基于卷积神经网络的数据稀疏环境下降雨诱发浅层滑坡自动检测方法

Roquia Salam , Filiberto Pla , Bayes Ahmed , Marco Painho
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引用次数: 0

摘要

在数据稀疏的地区探测降雨引起的浅层滑坡对于有效的滑坡灾害管理变得越来越重要。以前的研究主要集中在深层地震引发的滑坡的自动化方法上。本研究采用U-net卷积神经网络(CNN)模型,利用多时相、高分辨率PlanetScope(3米空间分辨率)、中分辨率Sentinel-2(10米空间分辨率)图像和alos - palsar提供的数字高程模型(DEM)检测降雨引起的浅层滑坡,从而解决了这一问题。创建了四个数据集:数据集A和B使用PlanetScope,数据集C和D使用Sentinel-2,数据集B和D也包括DEM数据。总共有181个人工圈定的滑坡多边形被用作地面真相掩模。每个数据集使用重复分层保留验证进行测试。性能指标包括精确度、召回率、F1分数、损失和准确性。结果表明,数据集A和B优于其他数据集;然而,将DEM与数据集B集成并没有提高模型的精度。数据集A和数据集b的最佳平均精度、召回率、F1分数、损失和准确度分别为1、0.625、0.625、0.380和0.999。该研究证明了U-net模型在全球不同地理和时间背景下检测降雨引起的浅层滑坡的潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Convolutional Neural Network-based approach for automatically detecting rainfall-induced shallow landslides in a data-sparse context
Detecting rainfall-induced shallow landslides in data-sparse regions has become increasingly important for effective landslides disaster management. Previous studies have predominantly focused on automated methods for deep-seated, earthquake-triggered landslides. This study addresses this gap by employing a U-net Convolutional Neural Network (CNN) model to detect rainfall-induced shallow landslides using multi-temporal, high-resolution PlanetScope (3m spatial resolution), medium-resolution Sentinel-2 (10m spatial resolution) imagery, and ALOS-PALSAR-provided digital elevation model (DEM). Four datasets were created: Datasets A and B using PlanetScope, and Datasets C and D using Sentinel-2, with Datasets B and D also including DEM data. A total of 181 manually delineated landslide polygons were used as ground truth masks. Each dataset was tested using repeated stratified hold-out validation. Performance metrics included precision, recall, F1 score, loss, and accuracy. Results indicated that Datasets A and B outperformed the others; however, integrating DEM with Dataset B did not enhance model accuracy. The best mean precision, recall, F1 score, loss, and accuracy were 1, 0.625, 0.625, 0.380, and 0.999, respectively, for both Datasets A and B. This study demonstrates the U-net model's potential for detecting rainfall-induced shallow landslides in various geographic and temporal contexts globally.
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