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In the shallow waters, it is possible that the wind-generated mixed layer reaches the bottom or the mixed layer generated by bottom friction and the two become melded together.
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Oligotrophy lasted until the mixed layer reached the nutricline in autumn.
As this water entered the Chesapeake Bay through the northern part of its mouth, the concentration of R-iodate decreased while that of R-iodide increased progressively until the former became undetectable in the surface mixed layer while the latter reached a maximum of 0.42 μM in the deep water in the upper Bay.
The planetary boundary layer is well mixed, and the surface measurements are representative of the whole convective mixed layer, when the daily maximum ozone concentration is reached.
The initial depth of the oceanic mixed layer was determined from oceanic reanalysis data by defining the mixed layer as reaching a depth at which the density was no more than 0.25 kg m−3 higher than the density at the surface and having a maximum depth of 200 m.
During the Spring Inter-monsoon, the mixed layer was much less pronounced.
The uppermost layer was the mixed layer, where the density was vertically uniform.
The isothermal layer was deeper than the mixed layer in both typhoons.
Xin, et al [5], investigate that there are five layers: oxide layer, mixed layer, TTS layer, plastic deformation layer and base materials in the fretting wear subsurface.
The thickness of inner oxide layer reaches 20% of that of the outer oxide layer.
Sea-surface irradiance is divided by mixed layer depth to provide an estimate of the mean near-surface irradiance experienced by phytoplankton entrained in the mixed layer.
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