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Volume XXXVII-XXXVIII (37-38)

 

 

Michał Kasina, Joanna-Pociask-Karteczka, Zenon Nieckarz 

Tendencje występowania wysokich przepływów w dorzeczu Dunajca w II połowie XX wieku.
(Trends in high river flows in the Dunajec River drainage basin in the second half of the 20th century)

Kasina M., Joanna-Pociask-Karteczka , Nieckarz Z., 2006-2007, Tendencje występowania wysokich przepływów w dorzeczu Dunajca w II połowie XX wieku., Folia Geographica ser. Geographica-Physica, vol. XXXVII-XXXVIII (37-38): 5-35 (in polish).

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Ladislav Holko, Hubert Kostka 

Snow cover in northern Slovakia - past, present and future

Holko L., Kostka H., 2006-2007, Snow cover in northern Slovakia - past, present and future, Folia Geographica ser. Geographica-Physica, vol. XXXVII-XXXVIII (37-38): 37-51.

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Pavol Miklanek, Pavla Pekarova 

Influence of forest on snowmelt runoff in small highland basins in Slovakia.

Miklanek P., Pekarova P., 2006-2007, Influence of forest on snowmelt runoff in small highland basins in Slovakia., Folia Geographica ser. Geographica-Physica, vol. XXXVII-XXXVIII (37-38): 53-64.

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Adam Choiński 

Zjawiska lodowe na Morskim Oku w Tatrach
(Ice phenomena on the Morskie Oko Lake in the Tatra Mts.)

Choiński A., 2006-2007, Zjawiska lodowe na Morskim Oku w Tatrach, Folia Geographica ser. Geographica-Physica, vol. XXXVII-XXXVIII (37-38): 65-77 (in polish).

Keywords: ice phenomena on lakes, the Morskie Oko Lake, tendencies of changes of ice cover

Summary: Despite 200-year long research on the Morskie Oko Lake, there are still many questions concerning its thermal conditions and ice phenomena. In the paper, on the basis of data collected by the Institute of Meteorology and Water Management (IMGiW) over the period 1971-1995, an analysis of the many years' changes of the duration of ice phenomena and ice cover as well as of changes of the annual maximum ice thickness was made. It was observed that the duration of ice cover and ice phenomena becomes shorter and that there is a tendency to reduce the annual maximum ice thickness. Basing on carried out thrice (May 9, 2006, January 26, 2007 and April 11-12, 2007) measurements of the ice thickness the spatial differentiation of the ice covers was defined. It was found that in some periods it is insignificant (for example, only 7 cm on January 26, 2007), while in some other it is noticeable (for example, as much as 30 cm on April 11-12, 2007). However, periodical measurements of the ice thickness may be not representative of the whole ice sheet cover and they may significantly differ from the mean ice cover thickness. Subglacial outflow of the Morskie Oko Lake waters to the Rybi Potok Stream, differences of insolation caused by overshading of the ice sheets by the mountains, dependence of the ice thickness on the depth of the underlying water as well as possible inflow of the bottom waters may be pointed out as main factors leading to such big differences of the ice cover thickness.

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Rafał Kroczak 

Użytkowanie terenu a zmiany sieci dróg polnych na Pogórzu Cięzkowickim w XX wieku.
(The correlation between the land use and changes in the unmetalled road network in Pogórze Ciężkowickie in the 20th century.)

Kroczak R., 2006-2007, Użytkowanie terenu a zmiany sieci dróg polnych na Pogórzu Cięzkowickim w XX wieku., Folia Geographica ser. Geographica-Physica, vol. XXXVII-XXXVIII (37-38): 79-94 (in polish).

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Łukasz Wiejaczka 

Relacje między temperaturą wody w rzece a temperaturą powietrza (na przykładzie rzeki Ropy).
(Relationship between water temperature in the river and air temperature (on the Ropa River as an example).)

Wiejaczka Ł., 2006-2007, Relacje między temperaturą wody w rzece a temperaturą powietrza (na przykładzie rzeki Ropy)., Folia Geographica ser. Geographica-Physica, vol. XXXVII-XXXVIII (37-38): 95-105 (in polish).

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