Fog Condensation Processes

Fog Condensation Processes is a meteorological phenomenon representing the physical mechanism by which atmospheric water vapor undergoes phase transition into liquid droplets near the Earth's surface, distinguished from other condensation processes by its occurrence within a saturated planetary boundary layer under conditions of high relative humidity and minimal vertical mixing.

50

Publications

2.4K

Citations

180

Authors

78

Institutions

Publications per year

2017–2026

9

Authors

180

  1. MH
    Martial Haeffelin

    Institut Pierre-Simon Laplace, France

    5 publications · 245 citations

    5

    h-index

  2. JD
    Jean‐Charles Dupont

    Institut Pierre-Simon Laplace, France

    5 publications · 245 citations

    5

    h-index

  3. SF
    S. Fuzzi

    Institute of Atmospheric Sciences and Climate, Italy

    4 publications · 335 citations

    4

    h-index

  4. MC
    M. C. Facchini

    Institute of Atmospheric Sciences and Climate, Italy

    3 publications · 275 citations

    3

    h-index

  5. GO
    G. Orsi

    Istituto Giordano, Italy

    3 publications · 275 citations

    3

    h-index

1–5 of 180

Venues

  1. 3

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  2. Tellus B

    2 publications · 201 citations

    2

    h-index

  3. Atmospheric chemistry and physics

    2 publications · 105 citations

    2

    h-index

  4. Journal of applied meteorology

    2 publications · 39 citations

    2

    h-index

  5. Pure and Applied Geophysics

    PAGEOPH · 2 publications · 82 citations

    2

    h-index

1–5