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• W2985763054 abstract "Abstract The nighttime ocean cool skin signal Δ T [defined as skin sea surface temperature (SST skin ) minus depth SST (SST depth )] is investigated using 103 days of matchups between shipborne Infrared SST Autonomous Radiometer (ISAR) SST skin and water intake SST depth at ~7.1–9.9-m depths, in oceans around Australia. Before data analysis, strict quality control of ISAR SST skin data is conducted and possible diurnal warming contamination is carefully minimized. The statistical distribution of Δ T , and its dependencies on wind speed, heat flux, etc., are consistent with previous findings. The overall average Δ T value is −0.23 K. It is observed that the magnitude of the cool skin signal increases after midnight and a coolest skin offset (with an average value of −0.36 K) is found at around dawn. The dependency of Δ T on SST conditions is observed. Direct warm skin events are discovered when the net heat flux direction is from the atmosphere to the ocean, which is more likely to occur at high latitudes when the air is very humid and warmer than the SST. In addition, several cool skin models are validated: one widely used physical model performs best and can capture most skin-effect trends and details; the empirical models only reflect the basic features of the observed Δ T values. If the user cannot apply the physical model (due to, e.g., the algorithm complexity or missing inputs), then the empirical parameterization in the form proposed in a 2002 study can be used. However, we recommend using a new set of parameters, calculated in this study, based on much more representative dataset, and with more rigorous quality control." @default.
• W2985763054 created "2019-11-22" @default.
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• W2985763054 date "2020-01-01" @default.
• W2985763054 modified "2023-10-10" @default.
• W2985763054 title "Nighttime Cool Skin Effect Observed from Infrared SST Autonomous Radiometer (ISAR) and Depth Temperatures" @default.
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• W2985763054 doi "https://doi.org/10.1175/jtech-d-19-0161.1" @default.
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