scholarly journals Structural Identification of Static Systems with Distributed Lags

2013 ◽  
Vol 2 (6) ◽  
pp. 136-142 ◽  
Author(s):  
Nikolay Karabutov
Keyword(s):  
Structural Identification ◽  
Distributed Lags ◽  
Static Systems

The Structural Identification of Interval Models of Static Systems

2008 ◽  
Vol 40 (4) ◽  
pp. 49-61 ◽  
Author(s):  
Nikolay P. Dyvak ◽  
Vladimir I. Manzhula
Keyword(s):  
Structural Identification ◽  
Static Systems

scholarly journals THE ALGORITHM OF SUPPLEMENTARY ARGUMENTS INCLUSION FOR INTERVAL MODELS STRUCTURAL IDENTIFICATION OF THE STATIC SYSTEMS

2014 ◽  
pp. 99-112
Author(s):  
Mykola Dyvak ◽  
Volodymyr Manzhula
Keyword(s):  
Unique Solution ◽  
Iterative Procedure ◽  
Structural Identification ◽  
Static Models ◽  
Static Systems ◽  
Interval Systems ◽  
Magnitude Interval

The problem of structural identification of static models of interval systems. Showing getting a unique solution for the problem of structural identification for different initial given structure models based on the complexity of the proposed algorithm sequential structures. An adaptive iterative procedure, which reduces the dependence of the result of structural identification of the magnitude interval error data.

Structural identification of static systems with saturation

2011 ◽  
Vol 54 (2) ◽  
pp. 135-142
Author(s):  
N. N. Karabutov
Keyword(s):  
Structural Identification ◽  
Static Systems

Note on Selection of Coordinate Systems for Geodynamics

1975 ◽  
Vol 26 ◽  
pp. 395-407
Author(s):  
S. Henriksen
Keyword(s):  
Sea Level ◽  
The Other ◽  
Coordinate Systems ◽  
Mean Sea Level ◽  
The Earth ◽  
The One ◽  
Static Systems ◽  
Selection Of

The first question to be answered, in seeking coordinate systems for geodynamics, is: what is geodynamics? The answer is, of course, that geodynamics is that part of geophysics which is concerned with movements of the Earth, as opposed to geostatics which is the physics of the stationary Earth. But as far as we know, there is no stationary Earth – epur sic monere. So geodynamics is actually coextensive with geophysics, and coordinate systems suitable for the one should be suitable for the other. At the present time, there are not many coordinate systems, if any, that can be identified with a static Earth. Certainly the only coordinate of aeronomic (atmospheric) interest is the height, and this is usually either as geodynamic height or as pressure. In oceanology, the most important coordinate is depth, and this, like heights in the atmosphere, is expressed as metric depth from mean sea level, as geodynamic depth, or as pressure. Only for the earth do we find “static” systems in use, ana even here there is real question as to whether the systems are dynamic or static. So it would seem that our answer to the question, of what kind, of coordinate systems are we seeking, must be that we are looking for the same systems as are used in geophysics, and these systems are dynamic in nature already – that is, their definition involvestime.

STRUCTURAL IDENTIFICATION OF A THERMAL PROCESS USING THE VOLTERRA MODEL

2014 ◽  
Vol 45 (5) ◽  
pp. 471-484
Author(s):  
Safa Chouchane ◽  
Kais Bouzrara ◽  
Hassani Messaoud
Keyword(s):  
Thermal Process ◽  
Structural Identification ◽  
Volterra Model
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