{"title":"Distributed estimation of surface sediment size in paraglacial and periglacial environments using drone photogrammetry","authors":"Gerardo Zegers, Masaki Hayashi, Alex Garcés","doi":"10.1002/esp.70093","DOIUrl":null,"url":null,"abstract":"<p>Grain-size analysis offers insights into geological processes and landform dynamics. Traditional grain-size sampling methods are labour intensive and offer limited spatial coverage, posing challenges in paraglacial and periglacial environments characterized by large spatial variability in sediment sizes. This study introduces a new workflow that combines structure-from-motion, image segmentation and texture-based optical granulometry techniques to estimate surface grain size in paraglacial and periglacial environments efficiently. Utilizing high-resolution orthomosaics (ground sampling distance <span></span><math>\n <semantics>\n <mrow>\n <mo>∼</mo>\n </mrow>\n <annotation>$$ \\sim $$</annotation>\n </semantics></math>8 mm) and Cellpose, a deep-learning image segmentation model, the new workflow achieves high-accuracy grain-size distributions (GSDs) with low errors. These GSDs, along with lower resolution orthomosaics (ground sampling distance <span></span><math>\n <semantics>\n <mrow>\n <mo>∼</mo>\n </mrow>\n <annotation>$$ \\sim $$</annotation>\n </semantics></math>30 mm), are used to train SediNet—a machine-learning framework—to predict GSDs accurately from <span></span><math>\n <semantics>\n <mrow>\n <mn>340</mn>\n <mo>×</mo>\n <mn>340</mn>\n </mrow>\n <annotation>$$ 340\\times 340 $$</annotation>\n </semantics></math> pixel tiles. Tested across six alpine basins in the Canadian Rockies and a rock glacier in Italy, the model demonstrates effectiveness and accuracy, promising advancements in geoscientific research and the understanding of paraglacial and periglacial dynamics.</p>","PeriodicalId":11408,"journal":{"name":"Earth Surface Processes and Landforms","volume":"50 7","pages":""},"PeriodicalIF":2.8000,"publicationDate":"2025-06-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/esp.70093","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Earth Surface Processes and Landforms","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/esp.70093","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
引用次数: 0
Abstract
Grain-size analysis offers insights into geological processes and landform dynamics. Traditional grain-size sampling methods are labour intensive and offer limited spatial coverage, posing challenges in paraglacial and periglacial environments characterized by large spatial variability in sediment sizes. This study introduces a new workflow that combines structure-from-motion, image segmentation and texture-based optical granulometry techniques to estimate surface grain size in paraglacial and periglacial environments efficiently. Utilizing high-resolution orthomosaics (ground sampling distance 8 mm) and Cellpose, a deep-learning image segmentation model, the new workflow achieves high-accuracy grain-size distributions (GSDs) with low errors. These GSDs, along with lower resolution orthomosaics (ground sampling distance 30 mm), are used to train SediNet—a machine-learning framework—to predict GSDs accurately from pixel tiles. Tested across six alpine basins in the Canadian Rockies and a rock glacier in Italy, the model demonstrates effectiveness and accuracy, promising advancements in geoscientific research and the understanding of paraglacial and periglacial dynamics.
期刊介绍:
Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with:
the interactions between surface processes and landforms and landscapes;
that lead to physical, chemical and biological changes; and which in turn create;
current landscapes and the geological record of past landscapes.
Its focus is core to both physical geographical and geological communities, and also the wider geosciences