Front-induced Stratification Changes

Front-Induced Stratification Changes is a geophysical process characterized by the alteration of vertical density structure in the oceanic water column due to the convergence and divergence dynamics associated with oceanic fronts, distinguishing it from other forms of stratification variability by its direct mechanistic linkage to frontal circulation and associated lateral gradients in temperature and salinity.

28

Publications

1.4K

Citations

91

Authors

56

Institutions

Publications per year

2017–2026

3

Authors

91

  1. HP
    Hsien‐Ping Pao

    Catholic University of America, United States

    2 publications · 62 citations

    2

    h-index

  2. LN
    Leif N. Thomas

    Stanford University, United States

    2 publications · 193 citations

    2

    h-index

  3. AR
    Alberto Ribotti

    Fondazione Centro Marino Internazionale, Italy

    2 publications · 63 citations

    2

    h-index

  4. JT
    Joaquı́n Tintoré

    Mediterranean Institute for Advanced Studies, Spain

    2 publications · 63 citations

    2

    h-index

  5. CP
    Cheol Park

    Korea University, South Korea

    2 publications · 62 citations

    2

    h-index

1–5 of 91

Venues

  1. Journal of Physical Oceanography

    5 publications · 418 citations

    5

    h-index

  2. Journal of Marine Systems

    3 publications · 122 citations

    3

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 3 publications · 72 citations

    3

    h-index

  4. 2

    h-index

  5. Estuarine and Coastal Marine Science

    1 publications · 53 citations

    1

    h-index

1–5