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A. S. Blatov, N. P. Bulgakov, V. A. Ivanov (1984)
Variability of Hydrophysical Fields of the Black Sea
E. Stanev, D. Trukhchev, V. Rusenov (1988)
Water Circulation and Numerical Simulation of Currents of the Black Sea
V. A. Ivanov, A. I. Kubryakov, N. B. Shapiro (1997)
The thermohaline structure and dynamics of waters in the Gulf of IzmirMorsk. Gidrofiz. Zh., 4
S. Hellerman, M. Rosenstein (1983)
Normal Monthly Wind Stress Over the World Ocean with Error EstimatesJournal of Physical Oceanography, 13
J. Sarmiento, K. Bryan (1982)
An ocean transport model for the North AtlanticJournal of Geophysical Research, 87
Yu. N. Ryabtsev, N. B. Shapiro (1997)
Modelling of the seasonal variability of the Black SeaMorsk. Gidrofiz. Zh., 1
N. H. Rachev, V. M. Roussenov, E. V. Stanev (1991)
The Black Sea climatological wind stressBulg. J. Meteorol. Hydrol., 2
E. N. Mikhailova, N. B. Shapiro (1992)
A quasiisopycnic layered model of large-scale oceanic circulationMorsk. Gidrofiz. Zh., 4
D. Trukhchev, A. S. Sarkisyan (1995)
Hydrodynamic diagnosis of climatic fields of temperature, salinity, and currents in the Black SeaIzv. Ros. Akad. Nauk, Fiz. Atmos. Okeana, 31
V. I. Klimok, K. K. Makeshov, M. V. Pertseva (1989)
On the numerical simulation of currents in the northwest shelf zone of the Black SeaMorsk. Gidrofiz. Zh., 3
Yu. N. Ryabtsev, N. B. Shapiro (1995)
Modelling of formation and evolution of a cold intermediate layer in the Black SeaMorsk. Gidrofiz. Zh., 1
V. A. Ivanov, V. K. Kosnyrev, E. N. Mikhailova (1996)
Diagnosis of the Medium State of Near-Coastal and Shelf Zones of the Black Sea
N. B. Shapiro (1998)
Formation of circulation in a quasiisopycnic model of the Black Sea with regard for the stochasticity of the wind stressMorsk. Gidrofiz. Zh., 6
We propose a method for the adaptive numerical analysis of current velocities in a basin including a shelf zone and having a lengthy open boundary with the sea, at which the current velocity is not given. This method is based on a multilayer quasiisopycnic model. We use an approach according to which one introduces additional terms of the source type into the equations of heat and salt transfer and the equation of evolution of the thicknesses of layers. We describe the results of calculations of the current velocities in the northwest part of the Black Sea in June on the basis of climatic data. We also analyse specific features of thermohaline and dynamic structure of waters.
Physical Oceanography – Springer Journals
Published: Sep 18, 2006
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