UAV-Based Quantification of Dynamic Lahar Channel Morphology at Volcán de Fuego, Guatemala

This study quantified erosional and depositional processes for secondary lahars in Las Lajas drainage at Volcán de Fuego, Guatemala, during the rainy season from May to October 2021. Abundant pyroclastic material from ongoing eruptive activity is remobilized seasonally during heavy precipitation, wh...

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Main Authors: Jerry C. Mock, Jeffrey B. Johnson, Armando Pineda, Gustavo Bejar, Amilcar Roca
Format: Article
Language:English
Published: MDPI AG 2023-07-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/15/15/3713
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author Jerry C. Mock
Jeffrey B. Johnson
Armando Pineda
Gustavo Bejar
Amilcar Roca
author_facet Jerry C. Mock
Jeffrey B. Johnson
Armando Pineda
Gustavo Bejar
Amilcar Roca
author_sort Jerry C. Mock
collection DOAJ
description This study quantified erosional and depositional processes for secondary lahars in Las Lajas drainage at Volcán de Fuego, Guatemala, during the rainy season from May to October 2021. Abundant pyroclastic material from ongoing eruptive activity is remobilized seasonally during heavy precipitation, which can impact infrastructure and populations living near Fuego. Our region of focus was in an agricultural zone 6 to 10 km from the summit, surveyed with an unoccupied aerial vehicle (UAV) quadcopter at monthly intervals. Imagery was processed into overlapping time-lapse structure from motion digital elevation models (DEMs). DEMs were differenced to find volumetric changes as a function of the channel flow path distance (quantified in 500 m sections) to track channel morphology changes over time. The largest measured volume changes were a 490 m<sup>3</sup>/day loss in the upper section (~6 km from summit) and a 440 m<sup>3</sup>/day gain in the lower sections (~10 km from summit). We discussed how the natural channel’s constriction and widening of Las Lajas in more distal sections control the behavior and stability of the stream evolution. Above the constriction, the channel is primarily downcutting and meandering within an old flood plain, which had been filled in by pyroclastic materials deposited by the June 2018 paroxysm.
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spelling doaj.art-cbd89dd0e36c4479a8bb1b8063541c622023-11-18T23:29:50ZengMDPI AGRemote Sensing2072-42922023-07-011515371310.3390/rs15153713UAV-Based Quantification of Dynamic Lahar Channel Morphology at Volcán de Fuego, GuatemalaJerry C. Mock0Jeffrey B. Johnson1Armando Pineda2Gustavo Bejar3Amilcar Roca4Department of Geosciences, Boise State University, Boise, ID 83725, USADepartment of Geosciences, Boise State University, Boise, ID 83725, USAIndependent Researcher, Guatemala City 01013, GuatemalaDepartment of Geological and Mining Engineering and Science, Michigan Technological University, Houghton, MI 49931, USAInstituto Nacional de Sismología, Vulcanologia, Meteorologia e Hidrología (INSIVUMEH), Guatemala City 01013, GuatemalaThis study quantified erosional and depositional processes for secondary lahars in Las Lajas drainage at Volcán de Fuego, Guatemala, during the rainy season from May to October 2021. Abundant pyroclastic material from ongoing eruptive activity is remobilized seasonally during heavy precipitation, which can impact infrastructure and populations living near Fuego. Our region of focus was in an agricultural zone 6 to 10 km from the summit, surveyed with an unoccupied aerial vehicle (UAV) quadcopter at monthly intervals. Imagery was processed into overlapping time-lapse structure from motion digital elevation models (DEMs). DEMs were differenced to find volumetric changes as a function of the channel flow path distance (quantified in 500 m sections) to track channel morphology changes over time. The largest measured volume changes were a 490 m<sup>3</sup>/day loss in the upper section (~6 km from summit) and a 440 m<sup>3</sup>/day gain in the lower sections (~10 km from summit). We discussed how the natural channel’s constriction and widening of Las Lajas in more distal sections control the behavior and stability of the stream evolution. Above the constriction, the channel is primarily downcutting and meandering within an old flood plain, which had been filled in by pyroclastic materials deposited by the June 2018 paroxysm.https://www.mdpi.com/2072-4292/15/15/3713DEMorthomosaicUAVvolcanolaharSfM
spellingShingle Jerry C. Mock
Jeffrey B. Johnson
Armando Pineda
Gustavo Bejar
Amilcar Roca
UAV-Based Quantification of Dynamic Lahar Channel Morphology at Volcán de Fuego, Guatemala
Remote Sensing
DEM
orthomosaic
UAV
volcano
lahar
SfM
title UAV-Based Quantification of Dynamic Lahar Channel Morphology at Volcán de Fuego, Guatemala
title_full UAV-Based Quantification of Dynamic Lahar Channel Morphology at Volcán de Fuego, Guatemala
title_fullStr UAV-Based Quantification of Dynamic Lahar Channel Morphology at Volcán de Fuego, Guatemala
title_full_unstemmed UAV-Based Quantification of Dynamic Lahar Channel Morphology at Volcán de Fuego, Guatemala
title_short UAV-Based Quantification of Dynamic Lahar Channel Morphology at Volcán de Fuego, Guatemala
title_sort uav based quantification of dynamic lahar channel morphology at volcan de fuego guatemala
topic DEM
orthomosaic
UAV
volcano
lahar
SfM
url https://www.mdpi.com/2072-4292/15/15/3713
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