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Mercury concentration in waters shallower than 100 meters has tripled compared with preindustrial times, they found, whereas mercury levels in intermediate waters have increased by 1.5 times.
A comparison of the shelf-open sea exchanges, with particular focus on the cold intermediate waters, shows that both models lead to a replenishment of the CIL in the basin interior by cold waters formed on the shelf.
The surface waters come from the Atlantic and turn into intermediate waters in the Eastern Mediterranean.
The temporal response of total Hg concentrations in the ocean surface mixed layer (< 100 m) will be relatively rapid (several years) compared with those of intermediate waters (decades to centuries) and deep waters (many centuries) (Sunderland and Mason 2007; Sunderland et al. 2009).
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The middle water's origin is in the intermediate water layers of the Kuroshio off the coast of Kyushu that enter the Sea of Japan via the Tsushima Current during the winter and spring.
At intermediate water saturations, a mixed flow pattern (thin channels and slugs) was observed.
The intermediate water was probably warmer than it is today, especially from 3.0 to 2.9 Ma.
However, we also consider the implementation of intermediate water-jets to improve the motion.
Results from coupled analysis are compared with experimental data in intermediate water depth.
The equation yields celerities in reasonable agreement with those for cnoidal waves in intermediate water depths.
It is well established that in the hydrogel polymeric networks the water is present in three different states: free water, intermediate water and bound water [25].
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