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...
Published in: | Remote Sensing |
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Main Authors: | , , , , , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2023
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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. |
format | Text |
genre | Antarc* Antarctica |
genre_facet | Antarc* Antarctica |
id | ftmdpi:oai:mdpi.com:/2072-4292/15/10/2615/ |
institution | Open Polar |
language | English |
op_collection_id | ftmdpi |
op_coverage | agris |
op_doi | https://doi.org/10.3390/rs15102615 |
op_relation | Environmental Remote Sensing https://dx.doi.org/10.3390/rs15102615 |
op_rights | https://creativecommons.org/licenses/by/4.0/ |
op_source | Remote Sensing; Volume 15; Issue 10; Pages: 2615 |
publishDate | 2023 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
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 |