Horizontal inhomogeneities of the density field have been identified at ten depth levels for four seasons. Spatio-temporal variabilities of the maximal gradient zones have been established in the meridional and zonal directions and in the direction of the largest growth of the density gradient. The characteristics of the density field inhomogeneities have been determined (climatic horizontal area), which are used to model dynamic processes in the ocean.
Physical Oceanography – Springer Journals
Published: Oct 23, 2006
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