Assessment of Electromagnetic Absorption of Ice From Ice Core Measurements
DOME C is located on the East Antarctic Plateau at an altitude of 3233 m above sea level and is the site of the Italian–French base, i.e., the Concordia Station ( 123∘20′ E, 75∘06′ S). It has become an important location for several scientific research studies, including astrophysics, geophysics, gl...
Published in: | IEEE Transactions on Geoscience and Remote Sensing |
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Online Access: | http://hdl.handle.net/2122/10668 https://doi.org/10.1109/TGRS.2016.2551300 |
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ftingv:oai:www.earth-prints.org:2122/10668 2023-05-15T14:01:37+02:00 Assessment of Electromagnetic Absorption of Ice From Ice Core Measurements Zirizzotti, Achille Emanuele Cafarella, Lili Urbini, Stefano Baskaradas, James Arokiasami Settimi, Alessandro Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia #PLACEHOLDER_PARENT_METADATA_VALUE# 2016 http://hdl.handle.net/2122/10668 https://doi.org/10.1109/TGRS.2016.2551300 en eng IEEE Transactions on Geoscience and Remote Sensing 8/54 (2016) http://hdl.handle.net/2122/10668 doi:10.1109/TGRS.2016.2551300 open Ice thickness Radar antennas Antarctica Signal resolution Receivers Surface morphology 02.02. Glaciers article 2016 ftingv https://doi.org/10.1109/TGRS.2016.2551300 2022-07-29T06:07:10Z DOME C is located on the East Antarctic Plateau at an altitude of 3233 m above sea level and is the site of the Italian–French base, i.e., the Concordia Station ( 123∘20′ E, 75∘06′ S). It has become an important location for several scientific research studies, including astrophysics, geophysics, glaciology, and climatology, due to the perceived long-term stability and thickness of ice at this location [1], [5], [18], [24]. During the site selection and follow up of the EPICA Dome C coring project, which ultimately provided more than 800 000 years of palaeoclimatic series distributed along 3270 m [6], numerous radio-echo sounding (RES) surveys were undertaken to improve core positioning and subsequently to better leverage data and logistical infrastructures from the coring effort. These studies were conducted at very different scales over the Dome C region and revealed important information about the bedrock physiography and its physical conditions [2]– [4], [8], [9], [19], [20], [30], [31]. This study builds upon these efforts using data from two recently acquired ground-based surveys collected during 2009 and 2011 in a very small area (2.5 × 2.0 km) in the immediate proximity of the EPICA drilling site, to test advances in the acquisition and digitization technology and resolve the basal environment to unprecedented detail. Published 4758 - 4763 5A. Paleoclima e ricerche polari JCR Journal Article in Journal/Newspaper Antarc* Antarctic Antarctica EPICA ice core Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Antarctic Concordia Station ENVELOPE(123.333,123.333,-75.100,-75.100) IEEE Transactions on Geoscience and Remote Sensing 54 8 4758 4763 |
institution |
Open Polar |
collection |
Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) |
op_collection_id |
ftingv |
language |
English |
topic |
Ice thickness Radar antennas Antarctica Signal resolution Receivers Surface morphology 02.02. Glaciers |
spellingShingle |
Ice thickness Radar antennas Antarctica Signal resolution Receivers Surface morphology 02.02. Glaciers Zirizzotti, Achille Emanuele Cafarella, Lili Urbini, Stefano Baskaradas, James Arokiasami Settimi, Alessandro Assessment of Electromagnetic Absorption of Ice From Ice Core Measurements |
topic_facet |
Ice thickness Radar antennas Antarctica Signal resolution Receivers Surface morphology 02.02. Glaciers |
description |
DOME C is located on the East Antarctic Plateau at an altitude of 3233 m above sea level and is the site of the Italian–French base, i.e., the Concordia Station ( 123∘20′ E, 75∘06′ S). It has become an important location for several scientific research studies, including astrophysics, geophysics, glaciology, and climatology, due to the perceived long-term stability and thickness of ice at this location [1], [5], [18], [24]. During the site selection and follow up of the EPICA Dome C coring project, which ultimately provided more than 800 000 years of palaeoclimatic series distributed along 3270 m [6], numerous radio-echo sounding (RES) surveys were undertaken to improve core positioning and subsequently to better leverage data and logistical infrastructures from the coring effort. These studies were conducted at very different scales over the Dome C region and revealed important information about the bedrock physiography and its physical conditions [2]– [4], [8], [9], [19], [20], [30], [31]. This study builds upon these efforts using data from two recently acquired ground-based surveys collected during 2009 and 2011 in a very small area (2.5 × 2.0 km) in the immediate proximity of the EPICA drilling site, to test advances in the acquisition and digitization technology and resolve the basal environment to unprecedented detail. Published 4758 - 4763 5A. Paleoclima e ricerche polari JCR Journal |
author2 |
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia #PLACEHOLDER_PARENT_METADATA_VALUE# |
format |
Article in Journal/Newspaper |
author |
Zirizzotti, Achille Emanuele Cafarella, Lili Urbini, Stefano Baskaradas, James Arokiasami Settimi, Alessandro |
author_facet |
Zirizzotti, Achille Emanuele Cafarella, Lili Urbini, Stefano Baskaradas, James Arokiasami Settimi, Alessandro |
author_sort |
Zirizzotti, Achille Emanuele |
title |
Assessment of Electromagnetic Absorption of Ice From Ice Core Measurements |
title_short |
Assessment of Electromagnetic Absorption of Ice From Ice Core Measurements |
title_full |
Assessment of Electromagnetic Absorption of Ice From Ice Core Measurements |
title_fullStr |
Assessment of Electromagnetic Absorption of Ice From Ice Core Measurements |
title_full_unstemmed |
Assessment of Electromagnetic Absorption of Ice From Ice Core Measurements |
title_sort |
assessment of electromagnetic absorption of ice from ice core measurements |
publishDate |
2016 |
url |
http://hdl.handle.net/2122/10668 https://doi.org/10.1109/TGRS.2016.2551300 |
long_lat |
ENVELOPE(123.333,123.333,-75.100,-75.100) |
geographic |
Antarctic Concordia Station |
geographic_facet |
Antarctic Concordia Station |
genre |
Antarc* Antarctic Antarctica EPICA ice core |
genre_facet |
Antarc* Antarctic Antarctica EPICA ice core |
op_relation |
IEEE Transactions on Geoscience and Remote Sensing 8/54 (2016) http://hdl.handle.net/2122/10668 doi:10.1109/TGRS.2016.2551300 |
op_rights |
open |
op_doi |
https://doi.org/10.1109/TGRS.2016.2551300 |
container_title |
IEEE Transactions on Geoscience and Remote Sensing |
container_volume |
54 |
container_issue |
8 |
container_start_page |
4758 |
op_container_end_page |
4763 |
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1766271566400716800 |