Canopy Evaporation

Canopy Evaporation is a microclimatic process representing the latent heat exchange mechanism by which intercepted precipitation or dew on vegetative surfaces transitions directly to vapor without infiltrating the soil, distinguished from other evapotranspiration components by its exclusive origin from intercepted water rather than root-uptaken moisture.

227

Publications

23.8K

Citations

708

Authors

290

Institutions

Publications per year

2017–2026

35

Authors

708

  1. JB
    J.D. Beresford

    Commonwealth Scientific and Industrial Research Organisation, Australia

    5 publications · 189 citations

    5

    h-index

  2. AL
    Anders Lindroth

    Lund University, Sweden

    5 publications · 276 citations

    5

    h-index

  3. EG
    E.A.N. Greenwood

    Commonwealth Scientific and Industrial Research Organisation, Australia

    5 publications · 189 citations

    5

    h-index

  4. JH
    J. H. C. Gash

    UK Centre for Ecology & Hydrology, United Kingdom

    5 publications · 985 citations

    5

    h-index

  5. DD
    David D. Breshears

    University of Arizona, United States

    5 publications · 712 citations

    5

    h-index

1–5 of 708

Venues

  1. Agricultural and Forest Meteorology

    32 publications · 2.6K citations

    26

    h-index

  2. Hydrological Processes

    23 publications · 852 citations

    19

    h-index

  3. Journal of Hydrology

    21 publications · 974 citations

    18

    h-index

  4. Water Resources Research

    9 publications · 3.2K citations

    9

    h-index

  5. Ecohydrology

    8 publications · 349 citations

    8

    h-index

1–5