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Hydrologiczne i geomorfologiczne skutki ekstremalnego opadu w maju 2014 roku w zlewni Rybnego Potoku (Masyw Babiej Góry)

100%
Franczak P.
Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia
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2015
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vol. 70
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issue 2
EN
Mountain streams are subject to continuous modeling of river beds during floods. The greatest changes occur within them, however, during the catastrophic floods caused by sudden rainfall. The increase in the intensity of transformation occurs in forest areas, where the wooden logs carried by the swollen streams create a dumping ground, around which there is a greater accumulation of transported material and the formation of an increased mosaic of geomorphological forms.The study was conducted in the Rybny Potok catchment area (Babia Góra National Park). The flooding occurred on 15–16 May 2014 due to the heavy rainfall, which on 15 May amounted to 138 mm. Whereas 216.5 mm of rainfall fell in the catchment area in three days. This resulted in a sudden and full spate streams, contributing to a significant transformation in the bottoms of their geomorphological valleys. There were created many new forms, while the pre-existing increased their size.
2
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Podnoszenie jakości edukacji przyrodniczej poprzez utrwalenie istniejącej i rozwój innowacyjnej bazy edukacyjnej, na przykładzie gminy Zawoja

100%
Franczak P.
Annales Universitatis Paedagogicae Cracoviensis Studia Geographica
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2014
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vol. 7
51-66
PL
W artykule przedstawiono sposoby nowoczesnego rozwoju edukacji przyrodniczej na przykładzie gminy Zawoja. Zaprezentowano powstałą już infrastrukturę dydaktyczną (9 ścieżek dydaktycznych oraz infrastrukturę dydaktyczną skierowaną do osób niepełnosprawnych, na terenie Babiogórskiego Parku Narodowego). Następnie zaprezentowano będące w trakcie budowy Centrum Górskie w Zawoi, które ma pełnić funkcję dydaktyczną na temat obszarów górskich i himalaizmu. Autor zaprezentował też cztery projekty szlaków geoturystycznych, mających na celu edukację w zakresie procesów kształtujących powierzchnię Ziemi.
EN
The author presents the development of modern methods of environmental education based on the example of the Zawoja commune. The paper presents the educational infrastructure already formed (nine nature trails and educational infrastructure founded by the Babia Góra National Park and targeted at disabled people). The mountain centre at Zawoja that will be concerned with the teaching of the mountains and mountaineering was also presented. The author additionally presented four projected geotourism trails aimed at educating about the processes shaping the Earth’s surface.
3
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Zróżnicowanie przestrzenne i zmienność odpływu w zlewniach fliszowych na obszarze Masywu Babiej Góry

51%
Franczak P., Hudyka M., Buczek K., Górnik M.
Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia
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2015
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vol. 70
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issue 1
EN
The paper refers to spatial diversity and lability of outflow from Flysh type drainage basins. It also shows dynamics of mean and high discharge by defining the trend, the variability index and the periodicity of the hydrological parameters mentioned. The research has been taken in the partial drainage basins located in the upper drainage basin of Skawica (the streams of Czatożanka, Marków Potok, Rybny Potok, Jaworzyna) and in the upper drainage basin of Czarna Orawa (Kiczorka) at the Babia Góra slopes. The analyzed two-year period (2012–2013) has been characterized comparing to the multiannual period of 1973–2014. The hydrological and meteorological data have been obtained due to monitoring of the hydrological environment of Babiogórski National Park. The database includes the data gained from The Institute of Meteorology and Water Management research. Poland is the one of the less water-rich European countries. The unit outflow is only 5.5 dm3·s-1·km-2 (Fall 1997). The water outflow is very space and time varied through the whole country. The outflow from drainage basins of Babia Góra area is one of the biggest in Poland (about 30 dm3·s-1·km-2). The outflow index (rate of outflow?) from Babia Góra area is 88% per annum, which distinguishes this area from the Beskidy Mountains. During the winter semester the outflow index is 12.7% and during the summer semester it is 70% (Łajczak).The outflow index and the seasonal lability of the outflow from the particular Babia Góra drainage basins are very varied which is the most noticeable between the northern and southern slopes located drainage basins, however the variety is also very clear to observe from the east to the west direction. The analyzed cycle were a general low-flow period including one thaw flood within this period (2012s) and several minor floods caused by severe rainfalls (2013s). The maximum unit outflow during the flood has been noticed in Czatożanka drainage basin and the minimum unit outflow has been noticed in Kiczorka drainage basin. The highest annual average unit outflow occurred within Marków Potok, and the lowest annual average unit outflow occurred within Czatożanka. The drainage basins located at the northern slopes of Babia Góra were characterized by big seasonal outflow fluctuation between winter and summer semesters. Only at the southern slopes in the Kiczorka drainage basin the outflow was not much varied comparing the particular semesters.
4
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Sunrise as a tourist attraction in the context of tourist motivation theory: a case study of the peak of Babia Góra (Western Carpathians)

39%
Mocior E., Nowak A., Rechciński M., Franczak P., Hibner J., Krąż P., Tokarczyk N.
Bulletin of Geography. Socio-economic Series
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2015
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vol. 30
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issue 30
109-122
EN
Tourist ascents of mountain peaks before sunrise are increasingly popular. Babia Góra (Western Carpathians) is a peak on the Polish-Slovak border frequently visited by a great number of tourists at sunrise. The main objective of our research, based on the case study of Babia Gora, was to answer a more general question whether the sunrise can be considered a tourist attraction. The research included the observation and description of every sunrise at summer holiday weekends during 2012 from the peak of Babia Góra as well as the collection of data on the number of tourists and weather conditions. Survey interviews, using questionnaire, with randomly selected hikers present on the peak of Babia Góra at sunrise (269) were conducted. The investigation showed that during summer holiday sunrises there were a maximum of 130 people on the summit of Babia Góra at the same time. Most of the surveyed people (84%) agreed that the opportunity to observe the sunrise was one of the pull factors for them. This confirms the hypothesis that sunrise constitutes a tourist attraction.
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