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Volume XXXV-XXXVI (35-36)

Meteorologiczne, hydrologiczne i geomorfologiczne zjawiska ekstremalne w południowej Polsce.  

 

Tadeusz Ziętara 

Przedmowa
(Introduction)

Ziętara T., 2004-2005, Przedmowa, Folia Geographica ser. Geographica-Physica, vol. XXXV-XXXVI (35-36): 5-9 (in polish).

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Małgorzata Bajgier-Kowalska 

Rola gospodarczej działalności człowieka w powstawaniu i odmładzaniu osuwisk w Karpatach Fliszowych
(The role of human activity in the incidence and reactivation of landslides in the flysch Carpathians)

Bajgier-Kowalska M., 2004-2005, Rola gospodarczej działalności człowieka w powstawaniu i odmładzaniu osuwisk w Karpatach Fliszowych, Folia Geographica ser. Geographica-Physica, vol. XXXV-XXXVI (35-36): 11-30 (in polish).

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Dominika Wrońska 

Wpływ procesów osuwiskowych na działalność człowieka oraz szatę roślinną Magurskiego Parku Narodowego
(The influence of landsliding on human activity and vegetation cover in Magura National Park)

Wrońska D., 2004-2005, Wpływ procesów osuwiskowych na działalność człowieka oraz szatę roślinną Magurskiego Parku Narodowego, Folia Geographica ser. Geographica-Physica, vol. XXXV-XXXVI (35-36): 31-52 (in polish).

Keywords: landsliding processes, human activity, vegetation cover, Magura Wątkowska Range

Summary: The author mapped 24 landslide sites in the northwestern part of the Magura Wątkowska ridge. The landslides covered the area of 7.6 km2, or 10.5% of the overall slope area. The "small tectonics analysis" method, as well as interviews with local population, was used to determine the activity of the landslides. The paper describes morphological and morphometric characteristics of selected landslides with the view of defining their impact on human activity, the impact of human activity on the landslide features and the impact of landsliding on the vegetation cover of the Magura National Park. It can be concluded that the significance of the landslide impact on the transformation of the geographical environment varies widely. A large majority of the sites are located within the National Park, and as such they pose no threat to human activities. Indeed, landsliding fulfils a role that is highly beneficial to the environment.
There are, however, landslides partly or entirely located outside the Park boundaries. Some villages are partly within the limits of such landslide sites. That is where landsliding processes have a major influence on human economic activity. They have caused numerous cases of damage to housing and other types of buildings, as well as to municipal and transport infrastructure. What is worrying is that the local population describe numerous displacements within the sites without realising that these constitute serious signals of potential catastrophic mass movements.
From the points of view of landslide ecosystems and human economic activity it is the best when an entire landslide is located within a protected area and outside any permitted broadly defined and unsound human activity. Thus, any landslide sites still free from development and located near the boundaries of a national park should definitely be included in such park. This could go some way to put a stop to the development on landslide slopes and to mitigate risks to human life and property and related to catastrophic-scale sliding processes.

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Roman Malarz 

Geomorfologiczne skutki działania zapór wodnych w okresach powodziowych w dolinie Soły
(Geomorphic effects of reservoir operation during floods in the Soła valley)

Malarz R., 2004-2005, Geomorfologiczne skutki działania zapór wodnych w okresach powodziowych w dolinie Soły, Folia Geographica ser. Geographica-Physica, vol. XXXV-XXXVI (35-36): 53-64 (in polish).

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Wojciech Chełmicki, Tomasz Bieńkowski 

Przepływy niżówkowe w dorzeczu górnego Dunajca w 2003 r. na tle wielolecia 1951-2003
(Low flows in the upper part of the Dunajec drainage basin in 2003 compared with the period of 1951-2003.)

Chełmicki W., Bieńkowski T., 2004-2005, Przepływy niżówkowe w dorzeczu górnego Dunajca w 2003 r. na tle wielolecia 1951-2003, Folia Geographica ser. Geographica-Physica, vol. XXXV-XXXVI (35-36): 65-75 (in polish).

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Jan Lach 

Skutki powodzi w lipcu 2001 r. w powiecie nowosądeckim
(Results of flood of july 2001 in the Nowy Sącz district.)

Lach J., 2004-2005, Skutki powodzi w lipcu 2001 r. w powiecie nowosądeckim, Folia Geographica ser. Geographica-Physica, vol. XXXV-XXXVI (35-36): 77-91 (in polish).

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Ewa Łupikasza, Zuzanna Bielec-Bąkowska 

Synoptyczne uwarunkowania dni ekstremalnych pod względem termicznym w Małopolsce w drugiej połowie XX wieku
(Synoptic conditions of the thermal extreme days in Małopolska in the second half of the 20th century )

Łupikasza E., Bielec-Bąkowska Z., 2004-2005, Synoptyczne uwarunkowania dni ekstremalnych pod względem termicznym w Małopolsce w drugiej połowie XX wieku, Folia Geographica ser. Geographica-Physica, vol. XXXV-XXXVI (35-36): 93-112 (in polish).

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Zuzanna Bielec-Bąkowska, Dorota Matuszko 

Warunki meteorologiczne sprzyjające występowaniu burz w Krakowie i w okolicach.
(Meteorological conditions of thunderstorms occurrence in Cracow and its surroundings)

Bielec-Bąkowska Z., Matuszko D., 2004-2005, Warunki meteorologiczne sprzyjające występowaniu burz w Krakowie i w okolicach., Folia Geographica ser. Geographica-Physica, vol. XXXV-XXXVI (35-36): 113-131 (in polish).

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Katarzyna Piotrowicz, Rafał Bąkowski, Marek Kozłowski 

Energia wiatru w wybranych sytuacjach synoptycznych w południowo-wschodniej Polsce
(The energy of wind in chosen synoptic situations in south-eastern Poland)

Piotrowicz K., Bąkowski R., Kozłowski M., 2004-2005, Energia wiatru w wybranych sytuacjach synoptycznych w południowo-wschodniej Polsce, Folia Geographica ser. Geographica-Physica, vol. XXXV-XXXVI (35-36): 133-151 (in polish).

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Janina Trepińska 

Pionowy profil prędkości wiatru przyziemnego.
(Vertical profile of wind speed at the ground elevation)

Trepińska J., 2004-2005, Pionowy profil prędkości wiatru przyziemnego., Folia Geographica ser. Geographica-Physica, vol. XXXV-XXXVI (35-36): 153-166 (in polish).

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