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Two decades of meander belt morphodynamics: How important is woody vegetation and in-channel large wood?

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F25%3AA2603A2A" target="_blank" >RIV/61988987:17310/25:A2603A2A - isvavai.cz</a>

  • Result on the web

    <a href="https://linkinghub.elsevier.com/retrieve/pii/S0341816224008701" target="_blank" >https://linkinghub.elsevier.com/retrieve/pii/S0341816224008701</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.catena.2024.108673" target="_blank" >10.1016/j.catena.2024.108673</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Two decades of meander belt morphodynamics: How important is woody vegetation and in-channel large wood?

  • Original language description

    Meandering rivers represent a common planform morphology in terrestrial environments, and their morphological evolution is a central focus in fluvial geomorphology. Despite this, the combined effects of living and dead woody vegetation on the dynamics of meandering rivers remain insufficiently understood and warrant further investigation. In this study, we focused beyond meander geometry to include the presence of woody vegetation and in-channel large wood as predictors of lateral shifts of the meander bends. We examined a 4-km-long reach of the Odra River in Czechia with a preserved active meandering pattern but a mosaic floodplain composed of woody patches and managed meadows. Over a 22-year period, we studied 13 subsequent meanders using detailed orthophoto analysis and hydrological regime analysis. A large flood event with a 20-year recurrence interval occurred in 2010, and a smaller flood event with a 5-year recurrence interval occurred in 2020. We found a negative relationship between the tested erosional parameters (annual bank retreat and annual eroded area) and two meander-scale parameters: meander amplitude and the proportion of woody vegetation along the outer meander bank. However, statistical significance was confirmed only for the period 2000-2009, characterized by frequent high flows and, consequently, the highest expended geomorphic work of flows. Conversely, we found a negligible role of large wood in erosional processes over the entire studied period. Additionally, we demonstrated that over the last two decades, the studied reach has been following an evolutionary trajectory characterized by increasing meander amplitude, sinuosity, and the proportion of woody vegetation along the outer meander banks. We documented that the activity of erosional processes decreases with increasing amplitude and proportion of woody vegetation, suggesting a further deceleration of meander morphodynamics in the near future.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10508 - Physical geography

Result continuities

  • Project

    <a href="/en/project/GA22-17474S" target="_blank" >GA22-17474S: Biogeomorphic interactions in meandering rivers across different spatiotemporal scales</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2025

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    CATENA

  • ISSN

    0341-8162

  • e-ISSN

    1872-6887

  • Volume of the periodical

  • Issue of the periodical within the volume

    February 2025

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    13

  • Pages from-to

  • UT code for WoS article

    001390437500001

  • EID of the result in the Scopus database

    2-s2.0-85212081460