Abstract

Glaciers in High Mountain Asia (HMA) have a significant impact on human activity. Thus, a detailed and up-to-date inventory of glaciers is crucial, along with monitoring them regularly. The identification of debris-covered glaciers is a fundamental and yet challenging component of research into glacier change and water resources, but it is limited by spectral similarities with surrounding bedrock, snow-affected areas, and mountain-shadowed areas, along with issues related to manual discrimination. Therefore, to use fewer human, material, and financial resources, it is necessary to develop better methods to determine the boundaries of debris-covered glaciers. This study focused on debris-covered glacier mapping using a combination of related technologies such as random forest (RF) and convolutional neural network (CNN) models. The models were tested on Landsat 8 Operational Land Imager (OLI)/Thermal Infrared Sensor (TIRS) data and the Advanced Spaceborne Thermal Emission and Reflection Radiometer Global Digital Elevation Model (ASTER GDEM), selecting Eastern Pamir and Nyainqentanglha as typical glacier areas on the Tibetan Plateau to construct a glacier classification system. The performances of different classifiers were compared, the different classifier construction strategies were optimized, and multiple single-classifier outputs were obtained with slight differences. Using the relationship between the surface area covered by debris and the machine learning model parameters, it was found that the debris coverage directly determined the performance of the machine learning model and mitigated the issues affecting the detection of active and inactive debris-covered glaciers. Various classification models were integrated to ascertain the best model for the classification of glaciers.

Highlights

  • Glacier changes have significant effects on the local climate, ecological environment, water resources, and sea-level rise [1,2,3]

  • The convolutional neural network (CNN) model performance dropped sharply initially, but it soon returned to its original level

  • The accuracy rate of the models that we trained (RF, CNN, and random forest (RF)–CNN) is extremely close to 100% (Figures 8–10), which directly indicates that the constructed model is suitable for the classification of debris-covered glaciers

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Summary

Introduction

Glacier changes have significant effects on the local climate, ecological environment, water resources, and sea-level rise [1,2,3]. From the perspective of global warming, the average temperature of High Mountain Asia (HMA) [4,5]—a region that has the largest number of glaciers (95,500) and ice reserves (7.02 ± 1.82 × 103 km3 ) outside of the polar regions [6]—has risen [7,8]. This has put the Qinghai–Tibet Plateau in a state of negative energy balance on the surface, causing most glaciers to retreat [9,10]. Through the study of glacier changes, it is possible to ascertain glacier dynamics [14], which has significant research value for understanding past glacial behavior and predicting future climate, environmental, and water resource changes [15]

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