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Icings in the Selenga River basin

Bibliographic Data

ID16840566
AuthorsVladimir Chernykh, Chernykh V (0000-0001-9365-7340, Baikal Institute of Nature Management, corresponding author), Andrey Shikhov (0000-0003-2489-8436, Perm State University), Alexander A Ayurzhanaev (0000-0002-2282-7848, Baikal Institute of Nature Management), Alexander Ayurzhanaev, Bator V Sodnomov (0000-0002-4099-7226, Baikal Institute of Nature Management), Bator Sodnomov, Bair Tsydypov, Bair Z Tsydypov (0000-0001-8340-7268, Baikal Institute of Nature Management), Margarita Zharnikova, M A Zharnikova (0000-0003-3428-6724, Baikal Institute of Nature Management), Bair Gurzhapov (Baikal Institute of Nature Management), Endon Garmaev, Е Ж Гармаев (0000-0002-8524-4930, Baikal Institute of Nature Management), Avirmed Dashtseren, Dashtseren Avirmed (0000-0003-4119-5345, Mongolian Academy of Sciences)
Year2024
Volume20
Issue1
Pages1-10
Publication date2024-12-31
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueJournal of Maps (JOURNAL)
Journal identifiersISSN: 1744-5647 • E-ISSN: 1744-5647
PublisherInforma UK Limited (PUBLISHER • GB)
DOI10.1080/17445647.2024.2340994
OpenAlexW4395028075
LanguageEN
References cited22

In 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

Cartography · Drainage basin · Geography · Geomorphology · Permafrost · Physical geography · Remote sensing · Ridge · Structural basin · Tributary · Arctic and Antarctic ice dynamics · Climate change and permafrost · Cryospheric studies and observations · Geology · Oceanography · Paleontology

  • WorldClim 2

    Open Access•Stephen E Fick, Robert J Hijmans•International Journal of…•2017

Citation velocityhistorical
Highly citedNo

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