Publication date: 08.02.2018
Licence:
CC BY-NC-ND
Editorial team
Editor-in-Chief Dorota Matuszko
Secretary Grzegorz Micek
Issue Editor Bartłomiej Rzonca
Geographical Studies, Issue 151, 2017, pp. 7 - 26
https://doi.org/10.4467/20833113PG.17.020.8032Geographical Studies, Issue 151, 2017, pp. 27 - 51
https://doi.org/10.4467/20833113PG.17.021.8033Geographical Studies, Issue 151, 2017, pp. 53 - 74
https://doi.org/10.4467/20833113PG.17.022.8034Geographical Studies, Issue 151, 2017, pp. 75 - 91
https://doi.org/10.4467/20833113PG.17.023.8035Geographical Studies, Issue 151, 2017, pp. 93 - 119
https://doi.org/10.4467/20833113PG.17.024.8036Geographical Studies, Issue 151, 2017, pp. 121 - 132
https://doi.org/10.4467/20833113PG.17.025.8037Geographical Studies, Issue 151, 2017, pp. 135 - 152
https://doi.org/10.4467/20833113PG.17.026.8038Geographical Studies, Issue 151, 2017, pp. 153 - 156
https://doi.org/10.4467/20833113PG.17.027.8039Słowa kluczowe: groundwater runoff, groundwater renewable resources, mountain catchments, southwestern Poland, flash flood, social memory of floods, mental sketch mapping, social media, mountain hydrology, precipitation, river catchment, runoff, Carpathians, East- -Central Europe, thus changes in precipitation and temperature could affect water circulation patterns. Stream runoff analysis in the upper San catchment up to Solina Lake is interesting due to semi-natural features of the catchment (minimum human impact) and potential c, the investigation of stream runoff in the High Bieszczady Mountains has not yet been studied extensively with the use of the longest data series. The research objectives were to (1) characterize stream runoff in the High Bieszczady Mountains; and to (2) i, the second period (1986–2015) revealed significant increase in mean and minimum runoff in the winter half-year (mainly January–March) and slight decrease in runoff in the summer half-year (particularly September). These changes are similar to trends obser, which have been explained by recent changes especially in Prace Geograficzne temperature but also in the type and sum of precipitation. Trends identified in the selected catchments as well as more frequent water deficits indicate a high demand for streamf, Water circulation in flysch mountains is characterized by a substantial role of runoff due to the mountain topography and thin slope covers, which result in low retention rates. Climatic conditions determine streamflow and runoff regime, mean and maximum streamflow records were analysed for trends with the nonparametric Mann-Kendall test in different time intervals: months, half-years and years. Streamflow regime of the San and Solinka rivers is characterized by the highest runoff values with low variability over a long period in spring months (March, April) due to snowmelt, whereas the lowest runoff occurres in August. Mean streamflow trends in the period 1961–2015 were not significant and indicated runoff fluctuations. However, discharge regime, discharge trends, the Sava River basin, hydrogeography, hydrology, lysimeter, tracer experiment, penetrometer-based electrical resistivity profiling, pasterstwo wysokogórskie, wypas bydła i owiec, połoniny, reprezentatywność, Czarnohora, Huculszczyzna