Depth to Diameter Analysis on Small Simple Craters at the Lunar South Pole—Possible Implications for Ice Harboring
In this paper, we present a study comparing the depth to diameter (d/D) ratio of small simple craters (200–1000 m) of an area between −88.5° to −90° latitude at the lunar south pole containing Permanent Shadowed Regions (PSRs) versus craters without PSRs. As PSRs can reach temperatures of 110 K and...
Published in: | Remote Sensing |
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Main Authors: | , , , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2022
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Subjects: | |
Online Access: | https://doi.org/10.3390/rs14030450 |
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author | Ramiro Marco Figuera Christian Riedel Angelo Pio Rossi Vikram Unnithan |
author_facet | Ramiro Marco Figuera Christian Riedel Angelo Pio Rossi Vikram Unnithan |
author_sort | Ramiro Marco Figuera |
collection | MDPI Open Access Publishing |
container_issue | 3 |
container_start_page | 450 |
container_title | Remote Sensing |
container_volume | 14 |
description | In this paper, we present a study comparing the depth to diameter (d/D) ratio of small simple craters (200–1000 m) of an area between −88.5° to −90° latitude at the lunar south pole containing Permanent Shadowed Regions (PSRs) versus craters without PSRs. As PSRs can reach temperatures of 110 K and are capable of harboring volatiles, especially water ice, we analyzed the relationship of depth versus diameter ratios and its possible implications for harboring water ice. Variations in the d/D ratios can also be caused by other processes such as degradation, isostatic adjustment, or differences in surface properties. The conducted d/D ratio analysis suggests that a differentiation between craters containing PSRs versus craters without PSRs occurs. Thus, a possible direct relation between d/D ratio, PSRs, and water ice harboring might exist. Our results suggest that differences in the target’s surface properties may explain the obtained results. The resulting d/D ratios of craters with PSRs can help to select target areas for future In-Situ Resource Utilization (ISRU) missions. |
format | Text |
genre | South pole |
genre_facet | South pole |
geographic | South Pole |
geographic_facet | South Pole |
id | ftmdpi:oai:mdpi.com:/2072-4292/14/3/450/ |
institution | Open Polar |
language | English |
op_collection_id | ftmdpi |
op_doi | https://doi.org/10.3390/rs14030450 |
op_relation | https://dx.doi.org/10.3390/rs14030450 |
op_rights | https://creativecommons.org/licenses/by/4.0/ |
op_source | Remote Sensing; Volume 14; Issue 3; Pages: 450 |
publishDate | 2022 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
spelling | ftmdpi:oai:mdpi.com:/2072-4292/14/3/450/ 2025-01-17T00:51:22+00:00 Depth to Diameter Analysis on Small Simple Craters at the Lunar South Pole—Possible Implications for Ice Harboring Ramiro Marco Figuera Christian Riedel Angelo Pio Rossi Vikram Unnithan 2022-01-18 application/pdf https://doi.org/10.3390/rs14030450 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs14030450 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 14; Issue 3; Pages: 450 craters lunar exploration ice harboring Text 2022 ftmdpi https://doi.org/10.3390/rs14030450 2023-08-01T03:52:28Z In this paper, we present a study comparing the depth to diameter (d/D) ratio of small simple craters (200–1000 m) of an area between −88.5° to −90° latitude at the lunar south pole containing Permanent Shadowed Regions (PSRs) versus craters without PSRs. As PSRs can reach temperatures of 110 K and are capable of harboring volatiles, especially water ice, we analyzed the relationship of depth versus diameter ratios and its possible implications for harboring water ice. Variations in the d/D ratios can also be caused by other processes such as degradation, isostatic adjustment, or differences in surface properties. The conducted d/D ratio analysis suggests that a differentiation between craters containing PSRs versus craters without PSRs occurs. Thus, a possible direct relation between d/D ratio, PSRs, and water ice harboring might exist. Our results suggest that differences in the target’s surface properties may explain the obtained results. The resulting d/D ratios of craters with PSRs can help to select target areas for future In-Situ Resource Utilization (ISRU) missions. Text South pole MDPI Open Access Publishing South Pole Remote Sensing 14 3 450 |
spellingShingle | craters lunar exploration ice harboring Ramiro Marco Figuera Christian Riedel Angelo Pio Rossi Vikram Unnithan Depth to Diameter Analysis on Small Simple Craters at the Lunar South Pole—Possible Implications for Ice Harboring |
title | Depth to Diameter Analysis on Small Simple Craters at the Lunar South Pole—Possible Implications for Ice Harboring |
title_full | Depth to Diameter Analysis on Small Simple Craters at the Lunar South Pole—Possible Implications for Ice Harboring |
title_fullStr | Depth to Diameter Analysis on Small Simple Craters at the Lunar South Pole—Possible Implications for Ice Harboring |
title_full_unstemmed | Depth to Diameter Analysis on Small Simple Craters at the Lunar South Pole—Possible Implications for Ice Harboring |
title_short | Depth to Diameter Analysis on Small Simple Craters at the Lunar South Pole—Possible Implications for Ice Harboring |
title_sort | depth to diameter analysis on small simple craters at the lunar south pole—possible implications for ice harboring |
topic | craters lunar exploration ice harboring |
topic_facet | craters lunar exploration ice harboring |
url | https://doi.org/10.3390/rs14030450 |