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- W2016645016 abstract "The diurnal variability of the near-surface ocean thermal structure is briefly considered along with the corresponding variability of various near-surface processes. Problem of the satellite remote sensing of sea surface temperature (SST) in the presence of the diurnal heated layer is discussed. Dependence of the diurnal thermocline temperature difference (ΔTD) and lower boundary depth (HD) on wind speed (u10) is demonstrated using field measurements in the range of u10 = 0–13 m/s. Here ΔTD decreases sharply from maximum values to about 1°C when u10 increases from 0 to 2 m/s, while H is practically unchanged. As the wind continues to increase ΔTD is approximately proportional to 1/u10 and HD is approximately proportional to u10. A simple method is proposed to estimate H from satellite or ship-borne measurements of the daily variation of SST and the heated layer enthalpy (computed from the daily total of incoming solar flux using a relation derived from field measurements)." @default.
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- W2016645016 title "Estimating parameters of the oceanic diurnal thermocline using satellite and ship-borne measurements" @default.
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- W2016645016 doi "https://doi.org/10.1016/0924-7963(94)90008-6" @default.
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