| 41. | If its passage mixed layers of cold surface and underlying warm water, this would raise the apparent surface temperature slightly.
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| 42. | In saline lakes and seas ( such as the Caspian Sea ), mixed layer formation generally behaves similarly to the ocean.
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| 43. | Layer 2 is below the first layer but above the 26.81 isopycnal and is no longer part of the mixed layer.
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| 44. | Below the mixed layer, a stable density gradient ( or pycnocline ) separates the upper and lower water which hinders vertical transport.
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| 45. | As long as there are adequate nutrients available, net primary production occurs whenever the mixed layer is shallower than the critical depth.
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| 46. | This hypothesis points to the difference between a mixed layer and an actively turbulent layer that could play a more important role.
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| 47. | During the early morning the mixed layer is shallow and its depth increases slowly because of the strong nocturnal stable inversion capping.
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| 48. | These are the reasons that the depth of the ocean mixed layer is more important in hurricane deepening than sea surface temperature.
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| 49. | Long term sea surface temperature variation may be induced by random atmospheric forcings that are integrated and reddened into the ocean mixed layer.
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| 50. | Another study which instead focused on the Central Equatorial Pacific Ocean found a tendency for increased depths of the mixed layer during nighttime.
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