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In the western Arabian Sea, the surface mixed layer extends to ~30 m with a seasonally variable in depth thermocline extending below.
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The winter cooling forms an upper mixed layer extending to depths of about 160 to 330 feet (50 to 100 metres), with temperatures at the lower boundary of about 44 to 46 °F (6.5 to 8 °C).
This magma layer extends at least 150 square miles and is located about five miles underground.
Basement layer extends down to 12 km in thermal models.
The layer extends vertically from about 13 to 18 km.
The layer extends from about 12 to 40 km.
Within the hippocampus region, measurements were performed over the layer extending from subregions CA1 CA3.
During the Spring Inter-monsoon, the mixed layer was much less pronounced.
The isothermal layer was deeper than the mixed layer in both typhoons.
The uppermost layer was the mixed layer, where the density was vertically uniform.
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.
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