Surface, intermediate, and deep-water processes and their
interaction in time and space drive the major ocean circulation of
the Mediterranean Sea. All major forcing mechanisms, such as
surface wind forcing, buoyancy fluxes, lateral mass exchange, and
deep convection determining the global oceanic circulation are
present in this body of water. Deep and intermediate water masses
are formed in different areas of the ocean layers and they drive
the Mediterranean thermohaline cell, which further shows important
analogies with the global ocean conveyor belt. "The Mediterranean
Sea: Temporal Variability and Spatial Patterns "is a comprehensive
volume that investigates the temporal and spatial variability
patterns in the ocean basin.
Volume highlights include: Discussions of state-of-the-art
physical and biogeochemical properties of the Mediterranean
SeaMultiple physical ocean circulation processes, both in time and
spatial scales (basin, sub-basin, and mesoscale)How different
regional phenomena in the sea influence the biogeochemistry of the
basin and the ocean dynamicsSpatio-temporal variability of the
surface circulation in the western MediterraneanDeep-water
variability and inter-basin interactions in the eastern
Mediterranean SeaUnderstanding the link between global ocean
circulation patterns and the global climate
"The Mediterranean Sea "will be a valuable resource for
geoscientists, oceanographers, and meteorologists.
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