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Publikační činnost
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Typ záznamu:
stať ve sborníku (D)
Domácí pracoviště:
Katedra fyzické geografie a geoekologie (31600)
Název:
Parameters, longitudinal distribution and dynamics of large wood in a Mediterranean ephemeral stream.
Citace
Galia, T., Škarpich, V., Tichavský, R., Vardakas, L. a Šilhán, K. Parameters, longitudinal distribution and dynamics of large wood in a Mediterranean ephemeral stream..
In:
State of geomorphological research in 2018: Geomorfologický sborník 16 2018-04-25 Vílanec.
Brno: Institute of Geonics of the CAS, Masaryk University, 2018. s. 32-32. ISBN 978-80-86407-77-7.
Podnázev
Rok vydání:
2018
Obor:
Zemský magnetismus, geodesie, geografie
Počet stran:
1
Strana od:
32
Strana do:
32
Forma vydání:
Paměťový nosič
Kód ISBN:
978-80-86407-77-7
Kód ISSN:
Název sborníku:
Geomorfologický sborník 16
Sborník:
Mezinárodní
Název nakladatele:
Institute of Geonics of the CAS, Masaryk University
Místo vydání:
Brno
Stát vydání:
Sborník vydaný v ČR
Název konference:
State of geomorphological research in 2018
Místo konání konference:
Vílanec
Datum zahájení konference:
Typ akce podle státní
příslušnosti účastníků akce:
Evropská akce
Kód UT WoS:
EID:
Klíčová slova anglicky:
large wood, ephemeral stream, Mediterranean, Crete
Popis v původním jazyce:
Many scientific papers have acknowledged the importance of large wood (LW) in the geomorphic functions of rivers and streams and its unique benefits for aquatic biota (e.g., increased habitat heterogeneity, providing source of food, creation of refuges for aquatic organisms). Although LW has been intensively studied in forested basins of humid temperate climates, data on LW patterns coming from different fluvial environments are scarce. We investigated the dimensions, characteristics, longitudinal distribution, and dynamics of LW along a 4.05-km-long reach of an ephemeral channel typical of semi-arid European Mediterranean mountainous landscape (Sfakiano Gorge, Crete, Greece). We analysed a total of 795 LW pieces, and the mean observed abundance of LW was generally lower (14.3 m3 per hectare of active valley floor or 19.6 LW pieces per 100 m of stream length) than is usually documented for more humid environments. The number of LW pieces was primarily controlled by trees growing on the valley floor, whereas LW recruitment from steep adjacent hillslopes was less important. The valley floor width and the distance from the coastline (the moisture gradient) played crucial roles in the distribution of living trees as the main source of LW for the studied channel. These living trees acted as important LW supply agents (by tree throws or the supply of individual branches with sufficient LW dimensions) and flow obstructions during large flood events, causing storage of transported LW pieces in jams.
Popis v anglickém jazyce:
Seznam ohlasů
Ohlas
R01:
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