Hydrologic Response Function

A Hydrologic Response Function is a mathematical representation that characterizes the temporal transformation of effective precipitation into streamflow within a watershed, distinguishing itself from other hydrologic models by explicitly describing the catchment’s impulse response to input forcings.

152

Publications

8.7K

Citations

423

Authors

221

Institutions

Publications per year

2017–2026

29

Publications

152

1–5 of 152

Authors

423

  1. AR
    Andrea Rinaldo

    University of Padua, Italy

    6 publications · 513 citations

    6

    h-index

  2. GB
    Gianluca Botter

    University of Padua, Italy

    6 publications · 478 citations

    6

    h-index

  3. KL
    Keith Loague

    Stanford University, United States

    6 publications · 364 citations

    6

    h-index

  4. MS
    Murugesu Sivapalan

    University of Illinois Urbana-Champaign, United States

    4 publications · 906 citations

    4

    h-index

  5. MD
    Michele Di Lazzaro

    Roma Tre University, Italy

    4 publications · 90 citations

    4

    h-index

1–5 of 423

Venues

  1. Water Resources Research

    32 publications · 2.3K citations

    26

    h-index

  2. Journal of Hydrology

    22 publications · 932 citations

    17

    h-index

  3. Hydrological Processes

    18 publications · 930 citations

    17

    h-index

  4. Hydrology and earth system sciences

    7 publications · 1.1K citations

    7

    h-index

  5. 6

    h-index

1–5