Enhanced Vertical Mixing in Coastal Upwelling Systems Driven by Diurnal-Inertial Resonance: Numerical Experiments
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS(2020)
摘要
The land-sea breeze is resonant with the inertial response of the ocean at the critical latitude of 30 degrees N/S. 1-D vertical numerical experiments were undertaken to study the key drivers of enhanced diapycnal mixing in coastal upwelling systems driven by diurnal-inertial resonance near the critical latitude. The effect of the land boundary was implicitly included in the model through the "Craig approximation" for first-order cross-shore surface elevation gradient response. The model indicates that for shallow water depths (更多
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关键词
inertial oscillations</AUTHOR_KEYWORD>,land-sea breeze</AUTHOR_KEYWORD>,diurnal-inertial resonance</AUTHOR_KEYWORD>,coastal upwelling</AUTHOR_KEYWORD>,diapycnal mixing</AUTHOR_KEYWORD>,phytoplankton blooms</AUTHOR_KEYWORD>
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