Icings in the Selenga River basin
ABSTRACTIn this study, we present a GIS dataset and map of icings formed in the transboundary Selenga River basin (largest tributary of the Lake Baikal). The GIS dataset of icings is compiled using Landsat and Sentinel-2 satellite images, as well as materials from the field expedition studies. It co...
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Taylor & Francis Group
2024
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Online Access: | https://doi.org/10.1080/17445647.2024.2340994 https://doaj.org/article/118b4d8f2d1a4b31a4eb5956ad76458b |
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ftdoajarticles:oai:doaj.org/article:118b4d8f2d1a4b31a4eb5956ad76458b 2024-09-15T18:29:52+00:00 Icings in the Selenga River basin Vladimir Chernykh Andrey Shikhov Alexander Ayurzhanaev Bator Sodnomov Bair Tsydypov Margarita Zharnikova Bair Gurzhapov Endon Garmaev Avirmed Dashtseren 2024-12-01T00:00:00Z https://doi.org/10.1080/17445647.2024.2340994 https://doaj.org/article/118b4d8f2d1a4b31a4eb5956ad76458b EN eng Taylor & Francis Group https://www.tandfonline.com/doi/10.1080/17445647.2024.2340994 https://doaj.org/toc/1744-5647 doi:10.1080/17445647.2024.2340994 1744-5647 https://doaj.org/article/118b4d8f2d1a4b31a4eb5956ad76458b Journal of Maps, Vol 20, Iss 1, Pp 1-10 (2024) Icings Selenga River basin Landsat and Sentinel-2 images normalized difference snow index permafrost spatial distribution Maps G3180-9980 article 2024 ftdoajarticles https://doi.org/10.1080/17445647.2024.2340994 2024-08-05T17:49:33Z ABSTRACTIn this study, we present a GIS dataset and map of icings formed in the transboundary Selenga River basin (largest tributary of the Lake Baikal). The GIS dataset of icings is compiled using Landsat and Sentinel-2 satellite images, as well as materials from the field expedition studies. It contains 29,054 individual icings with a total area of 1154.2 km2 (0.25% of the entire basin area), including at least 56 giant icings with an area ≥ 1 km2. Icings are widespread throughout the basin, but the highest icing coverage is found on the northern slopes of Hangayn ridge in the southeastern part of the basin, where most of the giant icings are located. The highest density of icings (more than 200 per km2) is found in the eastern part of the basin. Since icings can indicate climate-driven changes in streamflow and permafrost, the presented dataset will form the basis for future studies of these transformations. Article in Journal/Newspaper permafrost Directory of Open Access Journals: DOAJ Articles Journal of Maps 20 1 1 10 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Icings Selenga River basin Landsat and Sentinel-2 images normalized difference snow index permafrost spatial distribution Maps G3180-9980 |
spellingShingle |
Icings Selenga River basin Landsat and Sentinel-2 images normalized difference snow index permafrost spatial distribution Maps G3180-9980 Vladimir Chernykh Andrey Shikhov Alexander Ayurzhanaev Bator Sodnomov Bair Tsydypov Margarita Zharnikova Bair Gurzhapov Endon Garmaev Avirmed Dashtseren Icings in the Selenga River basin |
topic_facet |
Icings Selenga River basin Landsat and Sentinel-2 images normalized difference snow index permafrost spatial distribution Maps G3180-9980 |
description |
ABSTRACTIn this study, we present a GIS dataset and map of icings formed in the transboundary Selenga River basin (largest tributary of the Lake Baikal). The GIS dataset of icings is compiled using Landsat and Sentinel-2 satellite images, as well as materials from the field expedition studies. It contains 29,054 individual icings with a total area of 1154.2 km2 (0.25% of the entire basin area), including at least 56 giant icings with an area ≥ 1 km2. Icings are widespread throughout the basin, but the highest icing coverage is found on the northern slopes of Hangayn ridge in the southeastern part of the basin, where most of the giant icings are located. The highest density of icings (more than 200 per km2) is found in the eastern part of the basin. Since icings can indicate climate-driven changes in streamflow and permafrost, the presented dataset will form the basis for future studies of these transformations. |
format |
Article in Journal/Newspaper |
author |
Vladimir Chernykh Andrey Shikhov Alexander Ayurzhanaev Bator Sodnomov Bair Tsydypov Margarita Zharnikova Bair Gurzhapov Endon Garmaev Avirmed Dashtseren |
author_facet |
Vladimir Chernykh Andrey Shikhov Alexander Ayurzhanaev Bator Sodnomov Bair Tsydypov Margarita Zharnikova Bair Gurzhapov Endon Garmaev Avirmed Dashtseren |
author_sort |
Vladimir Chernykh |
title |
Icings in the Selenga River basin |
title_short |
Icings in the Selenga River basin |
title_full |
Icings in the Selenga River basin |
title_fullStr |
Icings in the Selenga River basin |
title_full_unstemmed |
Icings in the Selenga River basin |
title_sort |
icings in the selenga river basin |
publisher |
Taylor & Francis Group |
publishDate |
2024 |
url |
https://doi.org/10.1080/17445647.2024.2340994 https://doaj.org/article/118b4d8f2d1a4b31a4eb5956ad76458b |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
Journal of Maps, Vol 20, Iss 1, Pp 1-10 (2024) |
op_relation |
https://www.tandfonline.com/doi/10.1080/17445647.2024.2340994 https://doaj.org/toc/1744-5647 doi:10.1080/17445647.2024.2340994 1744-5647 https://doaj.org/article/118b4d8f2d1a4b31a4eb5956ad76458b |
op_doi |
https://doi.org/10.1080/17445647.2024.2340994 |
container_title |
Journal of Maps |
container_volume |
20 |
container_issue |
1 |
container_start_page |
1 |
op_container_end_page |
10 |
_version_ |
1810471351743414272 |