Global Spatial and Temporal Variability of the Oceanic Cool Skin Effect
Authors:
Open Access
- 27 March 2026
- journal article
- research article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Oceans
- Vol. 131 (4)
Abstract
The oceanic cool skin effect is characterized by a temperature depression between the ocean's submillimeter thermal skin layer (SST skin ) and the underlying water (SST depth ). This study evaluates the ability of the widely used Fairall et al. (1996), https://doi.org/10.1029/95jc03190 model (F96) to simulate the cool skin effect using surface forcing data from the Modern‐Era Retrospective analysis for Research and Applications, Version 2 (MERRA‐2), validated against high‐accuracy infrared radiometric measurements from the Marine‐Atmospheric Emitted Radiance Interferometer (M‐AERI) and the Infrared Sea Surface Temperature Autonomous Radiometer (ISAR) collected during research cruises spanning diverse oceanic regions. Results show that F96 model simulations driven by MERRA‐2 inputs generally match the observed skin effects, with mean biases of −0.03 to −0.04 K and standard deviations ∼0.1 K, attributed primarily to uncertainties in humidity, longwave radiative flux, and wind speed. A 24‐year global analysis (2000–2023) revealed a mean cool skin effect of approximately −0.2 K, with pronounced spatial and seasonal variability. Strongest cooling (−0.3 K or more) occurs in regions such as western boundary currents during colder months, while the Southern Ocean shows much weaker skin effects (−0.1 K) due to persistent high wind speeds and reduced net heat loss. These results suggest that the commonly applied constant correction of −0.17 K in satellite SST skin retrievals does not accurately represent the true magnitude and variability of the cool skin effect. A more accurate correction scheme incorporating latitude and seasonal dependence is recommended to improve the accuracy of satellite‐derived SST skin fields, and better support climate model applications.Keywords
Funding Information
- National Aeronautics and Space Administration (80NSSC24K1825)
- National Aeronautics and Space Administration (80NSSC22K0680)
- National Aeronautics and Space Administration (80NSSC18K0837)
This publication has 52 references indexed in Scilit:
- The ERA5 global reanalysisQuarterly Journal of the Royal Meteorological Society, 2020
- Global Sea Surface Temperature2019
- Shipboard automated meteorological and oceanographic system data archive: 2005–2017Geoscience Data Journal, 2018
- The Response of the Ocean Thermal Skin Layer to Variations in Incident Infrared RadiationJournal of Geophysical Research: Oceans, 2018
- Warm layer and cool skin corrections for bulk water temperature measurements for air‐sea interaction studiesJournal of Geophysical Research: Oceans, 2017
- Extension of the prognostic model of sea surface temperature to rain‐induced cool and fresh lensesJournal of Geophysical Research: Oceans, 2017
- Assimilation for skin SST in the NASA GEOS atmospheric data assimilation systemQuarterly Journal of the Royal Meteorological Society, 2016
- New correlations for seawater and pure water thermal conductivity at different temperatures and salinitiesDesalination, 2013
- Measurements of the oceanic thermal skin effectDeep Sea Research Part II: Topical Studies in Oceanography, 2011
- The dependence of the measured cool skin of the ocean on wind stress and total heat fluxBoundary-Layer Meteorology, 1976