Larsemann Hills: Geomorphometric modeling and mapping

Geomorphometric modeling is widely used in geosciences. However, geomorphometric modeling and mapping of Antarctic oases has not been performed so far. This article presents the first results of our work on geomorphometric modeling and mapping of the Larsemann Hills obtained in the frameworks of the...

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Published in:Polar Science
Main Author: Florinsky I.V.
Format: Other/Unknown Material
Language:English
Published: 2023
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/records/2000367
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spelling ftnipr:oai:nipr.repo.nii.ac.jp:02000367 2024-10-13T14:03:15+00:00 Larsemann Hills: Geomorphometric modeling and mapping Florinsky I.V. 2023-12-31 https://nipr.repo.nii.ac.jp/records/2000367 eng eng 10.1016/j.polar.2023.100969 https://doi.org/10.1016/j.polar.2023.100969 Polar Science 38 100969 18739652 https://nipr.repo.nii.ac.jp/records/2000367 Topography Digital elevation model Geomorphometry Surface NA 2023 ftnipr https://doi.org/10.1016/j.polar.2023.100969 2024-09-17T14:13:03Z Geomorphometric modeling is widely used in geosciences. However, geomorphometric modeling and mapping of Antarctic oases has not been performed so far. This article presents the first results of our work on geomorphometric modeling and mapping of the Larsemann Hills obtained in the frameworks of the 68th Russian Antarctic Expedition in January–April 2023. As input data, we used a fragment of the Reference Elevation Model of Antarctica (REMA). From the extracted and edited digital elevation model, we derived digital models and maps of the following 17 morphometric variables: slope, aspect, horizontal curvature, vertical curvature, mean curvature, Gaussian curvature, minimal curvature, maximal curvature, unsphericity curvature, difference curvature, vertical excess curvature, horizontal excess curvature, ring curvature, accumulation curvature, catchment area, topographic index, and stream power index. We also conducted a field geomorphometric interpretation work to provide correct physical geographic, geological, and geomorphological interpretations of morphometric maps. In the fieldwork, we carried out 54 foot routes with the total length of about 422 km. During the routes, we collected 150 rock samples for further petrological and mineralogical analyses as well as three-dimensional modeling of the samples. Derived morphometric maps can be useful for structural geological and process-oriented hydrological studies. The ultimate goal of the ongoing work is to create a large-scale geomorphometric atlas of Antarctic oases and other ice-free Antarctic territories. journal article Other/Unknown Material Antarc* Antarctic Antarctica Polar Science Polar Science National Institute of Polar Research Repository, Japan Antarctic Larsemann Hills ENVELOPE(76.217,76.217,-69.400,-69.400) Polar Science 38 100969
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
topic Topography
Digital elevation model
Geomorphometry
Surface
spellingShingle Topography
Digital elevation model
Geomorphometry
Surface
Florinsky I.V.
Larsemann Hills: Geomorphometric modeling and mapping
topic_facet Topography
Digital elevation model
Geomorphometry
Surface
description Geomorphometric modeling is widely used in geosciences. However, geomorphometric modeling and mapping of Antarctic oases has not been performed so far. This article presents the first results of our work on geomorphometric modeling and mapping of the Larsemann Hills obtained in the frameworks of the 68th Russian Antarctic Expedition in January–April 2023. As input data, we used a fragment of the Reference Elevation Model of Antarctica (REMA). From the extracted and edited digital elevation model, we derived digital models and maps of the following 17 morphometric variables: slope, aspect, horizontal curvature, vertical curvature, mean curvature, Gaussian curvature, minimal curvature, maximal curvature, unsphericity curvature, difference curvature, vertical excess curvature, horizontal excess curvature, ring curvature, accumulation curvature, catchment area, topographic index, and stream power index. We also conducted a field geomorphometric interpretation work to provide correct physical geographic, geological, and geomorphological interpretations of morphometric maps. In the fieldwork, we carried out 54 foot routes with the total length of about 422 km. During the routes, we collected 150 rock samples for further petrological and mineralogical analyses as well as three-dimensional modeling of the samples. Derived morphometric maps can be useful for structural geological and process-oriented hydrological studies. The ultimate goal of the ongoing work is to create a large-scale geomorphometric atlas of Antarctic oases and other ice-free Antarctic territories. journal article
format Other/Unknown Material
author Florinsky I.V.
author_facet Florinsky I.V.
author_sort Florinsky I.V.
title Larsemann Hills: Geomorphometric modeling and mapping
title_short Larsemann Hills: Geomorphometric modeling and mapping
title_full Larsemann Hills: Geomorphometric modeling and mapping
title_fullStr Larsemann Hills: Geomorphometric modeling and mapping
title_full_unstemmed Larsemann Hills: Geomorphometric modeling and mapping
title_sort larsemann hills: geomorphometric modeling and mapping
publishDate 2023
url https://nipr.repo.nii.ac.jp/records/2000367
long_lat ENVELOPE(76.217,76.217,-69.400,-69.400)
geographic Antarctic
Larsemann Hills
geographic_facet Antarctic
Larsemann Hills
genre Antarc*
Antarctic
Antarctica
Polar Science
Polar Science
genre_facet Antarc*
Antarctic
Antarctica
Polar Science
Polar Science
op_relation 10.1016/j.polar.2023.100969
https://doi.org/10.1016/j.polar.2023.100969
Polar Science
38
100969
18739652
https://nipr.repo.nii.ac.jp/records/2000367
op_doi https://doi.org/10.1016/j.polar.2023.100969
container_title Polar Science
container_volume 38
container_start_page 100969
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