The dynamics of mountain geosystems in southern Siberia |
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| Institution: | 1. Departamento de Ciencias Geológicas, Universidad Católica del Norte, Avenida Angamos 0610, Antofagasta, Chile;2. Department of Geological Sciences, University of Cape Town, Rondebosch 7700, South Africa;3. Centro de Excelencia en Geotermia de los Andes (CEGA) y Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile;4. Department of Earth Sciences, Natural Resources and Sustainable Development, Uppsala University, SE-75236 Uppsala, Sweden;5. Instituto de Estudios Ambientales y Recursos Naturales (i-UNAT), Departamento de Física (Geología), Universidad de Las Palmas de Gran Canaria, Spain;6. Bruker Nano GmbH, Am Studio 2D, Berlin 12,489, Germany;1. Adam Mickiewicz University, Institute of Geoinformation and Geoecology, Krygowskiego 10, Poznań, Poland;2. School of Geography, South China Normal University, Guangzhou 510631, China;3. University of Silesia, Institute of Earth Sciences, Faculty of Natural Sciences, B?dzińska 60, 41-200 Sosnowiec, Poland;1. Saint Petersburg State University, 7/9 Universitetskaya Emb., St. Petersburg 199034, Russia;2. Leibniz Institute of Ecological Urban and Regional Development, Weberplatz 1, Dresden 01217, Germany;3. Technische Universität Dresden, Chair Urban Development, Zellescher Weg 17, Dresden 01062, Germany |
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| Abstract: | Using three key areas as an example we examine the tendencies toward changes of the mountain geosystems in southern Siberia caused by fluctuations of climate. Presented are the quantitative parameters of the dynamics of nival-glacial geosystems (glaciers, perennial snow clusters, icings, and stony glaciers). Portions of large-scale maps for the key areas generated for a subsequent monitoring of the mountain geosystems are presented. |
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