,以及随着一些TP湖的扩张而对湖泊溢流洪水的监控和预报的重要信息,对周围居民和基础设施构成了严重威胁。

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