Criteria for the optimal selection of remote sensing optical images to map event landslides

Landslides leave discernible signs on the land surface, most of which can be captured in remote sensing images. Trained geomorphologists analyse remote sensing images and map landslides through heuristic interpretation of photographic and morphological characteristics. Despite a wide use of remot...

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Main Authors: F. Fiorucci, D. Giordan, M. Santangelo, F. Dutto, M. Rossi, F. Guzzetti
Format: Article
Language:English
Published: Copernicus Publications 2018-01-01
Series:Natural Hazards and Earth System Sciences
Online Access:https://www.nat-hazards-earth-syst-sci.net/18/405/2018/nhess-18-405-2018.pdf
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spelling doaj-82bc8587fabb455295654f36eb711f672020-11-24T22:15:46ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812018-01-011840541710.5194/nhess-18-405-2018Criteria for the optimal selection of remote sensing optical images to map event landslidesF. Fiorucci0D. Giordan1M. Santangelo2F. Dutto3M. Rossi4F. Guzzetti5Istituto di Ricerca per la Protezione Idrogeologica, Consiglio Nazionale delle Ricerche, via della Madonna Alta 126, 06128 Perugia, ItalyIstituto di Ricerca per la Protezione Idrogeologica, Consiglio Nazionale delle Ricerche, Strada delle Cacce 73, 10135 Turin, ItalyIstituto di Ricerca per la Protezione Idrogeologica, Consiglio Nazionale delle Ricerche, via della Madonna Alta 126, 06128 Perugia, ItalyServizio Protezione Civile della Città Metropolitana di Torino, Via Alberto Sordi 13, 10095 Grugliasco, ItalyIstituto di Ricerca per la Protezione Idrogeologica, Consiglio Nazionale delle Ricerche, via della Madonna Alta 126, 06128 Perugia, ItalyIstituto di Ricerca per la Protezione Idrogeologica, Consiglio Nazionale delle Ricerche, via della Madonna Alta 126, 06128 Perugia, ItalyLandslides leave discernible signs on the land surface, most of which can be captured in remote sensing images. Trained geomorphologists analyse remote sensing images and map landslides through heuristic interpretation of photographic and morphological characteristics. Despite a wide use of remote sensing images for landslide mapping, no attempt to evaluate how the image characteristics influence landslide identification and mapping exists. This paper presents an experiment to determine the effects of optical image characteristics, such as spatial resolution, spectral content and image type (monoscopic or stereoscopic), on landslide mapping. We considered eight maps of the same landslide in central Italy: (i) six maps obtained through expert heuristic visual interpretation of remote sensing images, (ii) one map through a reconnaissance field survey, and (iii) one map obtained through a real-time kinematic (RTK) differential global positioning system (dGPS) survey, which served as a benchmark. The eight maps were compared pairwise and to a benchmark. The mismatch between each map pair was quantified by the error index, <i>E</i>. Results show that the map closest to the benchmark delineation of the landslide was obtained using the higher resolution image, where the landslide signature was primarily photographical (in the landslide source and transport area). Conversely, where the landslide signature was mainly morphological (in the landslide deposit) the best mapping result was obtained using the stereoscopic images. Albeit conducted on a single landslide, the experiment results are general, and provide useful information to decide on the optimal imagery for the production of event, seasonal and multi-temporal landslide inventory maps.https://www.nat-hazards-earth-syst-sci.net/18/405/2018/nhess-18-405-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author F. Fiorucci
D. Giordan
M. Santangelo
F. Dutto
M. Rossi
F. Guzzetti
spellingShingle F. Fiorucci
D. Giordan
M. Santangelo
F. Dutto
M. Rossi
F. Guzzetti
Criteria for the optimal selection of remote sensing optical images to map event landslides
Natural Hazards and Earth System Sciences
author_facet F. Fiorucci
D. Giordan
M. Santangelo
F. Dutto
M. Rossi
F. Guzzetti
author_sort F. Fiorucci
title Criteria for the optimal selection of remote sensing optical images to map event landslides
title_short Criteria for the optimal selection of remote sensing optical images to map event landslides
title_full Criteria for the optimal selection of remote sensing optical images to map event landslides
title_fullStr Criteria for the optimal selection of remote sensing optical images to map event landslides
title_full_unstemmed Criteria for the optimal selection of remote sensing optical images to map event landslides
title_sort criteria for the optimal selection of remote sensing optical images to map event landslides
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2018-01-01
description Landslides leave discernible signs on the land surface, most of which can be captured in remote sensing images. Trained geomorphologists analyse remote sensing images and map landslides through heuristic interpretation of photographic and morphological characteristics. Despite a wide use of remote sensing images for landslide mapping, no attempt to evaluate how the image characteristics influence landslide identification and mapping exists. This paper presents an experiment to determine the effects of optical image characteristics, such as spatial resolution, spectral content and image type (monoscopic or stereoscopic), on landslide mapping. We considered eight maps of the same landslide in central Italy: (i) six maps obtained through expert heuristic visual interpretation of remote sensing images, (ii) one map through a reconnaissance field survey, and (iii) one map obtained through a real-time kinematic (RTK) differential global positioning system (dGPS) survey, which served as a benchmark. The eight maps were compared pairwise and to a benchmark. The mismatch between each map pair was quantified by the error index, <i>E</i>. Results show that the map closest to the benchmark delineation of the landslide was obtained using the higher resolution image, where the landslide signature was primarily photographical (in the landslide source and transport area). Conversely, where the landslide signature was mainly morphological (in the landslide deposit) the best mapping result was obtained using the stereoscopic images. Albeit conducted on a single landslide, the experiment results are general, and provide useful information to decide on the optimal imagery for the production of event, seasonal and multi-temporal landslide inventory maps.
url https://www.nat-hazards-earth-syst-sci.net/18/405/2018/nhess-18-405-2018.pdf
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