Effects of Oceanic Mesoscale and Submesoscale Frontal Processes on the Vertical Transport of Phytoplankton

Oceanic fronts are dynamically active regions of the global ocean that support upwelling and downwelling with significant implications for phytoplankton production and export. However (on time scales ≳ the inertial time scale), the vertical velocity is 103–104 times weaker than the horizontal veloc...

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Veröffentlicht in:	Journal of geophysical research. Oceans 2019-08, Vol.124 (8), p.5999-6014
Hauptverfasser:	Ruiz, Simón, Claret, Mariona, Pascual, Ananda, Olita, Antonio, Troupin, Charles, Capet, Arthur, Tovar‐Sánchez, Antonio, Allen, John, Poulain, Pierre‐Marie, Tintoré, Joaquín, Mahadevan, Amala
Format:	Artikel
Sprache:	eng
Schlagworte:	Chlorophyll Chlorophyll content Chlorophylls Downwelling Fluxes Fronts Geophysics mesoscale Mixed layer Ocean circulation ocean front Ocean models Oceanic fronts Oceans Phytoplankton Phytoplankton production Plankton Pycnocline submesoscale Surface boundary layer Surface layers Surface mixed layer transport Upwelling Velocity Vertical advection Vertical flux Vertical motion Vertical velocities
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