A5037736864- Cryospheric studies and observations
- Landslides and related hazards
- Geology and Paleoclimatology Research
- Winter Sports Injuries and Performance
- Soil erosion and sediment transport
Nicolaus Copernicus University
2022-2024
The Suwałki Glacial Megaflood Landsystem documented in NE Poland led to further morphological analysis of bedforms that originated from glacial lake-outburst floods (GLOFs) the central and eastern parts Augustów Plain. This article focuses on (1) recognition large-scale subaqueous dunes vicinity Serwy Lake, (2) creation a database consisting relevant morphometric parameters (lengths, heights gradients stoss lee slopes) indexes (steepness asymmetry ratios) (3) comparison with other landforms...
Abstract The structural change of the Svalbard landscape from glacially dominated to paraglacial, that has taken place since termination Little Ice Age (ca. 1900) is expressed by widespread retreat glaciers and progressive exposure glacial landforms. This study provides insights into rate post‐LIA deglaciation associated paraglacial transformation in foreland Gåsbreen, one first ever investigated glacier systems Arctic. Glacier situated Sørkapp Land (Southern Spitsbergen), a region...
The change in the structure of polar landscape since termination Little Ice Age (ca. 1900) is expressed by widespread retreat glaciers, progressive exposure glacial landforms at ice margins and opening marginal zones to increasing paraglacial periglacial processes operating synchronously adjacent areas. This study provides insights into rate post-LIA deglaciation associated transformation foreland Gåsbreen, a glacier situated north-western Sørkapp Land, region characterized one fastest rates...