Abstract

Glacial lakes are an important component of the cryosphere in the Tibetan Plateau. In response to climate warming, they threaten the downstream lives, ecological environment, and public infrastructures through outburst floods within a short time. Although most of the efforts have been made toward extracting glacial lake outlines and detect their changes with remotely sensed images, the temporal frequency and spatial resolution of glacial lake datasets are generally not fine enough to reflect the detailed processes of glacial lake dynamics, especially for potentially dangerous glacial lakes with high-frequency variability. By using full time-series Sentinel-1A/1B imagery over a year, this study presents a new systematic method to extract the glacial lake outlines that have a fast variability in the southeastern Tibetan Plateau with a time interval of six days. Our approach was based on a level-set segmentation, combined with a median pixel composition of synthetic aperture radar (SAR) backscattering coefficients stacked as a regularization term, to robustly estimate the lake extent across the observed time range. The mapping results were validated against manually digitized lake outlines derived from Gaofen-2 panchromatic multi-spectral (GF-2 PMS) imagery, with an overall accuracy and kappa coefficient of 96.54% and 0.95, respectively. In comparison with results from classical supervised support vector machine (SVM) and unsupervised Iterative Self-Organizing Data Analysis Technique Algorithm (ISODATA) methods, the proposed method proved to be much more robust and effective at detecting glacial lakes with irregular boundaries that have similar backscattering as the surroundings. This study also demonstrated the feasibility of time-series Sentinel-1A/1B SAR data in the continuous monitoring of glacial lake outline dynamics.

Highlights

  • Glacial lakes are important indicators of the regional glacier dynamics in response to climate warming and changing precipitation [1,2,3]

  • The validation conducted on alarge totaland of 283 glaciallakes lakeswere that were covered the area of it GFGF-2 imagery

  • These results suggest that the combination of the time series of Sentinel-1A/1B synthetic aperture radar (SAR). Both abundant rainfall and glacier meltwater (Figure 7b,c). These results suggest that the combination imagery and the median composite mapping method would provide reliable and accurate information of the time series of Sentinel-1A/1B SAR imagery and the median composite mapping method would of the temporal evolution of glacial lakes over the large and rugged alpine areas, and allow for the provide reliable and accurate information of the temporal evolution of glacial lakes over the large identification of potentially dangerous glacial lakes

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Summary

Introduction

Glacial lakes are important indicators of the regional glacier dynamics in response to climate warming and changing precipitation [1,2,3]. With the continuous retreating and thinning of mountain glaciers in the Tibetan Plateau, a large number of glacial lakes have developed and experienced rapid expansion in recent decades, leading to the increased hazard risk of glacial lake outburst floods (GLOFs) [4]. These GLOFs usually evolve and erupt over a short time and can trace long distances from high altitude regions, which will pose a great threat to the life and property in the downstream valleys [5,6]. Public Health 2020, 17, 1072; doi:10.3390/ijerph17031072 www.mdpi.com/journal/ijerph

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