Zobrazeno 1 - 10
of 51
pro vyhledávání: '"Václav Škarpich"'
Publikováno v:
Acta Universitatis Carolinae Geographica, Vol 59, Iss 1, Pp 108-119 (2024)
Gravel and sandy bars constitute critical components of river channel morphology, yet their morphodynamics in large, heavily regulated rivers during periods without significant flows remain poorly understood. This study investigates changes in surfac
Externí odkaz:
https://doaj.org/article/246e6ad61770437a810c391337dd4d0d
Publikováno v:
Acta Scientiarum Polonorum. Formatio Circumiectus, Vol 16, Iss 1, Pp 237-246 (2017)
Wolman [1954] pebble sampling is the most commonly used method to estimate surface bed grain sizes in gravel-bed streams. A few studies documented different results between individual operators or repeated measurements within the same channel-reach o
Externí odkaz:
https://doaj.org/article/860b963e2d2848d9833930800804d6ef
Autor:
Tomáš Galia, Václav Škarpich
Publikováno v:
Acta Scientiarum Polonorum. Formatio Circumiectus, Vol 14, Iss 2, Pp 57-64 (2015)
Bankfull widths of steep headwater channels were examined in the Western Carpathian flysch midmountains. The criteria of the top of banks, scoured lines and presence of bank vegetation were helpful in the bankfull width determination. A direct down
Externí odkaz:
https://doaj.org/article/298807ebbcbc48aaa08888fbc5c57fe4
Akademický článek
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Autor:
Tomáš Galia, Václav Škarpich, Leonidas Vardakas, Elias Dimitriou, Yiannis Panagopoulos, Vilém Spálovský
Publikováno v:
Earth Surface Processes and Landforms. 48:997-1010
Publikováno v:
Ecohydrology & Hydrobiology. 22:553-564
Publikováno v:
Check Dam Construction for Sustainable Watershed Management and Planning. :245-252
Meander bends are perceived as sites with high large wood (LW) retention potential by trapping transported LW at their concave banks or on point bars. We employed five field inventories between 2016 and 2022 (2016, 2019, 2020, 2021 and 2022) in 13 su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c544a18315c5a384a4b06de83e34a808
https://doi.org/10.5194/egusphere-egu23-3080
https://doi.org/10.5194/egusphere-egu23-3080
Publikováno v:
Environmental Earth Sciences. 82
Publikováno v:
CATENA. 224:106973