Wintertime Convection

Wintertime Convection is a meteorological phenomenon characterized by the seasonal occurrence of vertical heat and moisture transport in polar regions during the winter months, driven by strong surface cooling and atmospheric instability distinct from convection in other seasons.

106

Publications

5.8K

Citations

368

Authors

185

Institutions

Publications per year

2017–2026

25

Authors

368

  1. RS
    Robert S. Pickart

    Woods Hole Oceanographic Institution, United States

    4 publications · 646 citations

    4

    h-index

  2. JM
    Jonathan M. Lilly

    Northwest Research Associates, United States

    3 publications · 314 citations

    3

    h-index

  3. PB
    Peter B. Rhines

    University of Washington, United States

    3 publications · 397 citations

    3

    h-index

  4. JR
    J. R. Lazier

    Bedford Institute of Oceanography, Canada

    2 publications · 434 citations

    2

    h-index

  5. AM
    Andrew Meijers

    British Antarctic Survey, United Kingdom

    2 publications · 95 citations

    2

    h-index

1–5 of 368

Venues

  1. Journal of Physical Oceanography

    13 publications · 1.2K citations

    13

    h-index

  2. Geophysical Research Letters

    8 publications · 461 citations

    8

    h-index

  3. Climate Dynamics

    7 publications · 280 citations

    8

    h-index

  4. Journal of Climate

    7 publications · 344 citations

    7

    h-index

  5. Journal of Geophysical Research Oceans

    6 publications · 196 citations

    6

    h-index

1–5