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The paper outlines changes in the channel morphology of the Ropa riverbed over the last six years, taking into account the role of large floods and the Klimkówka water reservoir in shaping the morphology of the riverbed. The analysis was based on annual geodetic measurements of the Ropa riverbed conducted between 2009–2014. The research was carried out in four cross profiles of the riverbed located upstream (1 profile) and downstream (3 profiles) of the reservoir. In order to recognise the direction and scale of morphology changes of the riverbed, additional analyses of water levels in the Ropa River was performed in the analysed multiannual period. The conducted analysis led to the conclusion that floods with extremely large discharges are the key factor causing the deepening of the riverbed downstream from the reservoir. It can be up to about 70 cm deep during a single event. The reservoir is just one additional factor of many which shape the direction and scale of changes to the riverbed. A significant role in modifying the riverbed morphology upstream from the reservoir is played by river control works, which diminish the effects of sediment accumulation occurring on this section.
Słowa kluczowe
Wydawca
Czasopismo
Rocznik
Tom
Strony
61--76
Opis fizyczny
Bibliogr. 23 poz., rys., tab., wykr., fot.
Twórcy
autor
- Department of Geoenvironmental Research, Institute of Geography and Spatial Organization, PAS; Św. Jana str. 2231-018 Kraków, Poland
autor
- Research Station in Szymbark, Institute of Geography and Spatial Organization, PAS; 38-311 Szymbark 430, Poland
autor
- Research Station in Szymbark, Institute of Geography and Spatial Organization, PAS; 38-311 Szymbark 430, Poland
Bibliografia
- Brandt S.A., 2000. Classification of geomorphological effects downstream of dams. Catena 40, 4, 375–401.
- Dauksza L., 1976. Zmiany koryta Ropy w świetle materiałów kartograficznych. [in:] Wykształcenie młodoczwartorzędowych aluwiów rzek karpackich i ich znaczenie surowcowe. L. Starkel, J. Rutkowski (eds.), 45–47.
- Dauksza L., 2009. The Ropa river channel changes during 20th century at Szymbark (Polish Flysch Carpathians). Studia Geomorphologica Carpatho–Balcanica 43, 115–126.
- Dauksza L., Gil E., 1972. Fluvial processes in the upper reaches of the Carpathian rivers during the Holocene, with special consideration of the activity of man in recent years. [in:] Excursion Guide-Book Symposium of the INQUA Commission on Studies of the Holocene. Changes in the paleogeography of valley floors during the Holocene. First part. The Polish Carpathians. The site II–4 The Ropa river valley, Poland, 12–20 September, 46–49.
- Dauksza L., Gil E., Soja R., 1982. The Holocene and present–day evolution of the mountaineous reach of the Ropa river valley. [in:] Evolution of the Vistula River Valley during the last 15 000 years. Part I. L. Starkel (ed.), Prace Geograficzne IG i PZ PAN, Spec. Issue 1, 21–39.
- Kondolf G. M., 1997. PROFILE: hungry water: effects of dams and gravel mining on river channels. Environmental management 21, 4, 533–551.
- Korpak J. 2008. Rola maksymalnych wezbrań w funkcjonowaniu systemów uregulowanych koryt górskich. Landform Analysis 8, 41–44.
- Korpak J., Krzemień K., Radecki-Pawlik A., 2008. Wpływ czynników antropogenicznych na zmiany koryt cieków karpackich. Infrastruktura i Ekologia Terenów Wiejskich 04, 88 pp., (in Polish with an English summary).
- Krzemień K. 2006. Badania struktury i dynamiki koryt rzek karpackich. Infrastruktura i ekologia terenów wiejskich 4, 1, 131–142.
- Książek L., 2006. Morfologia koryta rzeki Skawy w zasięgu cofki zbiornika Świnna Poręba (The morphology of the Skawa River bed within back-water reach of Świnna Poręba Reservoir). Infrastruktura i Ekologia Terenów Wiejskich 4, 1, 249–267, (In Polish with an English sumary).
- Liro M. 2014a. Conceptual Model For Assessing The Channel Changes Upstream From Dam Reservoir. Quaestiones Geographicae 33, 1, 61–74.
- Liro M., 2014b. Gravel-bed channel changes upstream of a reservoir: The case of the Dunajec River upstream of the Czorsztyn Reservoir, southern Poland. Geomorphology, DOI: 10.1016/j.geomorph.2014.10.030
- Łajczak A., 1995. Studium nad zamulaniem wybranych zbiorników zaporowych w dorzeczu Wisły. Monografie Komitetu Gospodarki Wodnej PAN 8, 108 pp.
- Makkaveyev N. I., 1972. The impact of large water engineering projects on geomorphic processes in stream valleys. Soviet Geography 13, 6, 387–393.
- Malarz R., 2004–2005. Geomorfologiczne skutki działania zapór wodnych w okresach powodziowych w dolinie Soły. Folia Geographica ser. Geographica-Physica 35–36, 53–64.
- Petts G. E., Gurnell A. M., 2005. Dams and geomorphology: research progress and future directions. Geomorphology 71, 1, 27–47.
- Soja R., 1977. Deepening of channel in the light of the cross profile analysis (Carpathian river as example). Studia Geomorphologica Carpatho–Balcanica 11, 128–138.
- Starkel L., 2003. Extreme meteorological events and their role in environmental changes, the economy and history. Paper in Global Change 10, 7–13.
- Wiejaczka Ł., 2010.Zbiorniki retencyjne w polskich Karpatach. Aura 10, 7–9.
- Wiejaczka Ł., 2011. Wpływ zbiornika wodnego Klimkówka na abiotyczne elementy środowiska przyrodniczego w dolinie Ropy. (The Influence of the Klimkówka Water Reservoir on the Abiotic Elements of the Natural Environment in the Ropa River Valley). Prace Geograficzne IGiPZ PAN 229, 144 pp., (in Polish with an English summary).
- Wiejaczka Ł., Bochenek W., 2013. Przekształcanie dna koryta rzeki górskiej w czasie dużych wezbrań na przykładzie Ropy. Prace Geograficzne 132, 27–38.
- Wiejaczka Ł., Kijowska M., 2011. Zmiany położenia dna koryt rzek karpackich (powyżej zbiornika retencyjnego) w świetle analizy stanów niskich. Monitoring Środowiska Przyrodniczego12, 137–143.
- Wyżga B., 2008. Wcinanie się rzek polskich Karpat w ciągu XX wieku. [in:] Stan środowiska rzek południowej Polski i możliwości jego poprawy — wybrane aspekty. B. Wyżga (ed.), Instytut Ochrony Przyrody PAN, Kraków, 7–39.
Typ dokumentu
Bibliografia
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