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Taking into account these estimations, it is possible to get already the third approximation.
The third approximation, also presented in Figure 3a, assumes finer-grained discretization with 24 time periods (fA 24) in the case of a working day only.
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Thus in the first approximation even objects as large as the Earth and the Sun are treated as pointlike e.g., in calculating planetary orbital motion.
The second approximation is.
(b) The surface of the second approximation.
The second approximation is related to the time domain.
determine the initial data of the zeroth approximation.
The periodic solution in the first approximation is obtained.
The FEA was also used to examine the assumptions of the first approximation analytic solution.
The first approximation is based on interchanging the minimization and expectation operators.
In this paper, we give some of the first approximation algorithms for it.
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