Coastal Inflow

Coastal Inflow is a hydrodynamic process denoting the directed movement of offshore water masses into coastal regions, distinguished by its role in advecting momentum, heat, nutrients, and sediments across the continental shelf break under the influence of meteorological, tidal, and density-driven forcing mechanisms.

40

Publications

2.2K

Citations

155

Authors

71

Institutions

Publications per year

2017–2026

6

Authors

155

  1. HP
    Hans Pettersson

    Swedish University of Agricultural Sciences, Sweden

    2 publications · 25 citations

    2

    h-index

  2. RM
    Robert M. Brown

    Virginia Tech, United States

    2 publications · 146 citations

    2

    h-index

  3. SS
    Sunder Sethuraman

    Iowa State University, United States

    2 publications · 146 citations

    2

    h-index

  4. GS
    Gilbert S. Raynor

    Brookhaven National Laboratory, United States

    2 publications · 146 citations

    2

    h-index

  5. SL
    Seth L. Danielson

    University of Alaska Fairbanks, United States

    2 publications · 201 citations

    2

    h-index

1–5 of 155

Venues

  1. Marine Pollution Bulletin

    3 publications · 141 citations

    3

    h-index

  2. Journal of Coastal Research

    JCR · 3 publications · 44 citations

    3

    h-index

  3. Geografiska Annaler

    2 publications · 25 citations

    2

    h-index

  4. Journal of Marine Research

    2 publications · 123 citations

    2

    h-index

  5. Boundary-Layer Meteorology

    2 publications · 146 citations

    2

    h-index

1–5