Number of the records: 1  

Floods and floodplain changes of the River Morava, the Strážnické Pomoraví region (Czech Republic) over the past 130 years

  1. 1.
    SYSNO ASEP0367502
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleFloods and floodplain changes of the River Morava, the Strážnické Pomoraví region (Czech Republic) over the past 130 years
    Author(s) Brázdil, R. (CZ)
    Máčka, Z. (CZ)
    Řezníčková, L. (CZ)
    Soukalová, E. (CZ)
    Dobrovolný, P. (CZ)
    Grygar, Tomáš (UACH-T)
    Source TitleHydrological Sciences Journal. - : Taylor & Francis - ISSN 0262-6667
    Roč. 56, č. 7 (2011), s. 1166-1185
    Number of pages20 s.
    Languageeng - English
    CountryGB - United Kingdom
    Keywordsflood ; floodplain change ; channel change ; anabranching system ; Strážnické Pomoraví ; River Morava
    Subject RIVDA - Hydrology ; Limnology
    R&D ProjectsIAAX00130801 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    CEZAV0Z40320502 - UACH-T (2005-2011)
    UT WOS000297289600007
    DOI10.1080/02626667.2011.608359
    AnnotationThe development of the River Morava floodplain has been influenced by several natural and anthropogenic factors. This paper focuses on variations in flood activity and channel changes of the River Morava in the region of Strážnické Pomoraví (southeastern Czech Republic). Floods are analysed in terms of measured peak water stages, Hk (Rohatec, 1886-1920) and peak discharges Qk (Rohatec/Strážnice, 1921-2010) evaluated with respect to their N-year return period (HN or QN). The frequency of floods with Qk ? Q2 reaches a significant maximum in March, followed by July. According to flood series compiled from 1881 onwards, their frequency peaked in the 1961-1970 decade with the most severe events occurring in July 1997 (Q100), March 2006 and June 2010 (Q50). During the study period the natural dynamics of the original anabranching channel patterns were significantly modified by human intervention, such as the abandonment of some anabranching channels, channel straightening, enlargement of the main channel, flood-dike construction, and the creation of the Bat'a shipping channel. These changes resulted in decreased frequency and a reduction in the extent of floodplain inundations compared to the period prior to channel modifications in the 1930s.
    WorkplaceInstitute of Inorganic Chemistry
    ContactJana Kroneislová, krone@iic.cas.cz, Tel.: 311 236 931
    Year of Publishing2012
Number of the records: 1  

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