Combining Ground Penetrating Radar and Frequency Domain Electromagnetic Surveys to Characterize the Structure of the Calderone Glacieret (Gran Sasso d’Italia, Italy)

Ice is a rich reservoir of past climate information, and the well-documented increasing rate of glacier retreat represents a great loss for paleoclimate studies. In this framework, the Ice Memory project aims to extract and analyze ice cores from glacier regions worldwide and store them in Antarctic...

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Published in:Remote Sensing
Main Authors: Mirko Pavoni, Jacopo Boaga, Alberto Carrera, Stefano Urbini, Fabrizio de Blasi, Jacopo Gabrieli
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/rs15102615
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author Mirko Pavoni
Jacopo Boaga
Alberto Carrera
Stefano Urbini
Fabrizio de Blasi
Jacopo Gabrieli
author_facet Mirko Pavoni
Jacopo Boaga
Alberto Carrera
Stefano Urbini
Fabrizio de Blasi
Jacopo Gabrieli
author_sort Mirko Pavoni
collection MDPI Open Access Publishing
container_issue 10
container_start_page 2615
container_title Remote Sensing
container_volume 15
description Ice is a rich reservoir of past climate information, and the well-documented increasing rate of glacier retreat represents a great loss for paleoclimate studies. In this framework, the Ice Memory project aims to extract and analyze ice cores from glacier regions worldwide and store them in Antarctica as a heritage record for future generations of scientists. Ice coring projects usually require a focused geophysical investigation, often based on Ground Penetrating Radar (GPR) prospecting to assess the most suitable drilling positions. As a novel approach in the Calderone Glacieret, we integrated the GPR method with Frequency Domain Electromagnetic (FDEM) surveys, a technique not commonly applied in the glacial environment. We used a separated-coils FDEM instrument to characterize the glacieret structure. The acquired FDEM datasets were inverted and compared to the GPR data and borehole information. The results demonstrated the capability of the FDEM technique to define the structure of the glacieret correctly; therefore, the potential to be applied in frozen subsoil environments. This opens new perspectives for the use of the FDEM technique to characterize periglacial environments, such as rock glaciers, where the coarse-blocky surface hinders data acquisition and enhances the problem of signal scattering.
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spelling ftmdpi:oai:mdpi.com:/2072-4292/15/10/2615/ 2025-01-16T19:39:10+00:00 Combining Ground Penetrating Radar and Frequency Domain Electromagnetic Surveys to Characterize the Structure of the Calderone Glacieret (Gran Sasso d’Italia, Italy) Mirko Pavoni Jacopo Boaga Alberto Carrera Stefano Urbini Fabrizio de Blasi Jacopo Gabrieli agris 2023-05-17 application/pdf https://doi.org/10.3390/rs15102615 EN eng Multidisciplinary Digital Publishing Institute Environmental Remote Sensing https://dx.doi.org/10.3390/rs15102615 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 15; Issue 10; Pages: 2615 FDEM EMI GPR Calderone Glacieret cryosphere environmental geophysics Text 2023 ftmdpi https://doi.org/10.3390/rs15102615 2023-08-01T10:06:55Z Ice is a rich reservoir of past climate information, and the well-documented increasing rate of glacier retreat represents a great loss for paleoclimate studies. In this framework, the Ice Memory project aims to extract and analyze ice cores from glacier regions worldwide and store them in Antarctica as a heritage record for future generations of scientists. Ice coring projects usually require a focused geophysical investigation, often based on Ground Penetrating Radar (GPR) prospecting to assess the most suitable drilling positions. As a novel approach in the Calderone Glacieret, we integrated the GPR method with Frequency Domain Electromagnetic (FDEM) surveys, a technique not commonly applied in the glacial environment. We used a separated-coils FDEM instrument to characterize the glacieret structure. The acquired FDEM datasets were inverted and compared to the GPR data and borehole information. The results demonstrated the capability of the FDEM technique to define the structure of the glacieret correctly; therefore, the potential to be applied in frozen subsoil environments. This opens new perspectives for the use of the FDEM technique to characterize periglacial environments, such as rock glaciers, where the coarse-blocky surface hinders data acquisition and enhances the problem of signal scattering. Text Antarc* Antarctica MDPI Open Access Publishing Remote Sensing 15 10 2615
spellingShingle FDEM
EMI
GPR
Calderone Glacieret
cryosphere
environmental geophysics
Mirko Pavoni
Jacopo Boaga
Alberto Carrera
Stefano Urbini
Fabrizio de Blasi
Jacopo Gabrieli
Combining Ground Penetrating Radar and Frequency Domain Electromagnetic Surveys to Characterize the Structure of the Calderone Glacieret (Gran Sasso d’Italia, Italy)
title Combining Ground Penetrating Radar and Frequency Domain Electromagnetic Surveys to Characterize the Structure of the Calderone Glacieret (Gran Sasso d’Italia, Italy)
title_full Combining Ground Penetrating Radar and Frequency Domain Electromagnetic Surveys to Characterize the Structure of the Calderone Glacieret (Gran Sasso d’Italia, Italy)
title_fullStr Combining Ground Penetrating Radar and Frequency Domain Electromagnetic Surveys to Characterize the Structure of the Calderone Glacieret (Gran Sasso d’Italia, Italy)
title_full_unstemmed Combining Ground Penetrating Radar and Frequency Domain Electromagnetic Surveys to Characterize the Structure of the Calderone Glacieret (Gran Sasso d’Italia, Italy)
title_short Combining Ground Penetrating Radar and Frequency Domain Electromagnetic Surveys to Characterize the Structure of the Calderone Glacieret (Gran Sasso d’Italia, Italy)
title_sort combining ground penetrating radar and frequency domain electromagnetic surveys to characterize the structure of the calderone glacieret (gran sasso d’italia, italy)
topic FDEM
EMI
GPR
Calderone Glacieret
cryosphere
environmental geophysics
topic_facet FDEM
EMI
GPR
Calderone Glacieret
cryosphere
environmental geophysics
url https://doi.org/10.3390/rs15102615