New approaches to modeling the critical refreezing length of a Philberth melt probe for ice sheet exploration

In recent years, interest in using Philberth melt probes in the exploration of subglacial lakes or extraterrestrial ice-covered planets has significantly increased. Consequently, several Philberth melt probes have been developed or are currently being developed. The critical refreezing length is a k...

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Published in:Polar Science
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=17373
http://id.nii.ac.jp/1291/00017230/
id ftnipr:oai:nipr.repo.nii.ac.jp:00017373
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00017373 2023-06-11T04:05:44+02:00 New approaches to modeling the critical refreezing length of a Philberth melt probe for ice sheet exploration 2023-03 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=17373 http://id.nii.ac.jp/1291/00017230/ en eng https://doi.org/10.1016/j.polar.2023.100926 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=17373 http://id.nii.ac.jp/1291/00017230/ Polar Science, 35, 100926(2023-03) 18739652 Philberth melt probe Critical refreezing length Thermal head Penetration rate Ice temperature Journal Article 2023 ftnipr https://doi.org/10.1016/j.polar.2023.100926 2023-04-29T19:34:29Z In recent years, interest in using Philberth melt probes in the exploration of subglacial lakes or extraterrestrial ice-covered planets has significantly increased. Consequently, several Philberth melt probes have been developed or are currently being developed. The critical refreezing length is a key parameter in determining the distribution of the lateral heater of the Philberth melt probe. In this study, two new approaches for calculating the critical refreezing length were proposed. Approach I was established based on the refreezing of a virtual borehole, whereas approach II was developed in the COMSOL Multiphysics 5.6a software by modeling the phase change of water and ice in the non-heated section of the Philberth melt probe. The two novel approaches were validated with the field test results of RECoverable Autonomous Sonde (RECAS) in Antarctica. The difference between the two approaches and the existing calculation methods was less than 32% and approach I presented a smaller critical refreezing length. The thermal head efficiency and ice temperature had significant influence on the critical refreezing length. Usually, the critical refreezing length increased with an increase in the thermal-head diameter, penetration rate, and ice temperature, whereas it decreased with an increase in the thermal head efficiency. Article in Journal/Newspaper Antarc* Antarctica Ice Sheet Polar Science Polar Science National Institute of Polar Research Repository, Japan Polar Science 35 100926
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
topic Philberth melt probe
Critical refreezing length
Thermal head
Penetration rate
Ice temperature
spellingShingle Philberth melt probe
Critical refreezing length
Thermal head
Penetration rate
Ice temperature
New approaches to modeling the critical refreezing length of a Philberth melt probe for ice sheet exploration
topic_facet Philberth melt probe
Critical refreezing length
Thermal head
Penetration rate
Ice temperature
description In recent years, interest in using Philberth melt probes in the exploration of subglacial lakes or extraterrestrial ice-covered planets has significantly increased. Consequently, several Philberth melt probes have been developed or are currently being developed. The critical refreezing length is a key parameter in determining the distribution of the lateral heater of the Philberth melt probe. In this study, two new approaches for calculating the critical refreezing length were proposed. Approach I was established based on the refreezing of a virtual borehole, whereas approach II was developed in the COMSOL Multiphysics 5.6a software by modeling the phase change of water and ice in the non-heated section of the Philberth melt probe. The two novel approaches were validated with the field test results of RECoverable Autonomous Sonde (RECAS) in Antarctica. The difference between the two approaches and the existing calculation methods was less than 32% and approach I presented a smaller critical refreezing length. The thermal head efficiency and ice temperature had significant influence on the critical refreezing length. Usually, the critical refreezing length increased with an increase in the thermal-head diameter, penetration rate, and ice temperature, whereas it decreased with an increase in the thermal head efficiency.
format Article in Journal/Newspaper
title New approaches to modeling the critical refreezing length of a Philberth melt probe for ice sheet exploration
title_short New approaches to modeling the critical refreezing length of a Philberth melt probe for ice sheet exploration
title_full New approaches to modeling the critical refreezing length of a Philberth melt probe for ice sheet exploration
title_fullStr New approaches to modeling the critical refreezing length of a Philberth melt probe for ice sheet exploration
title_full_unstemmed New approaches to modeling the critical refreezing length of a Philberth melt probe for ice sheet exploration
title_sort new approaches to modeling the critical refreezing length of a philberth melt probe for ice sheet exploration
publishDate 2023
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=17373
http://id.nii.ac.jp/1291/00017230/
genre Antarc*
Antarctica
Ice Sheet
Polar Science
Polar Science
genre_facet Antarc*
Antarctica
Ice Sheet
Polar Science
Polar Science
op_relation https://doi.org/10.1016/j.polar.2023.100926
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=17373
http://id.nii.ac.jp/1291/00017230/
Polar Science, 35, 100926(2023-03)
18739652
op_doi https://doi.org/10.1016/j.polar.2023.100926
container_title Polar Science
container_volume 35
container_start_page 100926
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