TY - GEN A1 - Bochenek, Witold. Autor PB - Instytut Geografii i Przestrzennego Zgospodarowania im. Stanisława Leszczyckiego, Polska Akademia Nauk N1 - 182 pages : color illustrations ; 24 cm N1 - Bibliography on pages 163-177 N1 - English summary L1 - http://www.rcin.org.pl/igipz/Content/143571/PDF/WA51_178719_r2020-nr271_Prace-Geogr.pdf M3 - Text CY - Warszawa J2 - Prace Geograficzne / Polska Akademia Nauk. Instytut Geografii i Przestrzennego Zagospodarowania im. Stanisława Leszczyckiego, nr 271 PY - © copyright 2020 KW - hydrology KW - climate change KW - human impact KW - Bystrzanka catchment T1 - Prawidłowości obiegu wody na obszarze beskidzko-pogórskim Karpat Zachodnich na przykładzie zlewni Bystrzanki w świetle zmian klimatu i działalności człowieka = Regularities of the water cycle in the Western Carpathians Beskids-foothills area based on th UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/143571 ER - TY - GEN N1 - 24 cm N2 - Water flow in the Polish Carpathians was exemplified by long-term (1988‑2017) analysis of two foothill catchments (of the Skawinka and Stobnica) and two catchments in the Beskidy Mountains (of the Soła and Osława). The work allowed for the determination of the duration of low flows and outflow deficits in relation to changes in thermal and precipitation conditions, as well as land use and land cover. In the selected catchments, the 30-year period brought a decrease in the area of arable land and an increase in the area of grassland and forest. In addition built-up areas increased by 495% between 1990 and 2018. A greater susceptibility to the occurrence of total drought was noted for the Beskidy Mountains catchments, in which the duration of low flows and outflow deficit was greater than in the foothill catchments. At the same time, the mountain catchments proved less susceptible to the emergence of deep drought, on account of their higher levels of forest cover and levels of soil permeability. In regional terms, the durations of low flows and outflow deficits were greater in the catchments located in the eastern part of the Carpathians (those of the Stobnica and Osława), in line with this area’s intensified features of a continental climate. L1 - http://www.rcin.org.pl/igipz/Content/182726/PDF/WA51_214097_r2021-t93-z1_Przeg-Geogr-Bochenek.pdf M3 - Text J2 - Przegląd Geograficzny T. 93 z. 1 (2021) PY - 2021 IS - 1 EP - 25 KW - low flow KW - threshold level method KW - aridity index KW - land use and land cover changes KW - Polish Carpathians A1 - Bochenek, Witold. Autor A1 - Kijowska-Strugała, Małgorzata. Autor PB - IGiPZ PAN VL - 93 CY - Warszawa SP - 5 T1 - Zmienność przepływów niżówkowych w wybranych zlewniach pogórskich i beskidzkich w latach 1988‑2017 = Variability of low flow in Polish Carpathians (foothills and Beskidy Mountains) catchments in the period 1988‑2017 UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/182726 ER - TY - GEN N1 - 24 cm N2 - The aim of this study has been to analyse long-term (1971–2015) changes in climatic conditions in the foothills and Beskid region of the Western Carpathian Mountains (South-Eastern Poland), on the basis of selected geoindicators calculated by reference to average annual and monthly air temperatures and precipitation. Climatic conditions were analysed for the Szymbark Research Station of the Institute of Geography and Spatial Organization of the Polish Academy of Sciences (IGSO PAS). Average daily air temperature and daily amounts of precipitation were referred to. The average annual temperature over the 45 years (1971–2015) was 8.1°C. The annual temperature ranged from 6.3°C (1980) to 9.9°C (2014). In the multi-year period analysed, there was an increase in the average annual temperature of about 0.4°C/10 years, which testifies to an intensification of continental climatic characteristics, confirming the course of and trends of two geoindicators of climate, i.e. oceanism after Marsz (Oc) and continentalism after Gorczynski (KG). This increased average annual temperature has the effect of shifting the onset of the thermal pre-winter period (5-0° C) to the end of the year, while also increasing the length of the growing season, by an average of 5 days/10 years. The multi-year period analysed has also witnessed a decrease in the number of cold months. The average annual precipitation was 834 mm (1971–2015). This contrasts with the maximum amount (of 1164 mm) noted in 1974, as well as the minimum (of 535 mm) recorded in 1982. Overall, annual rainfall increased, by 16.2 mm/10 years. However, the rainfall geoindicator (LAN) showed a downward trend due to the increased the average annual air temperature. Equally, the pluviometric geoindicator P showed an increased trend influenced by ever-greater annual amplitude of temperature. Based on the classifications of monthly temperature and precipitation, it was find an increased trend of warm and wet months, as associated with a reduced incidence of cold and dry months. The values of indicators calculated for the Szymbark Research Station in 1971–2015 are similar to those recorded in other mountainous areas in Europe. L1 - http://www.rcin.org.pl/igipz/Content/65838/PDF/WA51_84751_r2018-t90-z1_Przeg-Geogr-Bochenek.pdf M3 - Text J2 - Przegląd Geograficzny T. 90 z. 1 (2018) PY - 2018 IS - 1 EP - 52 KW - air temperature KW - precipitation KW - climatic indices KW - Szymbark KW - Western Carpathians A1 - Bochenek, Witold A1 - Kijowska-Strugała, Małgorzata A1 - Kiszka, Krzysztof PB - IGiPZ PAN VL - 90 CY - Warszawa SP - 35 T1 - Wieloletnie tendencje warunków klimatycznych w Szymbarku na podstawie wybranych wskaźników = Long-term climatic trends in Szymbark (Poland), based on selected indicators UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/65838 ER -