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Patterns of phytoplankton and primary production variability in the Mediterranean Sea based on remote sensing data

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Academic year: 2020

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Figure

Fig I-1. Major constituents and processes composing the ocean’s biological carbon pump or transfer of  carbon from the atmosphere (inorganic CO 2 ) to the deep ocean (organic C)
Fig. II-3. Annual NPP distribution in the global ocean from the SeaWiFS sensor (1997-2002)
Fig. I-4 Mediterranean Sea bathymetry. Gray contour line delimits coastal waters (200 m isobath)
Fig. I- 5. Upper: Main circulation features of the Mediterranean Sea (surface circulation is in black,  intermediate circulation is in grey, symbol ϒ indicates site of dense water formation)
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