TY - GEN A1 - Długosz, Michał PB - IGiPZ PAN N1 - 112 pp. : il. color. ; 24 cm N1 - Summary in English. N1 - Bibliogr. p. 104-110 L1 - http://www.rcin.org.pl/igipz/Content/13282/PDF/WA51_22185_r2011-nr230_Prace-Geogr.pdf M3 - Text CY - Warszawa J2 - Prace Geograficzne / Polska Akademia Nauk. Instytut Geografii i Przestrzennego Zagospodarowania im. Stanisława Leszczyckiego, nr 230 J2 - Transformacja geosystemów polskich Karpat fliszowych przez ruchy masowe PY - 2011 KW - landslides KW - mass movements KW - flysch KW - Flysch Carpathians T1 - Podatność stoków na osuwanie w polskich Karpatach fliszowych = Landslide susceptibility in the Polish Carpathians UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/13282 ER - TY - GEN N1 - 24 cm L1 - http://www.rcin.org.pl/igipz/Content/1232/PDF/Wa51_12741_r2011-t83-z1_Przeglad_Geograficzny-Dlugosz.pdf M3 - Text J2 - Przegląd Geograficzny T. 83 z. 1 (2011) PY - 2011 IS - 1 EP - 68 A1 - Długosz, Michał PB - IGiPZ PAN VL - 83 CY - Warszawa SP - 51 T1 - Rola intensywnych opadów burzowych w transformacji rzeźby Karpat (na przykładzie zdarzenia z czerwca 2009 r. na Podhalu) = The role of extreme falls of rain in the transformation of Carpathian relief (a case study from Poland's Podhale region, June 2009) UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/1232 ER - TY - GEN N1 - 24 cm N2 - The upper sections of avalanche paths (avalanche starting zones) in the Tatras are being transformed by morphogenetic processes, both secular and rapid mass movements, which include avalanches. The erosion niches and scars occurring within the avalanche starting zones are most exposed to these processes. A three-year monitoring of the impacts of these processes leads to the conclusion that, in the absence of dirty avalanches, the efficiency of secular geomorphological processes is low (max. a few cm/year). Such avalanches can clearly transform the relief as is demonstrated by the results of analyses of erosion niches and scars on orthophotomaps. Furthermore, it was found that the direction of relief changes (accumulation or erosion) in the Tatras is spatially and temporally varied, as well as varying within individual avalanche starting zones, and sometimes within individual erosion niches or scars. L1 - http://www.rcin.org.pl/igipz/Content/58253/PDF/WA51_78427_r2016-t89-no1_G-Polonica-Raczkowsk.pdf M3 - Text J2 - Geographia Polonica Vol. 89 No. 1 (2016) PY - 2016 IS - 1 EP - 29 KW - morphodynamics KW - slopes KW - avalanche KW - starting zones KW - Tatra Mountains A1 - Rączkowska, Zofia A1 - Rojan, Elzbieta A1 - Długosz, Michał PB - IGiPZ PAN VL - 89 CY - Warszawa SP - 17 T1 - The morphodynamics of slopes within the snow avalanche starting zones in the Tatras UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/58253 ER - TY - GEN N1 - Bibliogr. N1 - Summ. eng. N1 - 244 p. : il. (color.) ; 24 cm N2 - Airborne Laser Scanning (Light Detection and Ranging – LiDAR) have proven to be a helpful tool in the analysis of mass movements. Even though LiDAR has been used in the environmental sciences recently, studies using these methods in the analysis of landslides are numerous. The aim of the study was to determine the ability to identify landslides in the commune scale based on spatial data from airborne laser scanning within the framework of “Information System of the National Guards against extraordinary threats” (ISOK). The assumption of the applied method was to determine the landslides areas, without fieldwork mapping, based only on data obtained from point clouds and afterwards to verify gathered results. Two researchers, lacking knowledge concerning study area, prepared the Digital Elevation Model from the point clouds and based on these data recognized the landslides as well as hazardous areas. The second part of the research team who previously made a detailed terrain landslides mapping in the study area had the task of verifying the outcomes of the first stage. Subsequently, combined analysis of mistakes made be the first part of research team was carried out and the capabilities and limitations of the method was established. Comparison of materials obtained from diverse data sources permit to perform two-way verification of conducted research. Mistakes coming from either vague parts of point cloud’ DEM or terrain landslide mapping in forested areas were recognized. L1 - http://www.rcin.org.pl/igipz/Content/58002/PDF/WA51_78247_r2014-t38_PEK-Kroh.pdf M3 - Text J2 - Problemy Ekologii Krajobrazu = The Problems of Landscape Ecology, t. 38 PY - 2014 EP - 75 KW - LiDAR KW - digital elevation model KW - landslides KW - local community A1 - Kroh, Paweł A1 - Struś, Paweł A1 - Gorczyca, Elżbieta A1 - Wrońska-Wałach, Dominika A1 - Długosz, Michał PB - Polska Asocjacja Ekologii Krajobrazu PB - Polska Akademia Nauk. Instytut Geografii i Przestrzennego Zagospodarowania im. Stanisława Leszczyckiego. VL - 38 CY - Warszawa SP - 61 T1 - Identyfikacja osuwisk w gminie Łososina Dolna na podstawie danych lotniczego skanowania laserowego = Identification of landslides in Łososina Dolna commune based on spatial data from airborne laser scanning UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/58002 ER -