Retrogressive thaw slumps recognition and occurrence analysis using deep learning with satellite remote sensing in the central Qinghai-Tibet Plateau

IF 3.1 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL Geomorphology Pub Date : 2025-02-15 Epub Date: 2024-12-15 DOI:10.1016/j.geomorph.2024.109581
Fan Wu , Chaowei Jiang , Chao Wang , Lichuan Zou , Tianyang Li , Shaoyang Guan , Yixian Tang
{"title":"Retrogressive thaw slumps recognition and occurrence analysis using deep learning with satellite remote sensing in the central Qinghai-Tibet Plateau","authors":"Fan Wu ,&nbsp;Chaowei Jiang ,&nbsp;Chao Wang ,&nbsp;Lichuan Zou ,&nbsp;Tianyang Li ,&nbsp;Shaoyang Guan ,&nbsp;Yixian Tang","doi":"10.1016/j.geomorph.2024.109581","DOIUrl":null,"url":null,"abstract":"<div><div>Due to permafrost degradation, retrogressive thaw slumps (RTSs) have increasingly occurred in the past decade, altering landscape patterns and ecological environments in permafrost regions while accelerating soil carbon emissions. This study introduces a framework for RTS recognition and occurrence analysis based on deep learning and change analysis techniques. We propose a hybrid convolution and transformer neural network (HCT-Net) to recognize RTSs automatically. The network employs Synthetic Aperture Radar (SAR) and optical imagery for RTS detection. To effectively integrate the feature extraction capabilities of Convolutional Neural Network (CNN) and Vision Transformer (ViT), a Cross Feature Fusion Module (CFFM) has been developed. With the generated RTS map, Landsat series satellite images spanning from 2001 to 2023 were acquired for long-term observation and analysis of RTSs evolution. The occurrence years of detected RTSs were estimated employing the LandTrendr model, enabling a year-to-year dynamics analysis of RTS development. Focusing on the central Qinghai-Tibet Plateau (QTP), including the Beiluhe basin, Hoh Xil Hill, and Mt. Fenghuo area, covering approximately 49,000 km<sup>2</sup>, experiments have been conducted for RTS recognition and multi-temporal analysis. Results demonstrate that the proposed method achieves an Intersection over Union (IOU) and F1 score of 72.95 % and 88.30 % for RTS recognition, outperforming other semantic segmentation methods such as Deeplabv3+, Segformer, UNet, and Swin-UNet. Based on the RTSs detected within the study area during 2001–2023, the occurrence year of the RTSs was estimated. The findings reveal a continuous expansion of RTSs since 2001 and confirm concentrated outbreaks in the years 2010 and 2016. The proposed framework offers a good approach for RTSs recognition and analysis, which can support further research into permafrost degradation.</div></div>","PeriodicalId":55115,"journal":{"name":"Geomorphology","volume":"471 ","pages":"Article 109581"},"PeriodicalIF":3.1000,"publicationDate":"2025-02-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geomorphology","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0169555X24005336","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"2024/12/15 0:00:00","PubModel":"Epub","JCR":"Q2","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
引用次数: 0

Abstract

Due to permafrost degradation, retrogressive thaw slumps (RTSs) have increasingly occurred in the past decade, altering landscape patterns and ecological environments in permafrost regions while accelerating soil carbon emissions. This study introduces a framework for RTS recognition and occurrence analysis based on deep learning and change analysis techniques. We propose a hybrid convolution and transformer neural network (HCT-Net) to recognize RTSs automatically. The network employs Synthetic Aperture Radar (SAR) and optical imagery for RTS detection. To effectively integrate the feature extraction capabilities of Convolutional Neural Network (CNN) and Vision Transformer (ViT), a Cross Feature Fusion Module (CFFM) has been developed. With the generated RTS map, Landsat series satellite images spanning from 2001 to 2023 were acquired for long-term observation and analysis of RTSs evolution. The occurrence years of detected RTSs were estimated employing the LandTrendr model, enabling a year-to-year dynamics analysis of RTS development. Focusing on the central Qinghai-Tibet Plateau (QTP), including the Beiluhe basin, Hoh Xil Hill, and Mt. Fenghuo area, covering approximately 49,000 km2, experiments have been conducted for RTS recognition and multi-temporal analysis. Results demonstrate that the proposed method achieves an Intersection over Union (IOU) and F1 score of 72.95 % and 88.30 % for RTS recognition, outperforming other semantic segmentation methods such as Deeplabv3+, Segformer, UNet, and Swin-UNet. Based on the RTSs detected within the study area during 2001–2023, the occurrence year of the RTSs was estimated. The findings reveal a continuous expansion of RTSs since 2001 and confirm concentrated outbreaks in the years 2010 and 2016. The proposed framework offers a good approach for RTSs recognition and analysis, which can support further research into permafrost degradation.

Abstract Image

查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
基于深度学习的青藏高原中部退行性融雪滑坡识别与发生分析
近十年来,由于多年冻土退化,退行性融化滑坡(RTSs)日益增多,改变了多年冻土区的景观格局和生态环境,同时加速了土壤碳的排放。本研究介绍了一个基于深度学习和变化分析技术的RTS识别和发生分析框架。我们提出了一种混合卷积和变压器神经网络(HCT-Net)来自动识别rts。该网络采用合成孔径雷达(SAR)和光学图像进行RTS检测。为了有效地整合卷积神经网络(CNN)和视觉变压器(ViT)的特征提取能力,开发了一种交叉特征融合模块(CFFM)。利用生成的RTS地图,获取2001 - 2023年的Landsat系列卫星图像,对RTS的演变进行长期观测和分析。使用LandTrendr模型估计了检测到的RTS的发生年份,从而实现了RTS发展的逐年动态分析。以青藏高原中部包括北麓河盆地、鹤西山和烽火山地区约49,000 km2的区域为研究对象,开展了RTS识别和多时相分析实验。结果表明,该方法对RTS识别的IOU和F1分值分别为72.95%和88.30%,优于Deeplabv3+、Segformer、UNet和swun -UNet等其他语义分割方法。根据2001-2023年研究区检测到的RTSs,估计了RTSs的发生年份。调查结果显示,自2001年以来,RTSs持续扩大,并证实了2010年和2016年的集中暴发。该框架为冻土退化的识别和分析提供了良好的方法,为进一步研究冻土退化提供了支持。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
Geomorphology
Geomorphology 地学-地球科学综合
CiteScore
8.00
自引率
10.30%
发文量
309
审稿时长
3.4 months
期刊介绍: Our journal''s scope includes geomorphic themes of: tectonics and regional structure; glacial processes and landforms; fluvial sequences, Quaternary environmental change and dating; fluvial processes and landforms; mass movement, slopes and periglacial processes; hillslopes and soil erosion; weathering, karst and soils; aeolian processes and landforms, coastal dunes and arid environments; coastal and marine processes, estuaries and lakes; modelling, theoretical and quantitative geomorphology; DEM, GIS and remote sensing methods and applications; hazards, applied and planetary geomorphology; and volcanics.
期刊最新文献
Climate-driven drainage reorganization and fluvial incision in the Huangshui River Basin, northeastern Tibetan Plateau Ice-dammed lakes, outburst floods, and formation of the Gaccetávži ravine in Finnmark, NE Norway Large rock slope deformations: Evidence of orogen-scale distribution from an original inventory in central Apennines (Italy) Gully system evolution in volcanic environments through digital elevation model comparisons: A case study from La Fossa Cone (Vulcano Island, Sicily) Morphologic adjustment and sediment balance of the Nile River in Egypt under cascade dam regulation
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1