TY - GEN A2 - Kotarba, Adam (1938– ). Ed. A2 - Kozłowska, Anna (1948– ). Ed. PB - IGiPZ PAN PB - Continuo N1 - 132 pp., [2] l. pl., [1] l. pl. col. : phot., maps ; 24 cm N1 - Bibliogr. N1 - Summ. eng. L1 - http://www.rcin.org.pl/igipz/Content/596/PDF/Wa51_3575_r1999-nr174_Prace-Geogr.pdf M3 - Text CY - Wrocław J2 - Prace Geograficzne = Geographical Studies / Polska Akademia Nauk. Instytut Geografii i Przestrzennego Zagospodarowania im. Stanisława Leszczyckiego ; nr 174 PY - 1999 KW - geoecological research KW - geoecology KW - high-mountain environment KW - high-mountain relief KW - high-mountain soils KW - high-mountain vegetation KW - snow cover KW - Tatra Mountains KW - Kasprowy Wierch T1 - Badania geoekologiczne w otoczeniu Kasprowego Wierchu = Geoecological research in the Kasprowy Wierch area UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/596 ER - TY - GEN A1 - Kotarba, Adam (1938– ) A1 - Kaszowski, Ludwik (1939– ) A1 - Krzemień, Kazimierz (1951– ) PB - Ossolineum PB - IGiPZ PAN N1 - 106 pp. : phot. ; 24 cm N1 - Bibliogr. p. [100]-104 N1 - Summary in Polish. L1 - http://www.rcin.org.pl/igipz/Content/18828/PDF/WA51_35225_r1987-nr3_Geogr-Stud-Special-I.pdf M3 - Text CY - Wrocław J2 - Geographical Studies. Special Issue / Polish Academy of Sciences. Institute of Geography and Spatial Organization, no. 3 PY - 1987 KW - geomorphology KW - denudation KW - high mountains KW - Tatra Mountains T1 - High-mountain denudational system of the Polish Tatra Mountains = Wysokogórski system denudacyjny Tatr Polskich UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/18828 ER - TY - GEN N1 - 24 cm N2 - The article presents a review of research into the thermal structure and ice cover characterising lakes in Poland’s Tatra Mountains, on the basis of two centuries of scientific publications appearing up to 2015. The literature review allowed for the identification of five periods in which research was of differing intensities and quality. The first research carried out in the 19th century is seen to be of limited scientific value, mostly being limited to one-off measurements of morphometry and thermal conditions in the Tatra Mountain lakes. Only the research done by L. Birkenmayer can be regarded as well-planned, detailed and continuous in nature. By contrast, measurements made in the 20th century (mainly on the basis of the better measuring devices making their appearance) have yielded many interesting studies on the thermal conditions present in Tatra Mountain lakes. The measurements made by Lityński were especially important, due to his new and extended classification of Tatra lakes based on changes in water temperature in the summer season and the thermal stratification present through the year. In turn, in the inter-War period, studies became more systematic on both slopes of the Tatra Mountains, and were primarily concerned with winter oxygen content in relation to water temperature. This work bore fruit in the thermal classification of Tatra lakes developed by Szaflarski, who took account of the time at which lakes iced over, as well as maximum temperatures of surface water. After World War II, study of the vertical distribution of temperature in the Tatra lakes was continued with at different times of the year. Here, the result was a distinction drawn in winter between two main types of thermal system. An important event influencing research on lakes in the Tatra Mountains was the ongoing observation of ice-cover thicknesses on the Morskie Oko tarn beginning in 1951 and being engaged in by the Institute of Meteorology and Water Management. Device development in following years brought the extension of the field study and an increase in the accuracy of measurement of thermal conditions in lakes. The first work on the influence of contemporary climate changes on surface water and the development of ice cover on high-altitude lakes was also carried out and then published. In the second half of the 20th century, the study of maximum ice thicknesses and durations of ice-related events on Morskie Oko confirmed the disappearance of ice phenomena on this lake. Measurement allowed for a better understanding of the relationship between the thickness of the ice cover and lake depth; the dynamics and direction of light and temperature transformations, and the conditioning of stability where the summer stratification of Tatra lakes is concerned. In recent years, the use of thermal imaging cameras to record the dynamics of water temperatures of the surface layer has allowed changes in water temperature at any time interval to be encapsulated. In the context of the literature review of the subject matter, the author poses several questions concerning the extension of modern research to other lakes and further directions of research into the thermal and ice-cover conditions characterising the Tatra lakes. Research on the waters and ice cover of these lakes over 200 years has not given rise to a comprehensive and up-to-date study. This work is therefore an attempt to trace the development of research on the variation and formation of thermal conditions in Tatra Mountain lakes. L1 - http://www.rcin.org.pl/igipz/Content/63172/PDF/WA51_82919_r2017-t89-z3_Przeg-Geogr-Szumny.pdf M3 - Text J2 - Przegląd Geograficzny T. 89 z. 3 (2017) PY - 2017 IS - 3 EP - 512 KW - hydrology KW - history KW - high mountains KW - Carpathians KW - Central and Eastern Europe A1 - Szumny, Mirosław PB - IGiPZ PAN VL - 89 CY - Warszawa SP - 491 T1 - Zarys rozwoju badań termiki wód i pokrywy lodowej jezior w polskich Tatrach = A general review of research into waters’ thermal structure and lake ice cover in the Polish Tatra Mountains UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/63172 ER - TY - GEN A2 - Rączkowska, Zofia (1953– ). Ed. A2 - Starkel, Leszek (1931– ). Ed. PB - IGiPZ PAN N1 - 133 pp. ; 24 cm L1 - http://www.rcin.org.pl/igipz/Content/87/PDF/Polonica%201%202008.pdf M3 - Text CY - Warszawa J2 - Modelling of high-mountain relief PY - 2008 KW - high-mountain relief KW - permafrost KW - glaciers KW - geomorphology KW - Canada KW - Alps KW - Carpathians KW - Sudety Mountains KW - Tatra Mountains KW - Bohemian Massif T1 - Geographia Polonica Vol. 81 No. 1 (2008) UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/87 ER - TY - GEN N1 - 24 cm L1 - http://www.rcin.org.pl/igipz/Content/35478/PDF/WA51_53137_r2013-t85-z3_Przeg-Geogr-Fidelus.pdf M3 - Text J2 - Przegląd Geograficzny T. 85 z. 3 (2013) PY - 2013 IS - 3 EP - 434 KW - slopes KW - man and environment KW - touristic movement KW - high mountains KW - West Tatra Mountains KW - Poland A1 - Fidelus, Joanna A2 - Płaczkowska, Eliza PB - IGiPZ PAN VL - 85 CY - Warszawa SP - 417 T1 - Współczesne przekształcanie stoków w Tatrach Zachodnich – na przykładzie ścieżek turystycznych i fragmentów stoków bez oddziaływania antropogenicznego = Contemporary transformation of slopes in the Western Tatras - as exemplified by fragments with tourist footpaths or UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/35478 ER - TY - GEN PB - IGiPZ PAN N1 - 24 cm L1 - http://www.rcin.org.pl/igipz/Content/77/PDF/2006-78_3-final.pdf M3 - Text CY - Warszawa PY - 2006 KW - structural geomorphology KW - land use KW - morphogenetic processes KW - anthropopression KW - tors morphology KW - geoecological catena KW - high mountains landscape KW - heat waves KW - mammals KW - Tatra Mountains KW - Sudety Mountains KW - Stołowe Mountains T1 - Przegląd Geograficzny T. 78 z. 3 (2006) UR - http://www.rcin.org.pl/igipz/dlibra/publication/edition/77 ER -