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Three-dimensional flow in the upper ocean.

R A Weller, J P Dean, J F Price

    Science (New York, N.Y.)
    |March 29, 1985
    PubMed
    Summary
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    Direct oceanographic measurements reveal narrow downwelling flow regions within the surface mixed layer. These flows, alongside horizontal jets, may transport heat and phytoplankton, offering new insights into ocean dynamics.

    Area of Science:

    • Oceanography
    • Fluid Dynamics

    Background:

    • The ocean's surface mixed layer plays a critical role in climate and marine ecosystems.
    • Understanding three-dimensional flow patterns within this layer is essential for accurate modeling.

    Purpose of the Study:

    • To provide direct observations of three-dimensional flow within the ocean's surface mixed layer.
    • To investigate the characteristics and potential impacts of observed flow structures.

    Main Methods:

    • Utilized the Research Platform FLIP for direct measurements.
    • Collected data on flow velocities and patterns within the mixed layer.

    Main Results:

    • Identified narrow regions of downwelling flow coinciding with convergent surface flow bands.

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  • Observed downwelling flow up to 0.2 m/s at mid-depth, accompanied by a similar magnitude downwind horizontal jet.
  • Found preliminary evidence suggesting transport of heat and phytoplankton by these motions.
  • Conclusions:

    • Direct observations reveal complex three-dimensional flow structures in the ocean mixed layer.
    • These flows, including downwelling and horizontal jets, likely play a significant role in vertical and horizontal transport processes.
    • Further research is warranted to fully understand the implications for heat and nutrient distribution.