Open AccessThe mixed layer salinity budget and sea ice in the Southern Ocean
Author(s) -
Ren Li,
Speer Kevin,
Chassignet Eric P.
Publication year - 2011
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2010jc006634
Subject(s) - geostrophic wind , sea ice , advection , ekman transport , ekman layer , mixed layer , environmental science , climatology , sea ice thickness , salinity , geology , oceanography , entrainment (biomusicology) , argo , geostrophic current , antarctic sea ice , wind stress , arctic ice pack , boundary layer , upwelling , philosophy , physics , rhythm , thermodynamics , aesthetics
The seasonal variation of the mixed layer salinity budget in the Southern Ocean is evaluated over the latitude range 45°S–62°S using Argo profiling float data, freshwater fluxes (evaporation minus precipitation (E‐P)), geostrophic velocity, wind stress, and sea ice concentration observations. The seasonal cycle of the mixed layer salinity is driven by seasonality in E‐P, Ekman advection, entrainment, and sea ice. Over large areas, the geostrophic advection and diffusion show smaller contributions to the seasonal variation relative to other terms. The air‐sea freshwater flux and Ekman advection in this area generally result in net decreases in salinity, while the entrainment term yields increases. Residual imbalance is consistent with a sea ice effect, whose contribution is evaluated. Sea ice is found to make a significant contribution, growing in importance toward the ice edge.