TY - GEN A1 - Tamulewicz, Jan (1945– ) PB - IGiPZ PAN PB - Zakład Narodowy im. Ossolińskich - Wydaw. Polskiej Akademii Nauk N1 - 91 pp., [2] k. tabl. : il. ; 24 cm N1 - Bibliogr. p. 84-87 N1 - Sum. eng, rus L1 - http://www.rcin.org.pl/igipz/Content/27016/PDF/WA51_39817_r1982-z3-4_Dokumentacja-Geogr.pdf M3 - Text CY - Wrocław CY - Warszawa J2 - Dokumentacja Geograficzna 1982 z. 3-4 PY - 1982 KW - downpours KW - typologies KW - West Pomerania T1 - Taksonomiczne podstawy typologii reżimu opadów atmosferycznych na przykładzie Pojezierza Pomorskiego i Niziny Wielkopolskiej = Taxonomic foundations of precipitation regime typology : a study of the Pomeranian Lake District and the Great Poland Lowland UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/27016 ER - TY - GEN A2 - Starkel, Leszek (1931– ). Red. PB - Wydaw. Continuo PB - IGiPZ PAN N1 - 107 pp., [1] k. tabl. złoż. : mapy, wykr. ; 24 cm N1 - Summary in English. L1 - http://www.rcin.org.pl/igipz/Content/5700/PDF/WA51_16174_r1998-nr11_Dokumentacja-Geogr.pdf M3 - Text CY - Wrocław CY - Warszawa J2 - Geomorphic and sedimentologic records of local downpours J2 - Dokumentacja Geograficzna, nr 11 PY - 1998 KW - downpours KW - geomorphic record of downpours KW - sedimentologic record of downpours KW - floods KW - extreme events KW - Poland T1 - Geomorfologiczny i sedymentologiczny zapis lokalnych ulew UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/5700 ER - TY - GEN A1 - Soja, Roman A1 - Wit-Jóźwik, Krystyna ( –2003) A1 - Welc, Andrzej PB - IGiPZ PAN PB - Zakład Narodowy im. Ossolińskich - Wydaw. Polskiej Akademii Nauk N1 - 85 pp. : maps ; 24 cm N1 - Bibliogr. N1 - Sum. eng, rus L1 - http://www.rcin.org.pl/igipz/Content/27317/PDF/WA51_39852_r1977-z6_Dokumentacja-Geogr.pdf M3 - Text CY - Wrocław CY - Warszawa J2 - Dokumentacja Geograficzna 1977 z. 6 PY - 1977 KW - aeolian erosion KW - downpours KW - deflation KW - Szymbark KW - Carpathians T1 - Opady atmosferyczne i deflacja w okolicach Szymbarku = Precipitation and eolian processes in the region of Szymbark UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/27317 ER - TY - GEN N1 - 24 cm N2 - Heavy downpours and flash floods accelerate the denudation of slopes, as well as erosion, and hence accumulation in the bottoms of valleys (Słupik, 1981; Starkel, 1996; Gil, 1998). However, the geomorphological impact depends less on the amount and duration of falls of rain, and more on intensity and spatial extent. The intensity of mass movements and floods also depends on relief, the type and thickness of soil, the lithology and tectonic history of rocks, which together determine infiltration rates and runoff. An important role in triggering mass movements is also played by human activity (land use, terracing and the undercutting of slopes). This paper presents the role of short-duration downpours occurring in the July of 1997 and 2008 where the shaping of the Jaszcze and Jamne valleys in the Gorce Mountains is concerned. The narrow valley of the Jaszcze has very steep slopes and is covered by dense patches of forest. In contrast, the Jamne Valley with its predominantly gentle slopes has been largely deforested. At higher elevations, the Jaszcze catchment has a prevalence of meadows and pastures that contrasts with the dominant arable land lower down. The Jamne catchment in turn has meadows and pastures of its own, plus arable fields reaching altitudes of 1100 m a.s.l. (Obrębska-Starklowa, 1970). Following the rainfall of July 1997, it proved possible to register 85 new superficial landslides on air photos (55 in the Jaszcze Valley and 30 in the Jamne Valley), these covering a total area of c. 29,700 m2. Among dominant forms were slumps and mudflows of loamy-sandy regolith, created mainly on steep, grass-covered slopes (≥20°), on the edges of field terraces and on the colluvium of old landslides. A flood of 23 July 2008 was also connected with a heavy downpour, daily rainfall that day reaching 76.3 mm at the river outlet. The highest level in the Jaszcze and Jamne was noted at about 17.00. The most marked changes characterised the Jamne channel, this reflecting its more limited forest cover and the higher density of the river network. Lateral erosion prevailed over downcutting, causing the reactivation of old undercuts and the development of new ones, the height reaching 3.5 m. Boulders up to 25 cm in size were transported, and the deposition of debris followed. Older gravel bars were cut and new ones built up. Only a few small earth slumps appeared on the slopes, and these were never in forest. A map showing the potential susceptibility of the Jaszcze and Jamne catchments was prepared on the basis of field data and a statistical analysis, using the landslide index method (Van Westen, 1994). While the greatest geomorphological effects of rainfall are to be noted in stream channels, the transformation of slopes by mass movements is less remarkable. However superficial landslides are characteristic of deforested slopes covered by a thin loamy regolith over flysch sandstones and shales. GIS analysis and field observations make it clear that the geological structure deeper down does not play an important role in triggering of superficial landslides. L1 - http://www.rcin.org.pl/igipz/Content/55592/PDF/WA51_75415_r2009-t81-z3_Przeg-Geogr-Bucala.pdf M3 - Text J2 - Przegląd Geograficzny T. 81 z. 3 (2009) PY - 2009 IS - 3 EP - 418 KW - shortlived downpours KW - mass movements KW - valley processes KW - Gorce Mountains A1 - Bucała, Anna PB - IGiPZ PAN VL - 81 CY - Warszawa SP - 399 T1 - Rola opadów nawalnych w kształtowaniu stoków i koryt w Gorcach na przykładzie zlewni potoków Jaszcze i Jamne = The role of shortlived downpours in shaping slopes and valley bottoms in the Gorce Mountains (as exemplified by the Jaszcze and Jamne catchments) UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/55592 ER - TY - GEN N1 - 187 pp. ; 24 cm L1 - http://www.rcin.org.pl/igipz/Content/2293/PDF/WA51_13948_r2011-vol84-z1_Geographia-Pol-pani.pdf M3 - Text J2 - Geographia Polonica Vol. 84 Special Issue Part 1 (2011) PY - 2011 IS - Special Issue Part 1 EP - 115 KW - erosion KW - gullies KW - fans KW - extreme events KW - downpours KW - palaeoclimate KW - palaeohydrology KW - Holocene KW - Russia A1 - Panin, Andrey A1 - Fuzeina, Yulia A1 - Karevskaya, Inessa A1 - Sheremetskaya, Elena PB - IGiPZ PAN VL - 84 CY - Warszawa SP - 95 T1 - Mid-Holocene gullying indicating extreme hydroclimatic events in the centre of the Russian Plain UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/2293 ER - TY - GEN A2 - Starkel, Leszek (1931– ). Red. PB - Wydawnictwo Continuo ; PB - IGiPZ PAN N1 - 107, [1] pp., [8] k. tabl. kolor. : il. ; 24 cm N1 - Summ. eng L1 - http://www.rcin.org.pl/igipz/Content/5697/PDF/WA51_16178_r1997-nr8_Dokumentacja-Geogr.pdf M3 - Text CY - Wrocław J2 - Role of heavy downpours in the evolution of the Miechów Upland (with downpour of 15 September 1995 as the example) J2 - Dokumentacja Geograficzna, nr 8 PY - cop. 1997 KW - relief evolution KW - extreme events KW - soil erosion KW - loess sites KW - gullies KW - downpours KW - Miechów Upland T1 - Rola gwałtownych ulew w ewolucji rzeźby Wyżyny Miechowskiej (na przykładzie ulewy w dniu 15 września 1995 roku) UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/5697 ER - TY - GEN N1 - 24 cm L1 - http://www.rcin.org.pl/igipz/Content/153/PDF/PrzG_2009_81_3-l_i.pdf M3 - Text J2 - Przegląd Geograficzny PY - 2009 IS - 3 EP - 315 KW - scales of ecological indicator values KW - plant communities KW - river valleys KW - springs KW - bioclimate KW - shortlived downpours KW - landslides KW - channel processes KW - glaciations KW - karst relief KW - Vistula river valley KW - Odra basin KW - Kołobrzeg KW - Gorce Mountains KW - Tatra Mountains PB - IGiPZ PAN VL - 81 CY - Warszawa SP - 315 T1 - Przegląd Geograficzny T. 81 z. 3 (2009), Spis treści UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/153 ER -