Sea-breeze Depth

Sea-Breeze Depth is a meteorological construct that denotes the vertical extent of the sea-breeze circulation, distinguished by the maximum altitude at which marine-influenced airflow deviates from the prevailing synoptic wind field due to density-driven coastal convergence.

17

Publications

697

Citations

53

Authors

25

Institutions

Publications per year

2017–2026

1

Authors

53

  1. DG
    D. G. Steyn

    University of British Columbia, Canada

    2 publications · 95 citations

    2

    h-index

  2. HK
    Hiroaki Kondo

    National Institute of Advanced Industrial Science and Technology, Japan

    2 publications · 113 citations

    2

    h-index

  3. BC
    Bernard Campistron

    Laboratoire d'Aérologie, France

    1 publications · 80 citations

    1

    h-index

  4. RM
    Robert M. Banta

    Cooperative Institute for Research in Environmental Sciences, United States

    1 publications · 58 citations

    1

    h-index

  5. SY
    Susumu Yamamoto

    The University of Tokyo, Japan

    1 publications · 10 citations

    1

    h-index

1–5 of 53

Venues

  1. Boundary-Layer Meteorology

    5 publications · 273 citations

    5

    h-index

  2. 2

    h-index

  3. South African Geographical Journal

    2 publications · 35 citations

    2

    h-index

  4. Atmospheric Research

    2 publications · 111 citations

    2

    h-index

  5. Monthly Weather Review

    2 publications · 123 citations

    2

    h-index

1–5