Fig_8.tif (1.29 MB)

Distributions of depth integrated (over 100 m) phytoplankton biomass at day 75 for (a) the abiabatic (unforced) simulation, and diabatic case with (b) down-front wind forcing, (c) buoyancy-induced cooling.

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posted on 11.06.2015, 03:47 authored by Temel Oguz, Diego Macias, Joaquin Tintore

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Ageostrophic Frontal Processes Controlling Phytoplankton Production in the Catalano-Balearic Sea (Western Mediterranean)

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ageostrophic Western Mediterranean Mesoscale cyclonic eddies High upwelling velocities phytoplankton biomass distribution mechanism Ageostrophic Frontal Processes Controlling Phytoplankton Production onshore side Biophysical model simulations nutrient

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Distributions of depth integrated (over 100 m) phytoplankton biomass at day 75 for (a) the abiabatic (unforced) simulation, and diabatic case with (b) down-front wind forcing, (c) buoyancy-induced cooling.

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