Stream Sinuosity

Stream Sinuosity is a dimensionless geomorphological metric that quantifies the degree of meandering in a river channel by the ratio of the channel's actual thalweg length to the straight-line downvalley distance, distinguishing it from other measures of channel complexity through its specific focus on path elongation.

54

Publications

3.7K

Citations

123

Authors

74

Institutions

Publications per year

2017–2026

4

Authors

123

  1. GT
    Gábor Tímár

    Eötvös Loránd University, Hungary

    5 publications · 265 citations

    5

    h-index

  2. JP
    Judit Petrovszki

    Eötvös Loránd University, Hungary

    3 publications · 86 citations

    3

    h-index

  3. JZ
    John Z. Seaberg

    University of Minnesota, United States

    2 publications · 189 citations

    2

    h-index

  4. BS
    Balázs Székely

    Eötvös Loránd University, Hungary

    2 publications · 122 citations

    2

    h-index

  5. RL
    Roger LeB. Hooke

    University of Minnesota, United States

    2 publications · 189 citations

    2

    h-index

1–5 of 123

Venues

  1. Water Resources Research

    3 publications · 604 citations

    3

    h-index

  2. Geomorphology

    3 publications · 145 citations

    3

    h-index

  3. Journal of Sedimentary Research

    JSR · 3 publications · 163 citations

    3

    h-index

  4. Earth Surface Processes and Landforms

    3 publications · 271 citations

    3

    h-index

  5. 3

    h-index

1–5