A. Ginzburg, A. G. Kostyanoy, D. A. Solov'yev, S. V. Stanichnyy
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引用次数: 2
Abstract
The results of an analysis of a series of infrared images recorded by the NOAA-12 and NOAA-14 satellites (6 September-14 November 1997), making it possible to trace the formation and evolution of coastal anticyclonic eddies (CACE) between Anapa and Gagra in the northeastern Black Sea are presented. The velocity of their movement along individual segments was determined and the movement of one of the coastal eddies from the shore west of Novorossiysk and its transformation into an open-sea eddy were observed. The possible relationship between the formation and trajectory of coastal anticyclonic eddies and bottom topographic features and atmospheric influences is discussed.
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