References
- Adrian, R., O’Reilly, C.M., Zagarese, H., Baines, S.B., Hessen, D.O., Keller, W., Livingstone, D.M., Sommaruga, R., Straile, D., Van Donk, E., Weyhenmeyer, G.A. & Winder M. (2009). Lakes as sentinels of climate change. Limnol. Oceanogr., 54(6), 2283−2297. DOI: 10.4319/lo.2009.54.6_part_2.2283.10.4319/lo.2009.54.6_part_2.2283285482620396409
- Baumgart-Kotarba, M. & Kotarba A. (2001). Deglaciation in the Sucha Woda and Pańszczyca Valleys in the Polish High Tatras. Studia Geomorphologica Carpatho-Balcanica, 35, 7−38.
- Boltižiar, M. (2007). Štruktúra vysokohorskej krajiny Tatier. Nitra: ÚKE SAV.
- Dąbrowska, K. & Guzik M. (Eds.) (2015). Atlas of the Tatra Mountains – Abiotic Nature. Zakopane: Wydawnictwo Tatrzańskiego Parku Narodowego.
- Długosz, M. & Kapusta J. (2015). Debris flows. (Plate V.2). In K. Dąbrowska & M. Guzik (Eds.), Atlas of the Tatra Mountains – Abiotic Nature. Zakopane: Wydawnictwo Tatrzańskiego Parku Narodowego.
- Dyakowska, J. (1932). Analiza pyłkowa kilku torfowisk tatrzańskich. Acta Botanica Polonica, 9(3−4), 473−530.10.5586/asbp.1932.018
- Emmer, A., Merkl, S. & Mergili M. (2015). Spatiotemporal patterns of high-mountain lakes and related hazards in western Austria. Geomorphology, 246, 602−616. DOI: 10.1016/j.geomorph.2015.06.032.10.1016/j.geomorph.2015.06.032
- Engel, Z., Mentlík, P., Braucher, R., Minár, J., Léanni, L. & Team A. (2015). Geomorphological evidence and 10Be exposure ages for the Last Glacial Maximum and deglaciation of the Veľká and Malá Studená dolina valleys in the High Tatra Mountains, central Europe. Quaternary Science Reviews, 124, 106−123. DOI: 10.1016/j.quascirev.2015.07.015.10.1016/j.quascirev.2015.07.015
- Falťan, V. & Bánovský M. (2008). Changes in land cover in the area of Vyšné Hágy-Starý Smokovec, impacted by the wind calamity in November 2004 (Slovakia). Moravian Geographical Reports, 16, 16–26.
- Feranec, J., Cebecauer, J. & Oťaheľ J. (2005). Photo-to-photo interpretation manual. Bratislava: Institute of Geography, Slovak Academy of Sciences, BIOPRESS.
- Gądek, B., Grabiec, M. & Kędzia S. (2015). Application of ground penetrating radar to identification of thickness and structure of sediments in postglacial lakes, illustrated with an example of the Mały Staw lake (the Karkonosze Mts.). Studia Geomorphologica Carpatho-Balcanica, 49, 5−13. DOI: 10.1515/sgcb-2015-0006.10.1515/sgcb-2015-0006
- Gallik, J. & Bolešová L. (2016). sUAS and their application in observing geomorphological processes. Solid Earth, 7, 1033–1042. DOI: 10.5194/se-7-1033-2016.10.5194/se-7-1033-2016
- Gerten, D. & Adrian R. (2000). Climate-driven changes in spring plankton dynamics and the sensitivity of shallow polymictic lakes to the North Atlantic Oscillation. Limnol. Oceanogr., 45, 1058−1066. DOI: 10.4319/lo.2000.45.5.1058.10.4319/lo.2000.45.5.1058
- Gregor, V. & Pacl J. (2005). Hydrológia tatranských jazier. Acta Hydrologica Slovaca, 6(1), 161−187.
- Haladová, I. & Petrovič F. (2015). Classification of land use changes (model area: Nitra town). Ekológia (Bratislava), 34(3), 249−259. DOI: 10.1515/eko-2015-0024.10.1515/eko-2015-0024
- Hamerlík, L. & Bitušík P. (2009). The distribution of littoral chironomids along an altitudinal gradient in High Tatra Mountain lakes: Could they be used as indicators of climate change? Ann. Limnol. – International Journal of Limnology, 45, 145−156. DOI: 10.1051/limn/2009021.10.1051/limn/2009021
- Hreško, J., Kanásová, D., Bugár, G., Petrovič, F. & Mačutek J. (2012). Morphodynamic effect on lacustrine deposits in the High Tatra Mts. Ekológia (Bratislava), 31(4), 390−404. DOI: 10.4149/ekol_2012_03_390.10.4149/ekol_2012_03_390
- Hutchinson, S.M., Akinyemi, F.O., Mîndrescu, M., Begy, R. & Feurdean A. (2016). Recent sediment accumulation rates in contrasting lakes in the Carpathians (Romania): impacts of shifts in socio-economic regime. Regional Environmental Change, 16(2), 501−513. DOI: 10.1007/S10113-015-0764-7.10.1007/s10113-015-0764-7
- Irmler, R., Daut, G. & Mäusbacher R. (2006). A debris flow calendar derived from sediments of lake Lago di Braies (N. Italy). Geomorphology, 77, 69−78. DOI: 10.1016/j.geomorph.2006.01.013.10.1016/j.geomorph.2006.01.013
- Ives, J.D., Shrestha, R.B. & Mool P.K. (2010). Formation of Glacial Lakes in the Hindu Kush-Himalayas and GLOF Risk Assessment. Kathmandu: ICIMOD.10.53055/ICIMOD.521
- Kaczka, R., Lempa, M., Czajka, B., Janecka, K., Rączkowska, Z., Hreško, J. & Bugár G. (2015). The recent timberline changes in the Tatra Mountains: a case study of the Mengusovská valley (Slovakia) and the Rybi potok valley (Poland). Geographia Polonica, 88(2), 71−83. DOI: 10.7163/GPol.0016.10.7163/GPol.0016
- Kapusta, J., Stankoviansky, M. & Boltižiar M. (2010). Changes in activity and geomorphic effectiveness of debris flows in the High Tatra Mts. within the last six decades (on the example of the Velická dolina and Dolina Zeleného plesa valleys). Studia Geomorphologica Carpatho-Balcanica, 44, 5−34.
- Kapusta, J. (2016). Metodika rekonštrukcie brehovej čiary tatranských plies. Rigorózna práca, UKF Nitra.
- Kłapyta, P., Zasadni, J., Pociask-Karteczka, J., Gajda, A. & Franczak P. (2015). Late Glacial and Holocene paleoenvironmental records in the Tatra Mountains, East-Central Europe, based on lake, peat bog and colluvial sedimentary data: A summary review. Quaternary International, 415, 126−144. DOI: 10.1016/j.quaint.2015.10.049.10.1016/j.quaint.2015.10.049
- Kohler, T., Wehrli, A. & Jurek M. (Eds.) (2014). Mountains and climate change: A global concern. Sustainable Mountain Development Series. Bern: Centre for Development and Environment (CDE), Swiss Agency for Development and Cooperation (SDC), Geographica Bernensia.
- Kotarba, A. (1996). Osady jeziorne jako wskaźnik przemian środowiska naturalnego Tatr Wysokich. In A. Kotarba (Ed.), Z badań fizycznogeograficznych w Tatrach, Dokumentacja Geograficzna, 4 (pp. 33−47). Warszawa: IGiPZ PAN.
- Kotarba, A. (2004). Rola małej epoki lodowej w przekształcaniu śrdowiska Tatr. Warszawa: IGiPZ PAN.
- Krippel, E. (1963). Postglaciálny vývoj lesov Tatranského národného parku. Biologické práce, 9(40), 5−44.
- Kubinský, D., Weis, K., Fuska, J., Lehotský, M. & Petrovič F. (2015). Changes in retention characteristics of 9 historical artificial water reservoirs near Banská Štiavnica, Slovakia. Open Geosciences, 1, 1−8. DOI: 10.1515/geo-2015-0056.10.1515/geo-2015-0056
- Łajczak, A. (2014). Rola podłoża w rozwoju torfowisk w polskich Karpatach. Studia Limnologica et Telmatologica, 8(1), 19−36.
- Lukniš, M. (1973). Reliéf vysokých Tatier a ich predpolia. Bratislava: SAV.
- Mason, I., Guzkowska, M., Rapley, C. & Street-Perrott F. (1994). The response of lake levels and areas to climatic change. Clim. Change, 27, 161−197. DOI: 10.1007/BF01093590.10.1007/BF01093590
- Mîndrescu, M., Cristea, I. & Hutchinson S.M. (2010). Bathymetric and sedimentological changes of glacial Lake Ştiol, Rodna Masiff. Carpathian Journal of Earth Environmental Sciences, 5(1), 57−65.
- Necsoiu, M., Dinwiddie, C.L., Walter, G.R., Larsen, A. & Stothoff S.A. (2013). Multitemporal image analysis of historical aerial photographs and recent satellite imagery reveals evolution of water body surface area and polygonal terrain morphology in Kobuk Valley National Park, Alaska. Environmental Research Letters, 8(2), 025007. DOI: 10.1088/1748–9326/8/2/025007.10.1088/17489326/8/2/025007
- Obidowicz, A. (1996). A Late glacial-Holocene history of the formation of vegetation belts in the Tatra Mts. Acta Paleobot., 36(2), 159−206.
- Owens, P. & Slaymaker O. (1994). Post-glacial temporal variability of sediment accumulation in a small alpine lake. Variability in Stream Erosion and Sediment Transport. Proceedings of the Canberra Symposium, December 1994. International Association of Hydrological Sciences, 224, 187−195.
- Rybníčková, E. & Rybníček K. (2005). Pollen and macroscopic analyses of sediments from two lakes in the High Tatra mountains, Slovakia. Veg. Hist. Archaeobot., 15, 345−356. DOI: 10.1007/s00334-006-0050-1.10.1007/s00334-006-0050-1
- Solár, J. (2013). Effect of climate change on Mountain Pine distribution in Western Tatra Mountains. In B.R. Singh (Ed.), Change - Realities, Impacts Over Ice Cap, Sea Level and Risks, pp. 437−458. Rijeka: InTech. DOI: 10.5772/54724.10.5772/54724
- Solár, J. & Janiga M. (2013). Long-term changes in Dwarf Pine (Pinus mugo) cover in the High Tatra Mountains, Slovakia. Mt. Res. Dev., 33(1), 51−62. DOI: 10.1659/MRD-JOURNAL-D-12-00079.1.10.1659/MRD--D-12-00079.1
- Strozzi, T., Wiesmann, A., Kääb, A., Joshi, S. & Mool P. (2012). Glacial lake mapping with very high resolution satellite SAR data. Natural Hazards and Earth System Sciences, 12, 2487−2498. DOI: 10.5194/nhess-12-2487-2012.10.5194/nhess-12-2487-2012
- Šporka, F., Štefková, E., Bitušík, P., Thompson, A.R., Agustí-Panareda, A., Appleby, P.G., Grytnes, J.A., Kamenik, C., Krno, I., Lami, A., Rose, N. & Shilland N.E. (2002). The paleolimnological analysis of sediments from High Mountain Lake Nižné Terianske pleso in the High Tatras (Slovakia). J. Paleolimnol., 28, 95−109. DOI: 10.1023/A:1020376003123.10.1023/A:1020376003123
- Zasadni, J. & Kłapyta P. (2014). The Tatra Mountains during the Last Glacial Maximum. Journal of Maps, 10(3), 440−456. DOI: 10.1080/17445647.2014.885854.10.1080/17445647.2014.885854