Vertical Microclimate Stratification

Vertical Microclimate Stratification is a microclimatic phenomenon characterized by the layering of distinct climatic conditions at different heights within a localized environment, distinguished by vertical gradients in temperature, humidity, wind speed, and solar radiation due to differential surface-atmosphere interactions.

15

Publications

627

Citations

60

Authors

33

Institutions

Publications per year

2017–2026

5

Authors

60

  1. NL
    Naftali Lazarovitch

    Ben-Gurion University of the Negev, Israel

    1 publications · 24 citations

    1

    h-index

  2. HZ
    Hucai Zhang

    Yunnan University, China

    1 publications · 33 citations

    1

    h-index

  3. BY
    Bailang Yu

    East China Normal University, China

    1 publications · 32 citations

    1

    h-index

  4. DT
    Daniel Tregidgo

    Lancaster University, United Kingdom

    1 publications · 28 citations

    1

    h-index

  5. QL
    Qie Lan

    University of Malaya, Malaysia

    1 publications · 28 citations

    1

    h-index

1–5 of 60

Venues

  1. Water Resources Research

    1 publications · 32 citations

    1

    h-index

  2. Marine and Freshwater Research

    1 publications · 25 citations

    1

    h-index

  3. Scientia Horticulturae

    1 publications · 24 citations

    1

    h-index

  4. Water

    1 publications · 33 citations

    1

    h-index

  5. Pacific Science

    1 publications · 32 citations

    1

    h-index

1–5