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V. Knysh, S. Demyshev, N. Inyushina, G. Korotaev (2008)
Assimilation of climatic hydrological data in a Black-Sea model based on the algorithm of adaptive statistics of prognostic errorsPhysical Oceanography, 18
P. Smolarkiewicz (1983)
A Simple Positive Definite Advection Scheme with Small Implicit DiffusionMonthly Weather Review, 111
S. G. Demyshev, V. V. Knysh, N. V. Inyushina (2005)
Seasonal variability and transformation of the climatic horizontal currents in the Black Sea with depth according to the results of assimilation of new climatic data on temperature and salinity in the modelMorsk. Gidrofiz. Zh., 6
PK Smolarkiewicz (1983)
A simple positive-definite advection transport scheme with small implicit diffusionMon. Weather Rev., 111
G. Mellor, Tetsuji Yamada (1982)
Development of a turbulence closure model for geophysical fluid problemsReviews of Geophysics, 20
P. Smolarkiewicz (1984)
A Fully Multidimensional Positive Definite Advection Transport Algorithm with Small Implicit DiffusionJournal of Computational Physics, 54
V. V. Knysh, S. G. Demyshev, G. K. Korotaev (2002)
A procedure of reconstruction of the climatic seasonal circulation in the Black Sea based on the assimilation of hydrological data in the modelMorsk. Gidrofiz. Zh., 2
S. Demyshev, V. Knysh, N. Inyushina (2005)
Seasonal Variations and Transformations of Climatic Currents with Depth on the Basis of Assimilation of New Climatic Data on Temperature and Salinity in a Model of the Black SeaPhysical Oceanography, 15
V. Knysh, S. Demyshev, G. Korotaev (2002)
A Procedure of Reconstruction of the Climatic Seasonal Circulation in the Black Sea Based on the Assimilation of Hydrological Data in the ModelPhysical Oceanography, 12
SG Demyshev, VV Knysh, GK Korotaev (2006)
Results of numerical analyses of the adapted fields in the Black Sea based on the assimilation of the data on climatic temperature and salinity in the modelIzv. Ros. Akad. Nauk, Fiz. Atmosf. Okean., 42
VV Knysh, VA Moiseenko, VV Chernov (1988)
Some results of the four-dimensional analysis of hydrophysical fields in the Tropical AtlanticIzv. Akad. Nauk SSSR, Fiz. Atmosf. Okean., 24
LS Gandin, RA Kagan (1976)
Statistical Methods for the Interpretation of Meteorological Data
We realize the algorithm of adaptive statistics of forecasting errors for the assimilation of the climatic fields of temperature and salinity in the σ-coordinate model of the dynamics of the Black Sea. The principal relations of this algorithm and its simplified version based on the Kalman filter are presented. The distinctive features of realization of the algorithm specified by the model are discussed. We also present the results of comparison of the hydrophysical fields of the Black Sea reconstructed according to the algorithm of adaptive statistics and a simplified scheme of assimilation of the climatic data. It is shown that the dependence of sources in the transport equations (heat and salt diffusion) on the four-dimensional variances of forecasting errors and threedimensional measurement errors enables one to reconstruct the mutually adapted climatic parameters of the sea more exactly.
Physical Oceanography – Springer Journals
Published: Jun 22, 2010
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