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- W4210629816 abstract "Measurements of the turbulent kinetic energy dissipation rate (ε) were conducted by a free-fall microstructure profiler in the western Pacific North Equatorial Current (WPNEC) during a continuous period of 25 h, from the sea surface to about 160 m depth. In the mixed layer (ML), ε values were typically on the order of 10-8∼10-7 W kg-1, and an obvious diurnal cycle existed in the upper 40 m of the surface mixing layer. Below the ML, ε was reduced to 10-9∼10-8 W kg-1 with some patches of high ε reaching 10-7.5 W kg-1. The barrier layer was identified in the nighttime with a maximum thickness of 20 m, and it was eroded by the advection of freshwater within the lower part of the isothermal layers associated with an anticyclonic eddy in the afternoon. A simple scaling relevant to shear (S2) instability and stratification (N2) that can predict turbulent dissipation rates in the transition layer, between the well-mixed layer and the thermocline below, was obtained through the scaling ε∼S-0.40N0.20. Besides turbulence, double-diffusive processes also contributed to the vertical mixing levels in the upper WPNEC." @default.
- W4210629816 created "2022-02-08" @default.
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- W4210629816 date "2022-02-03" @default.
- W4210629816 modified "2023-09-26" @default.
- W4210629816 title "Direct Measurements of Turbulence in the Upper Western Pacific North Equatorial Current over a 25-h Period" @default.
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- W4210629816 doi "https://doi.org/10.3390/s22031167" @default.
- W4210629816 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/35161911" @default.
- W4210629816 hasPublicationYear "2022" @default.
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