Modeling 3D Free-geometry Volumetric Sources Associated to Geological and Anthropogenic Hazards from Space and Terrestrial Geodetic Data

Recent decades have shown an explosion in the quantity and quality of geodetic data, mainly space-based geodetic data, that are being applied to geological and anthropogenic hazards. This has produced the need for new approaches for analyzing, modeling and interpreting these geodetic data. Typically...

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Main Authors: Antonio G. Camacho, José Fernández
Format: Article
Language:English
Published: MDPI AG 2019-08-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/11/17/2042
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spelling doaj-b8e6d5834dad4a7fac3bb2c299f68f3f2020-11-25T01:46:07ZengMDPI AGRemote Sensing2072-42922019-08-011117204210.3390/rs11172042rs11172042Modeling 3D Free-geometry Volumetric Sources Associated to Geological and Anthropogenic Hazards from Space and Terrestrial Geodetic DataAntonio G. Camacho0José Fernández1Institute of Geosciences (CSIC-UCM), C/ Doctor Severo Ochoa, 7, Facultad de Medicina (Edificio entrepabellones 7 y 8, 4a planta), Ciudad Universitaria, 28040 Madrid, SpainInstitute of Geosciences (CSIC-UCM), C/ Doctor Severo Ochoa, 7, Facultad de Medicina (Edificio entrepabellones 7 y 8, 4a planta), Ciudad Universitaria, 28040 Madrid, SpainRecent decades have shown an explosion in the quantity and quality of geodetic data, mainly space-based geodetic data, that are being applied to geological and anthropogenic hazards. This has produced the need for new approaches for analyzing, modeling and interpreting these geodetic data. Typically, modeling of deformation and gravity changes follows an inverse approach using analytical or numerical solutions, where normally regular geometries (point sources, disks, prolate or oblate spheroids, etc.) are assumed at the initial stages and the inversion is carried out in a linear context. Here we review an original methodology for the simultaneous, nonlinear inversion of gravity changes and/or surface deformation (measured with different techniques) to determine 3D (three-dimensional) bodies, without any a priori assumption about their geometries, embedded into an elastic or poroelastic medium. Such a fully nonlinear inversion has led to interesting results in volcanic environments and in the study of water tables variation due to its exploitation. This methodology can be used to invert geodetic remote sensing data or terrestrial data alone, or in combination.https://www.mdpi.com/2072-4292/11/17/2042inversion technique3D modelsfree-geometrysurface deformationearth observation dataterrestrial geodetic datahazards
collection DOAJ
language English
format Article
sources DOAJ
author Antonio G. Camacho
José Fernández
spellingShingle Antonio G. Camacho
José Fernández
Modeling 3D Free-geometry Volumetric Sources Associated to Geological and Anthropogenic Hazards from Space and Terrestrial Geodetic Data
Remote Sensing
inversion technique
3D models
free-geometry
surface deformation
earth observation data
terrestrial geodetic data
hazards
author_facet Antonio G. Camacho
José Fernández
author_sort Antonio G. Camacho
title Modeling 3D Free-geometry Volumetric Sources Associated to Geological and Anthropogenic Hazards from Space and Terrestrial Geodetic Data
title_short Modeling 3D Free-geometry Volumetric Sources Associated to Geological and Anthropogenic Hazards from Space and Terrestrial Geodetic Data
title_full Modeling 3D Free-geometry Volumetric Sources Associated to Geological and Anthropogenic Hazards from Space and Terrestrial Geodetic Data
title_fullStr Modeling 3D Free-geometry Volumetric Sources Associated to Geological and Anthropogenic Hazards from Space and Terrestrial Geodetic Data
title_full_unstemmed Modeling 3D Free-geometry Volumetric Sources Associated to Geological and Anthropogenic Hazards from Space and Terrestrial Geodetic Data
title_sort modeling 3d free-geometry volumetric sources associated to geological and anthropogenic hazards from space and terrestrial geodetic data
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2019-08-01
description Recent decades have shown an explosion in the quantity and quality of geodetic data, mainly space-based geodetic data, that are being applied to geological and anthropogenic hazards. This has produced the need for new approaches for analyzing, modeling and interpreting these geodetic data. Typically, modeling of deformation and gravity changes follows an inverse approach using analytical or numerical solutions, where normally regular geometries (point sources, disks, prolate or oblate spheroids, etc.) are assumed at the initial stages and the inversion is carried out in a linear context. Here we review an original methodology for the simultaneous, nonlinear inversion of gravity changes and/or surface deformation (measured with different techniques) to determine 3D (three-dimensional) bodies, without any a priori assumption about their geometries, embedded into an elastic or poroelastic medium. Such a fully nonlinear inversion has led to interesting results in volcanic environments and in the study of water tables variation due to its exploitation. This methodology can be used to invert geodetic remote sensing data or terrestrial data alone, or in combination.
topic inversion technique
3D models
free-geometry
surface deformation
earth observation data
terrestrial geodetic data
hazards
url https://www.mdpi.com/2072-4292/11/17/2042
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