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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2023
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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 |
_version_ |
1812819666669666304 |