TY - GEN A1 - Szostak, Mieczysław PB - IGiPZ PAN PB - Państwowe Wydawnictwo Naukowe N1 - 68, [3] pp., [4] k. tabl. złoż. : il., maps, err. ; 24 cm N1 - Bibliogr. p. 60-62 N1 - Sum eng., rus. L1 - http://www.rcin.org.pl/igipz/Content/15326/PDF/WA51_21957_r1967_nr58_Prace-Geogr.pdf M3 - Text CY - Warszawa J2 - Prace Geograficzne / Instytut Geografii Polskiej Akademii Nauk ; nr 58 PY - 1967 KW - lakes KW - genesis of lakes KW - water resources KW - Śniardwy Lake T1 - Pochodzenie jeziora Śniardwy i jego zasoby wodne = Origin of lake Śniardwy and its water resources = Ozero Snjardvy - ego genezis i vodnye resursy UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/15326 ER - TY - GEN N1 - 24 cm N2 - The aim of the presented research is to assess the storage capacity and the groundwater runoff dynamics in the High Bieszczady Mountain (SE Poland, Outer Eastern Carpathians) on the basis of measurements in three gauging stations within San river catchment. The study is based on recession curve analyses in the period 2005-2015.Recession coefficient (α) and storage capacity (Wmax) were calculated for each recession segment. Furthermore, for each gauging station master recession curves were constructed. Recession coefficients were about 10-2. All studied catchments were characterized by higher median of α and Wmax values in the winter half-year, than in the summer half-year. The master recession curves obtained in this study showed two-phase drainage model. During the first phase (higher α values) water resources were depleting faster, probably due to affecting of base flow by part of interflow, than in the second phase (lower α values). The largest catchments (San gauge in Zatwarnica and Dwernik) showed similar median values of storage capacity (Me: 14-21 mm), whereas the smallest Wołosaty catchment showed higher median values (Me: 20-32 mm). The higher values might be caused by higher average annual precipitation and the more complex geological condition, what might locally influence on the storage capacity increase. L1 - http://www.rcin.org.pl/igipz/Content/65841/PDF/WA51_84761_r2018-t90-z1_Przeg-Geogr-Mostowik.pdf M3 - Text J2 - Przegląd Geograficzny T. 90 z. 1 (2018) PY - 2018 IS - 1 EP - 110 KW - water resources KW - recession curves KW - underground run-off KW - Flysch Carpathians A1 - Mostowik, Karolina A1 - Kisiel, Marta A1 - Rzonca, Bartłomiej A1 - Siwek, Janusz PB - IGiPZ PAN VL - 90 CY - Warszawa SP - 93 T1 - Potencjał zasobności zbiorników wód podziemnych w Bieszczadach Wysokich = The storage capacity of groundwater reservoirs in the High Bieszczady Mountains (SE Poland) UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/65841 ER - TY - GEN PB - IGiPZ PAN N1 - 24 cm L1 - http://www.rcin.org.pl/igipz/Content/8688/PDF/WA51_16378_r1969-t41-z3_Przeg-Geogr.pdf M3 - Text CY - Warszawa PY - 1969 KW - water balance KW - water economy KW - water resources KW - geomorphology KW - palaeohydrology KW - marginal zones KW - deglaciation KW - synthesis of regions KW - postglacial lakes KW - spatial planning KW - gypsy population KW - geographical environment KW - Gorzów Wielkopolski KW - Gardno-Łeba Lowland KW - Grajewo county KW - Vistula river valley KW - Świecie Plain KW - Volga delta T1 - Przegląd Geograficzny T. 41 z. 3 (1969) UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/8688 ER -