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Secondary, Earth-induced fields are determined (up to n = 15) from those primary coefficients using the 3D mantle conductivity model, including oceans, discussed in Kuvshinov et al. (2006).
This paper proposes a new method of compromising adjustment solution based on target decomposition strategy and Error Correction Chaos Optimization (ECCO) algorithm to mainly acquire rational primary coefficients, and kinetics parameters when necessary.
The input model describing the ionospheric primary field is taken from CM4 (Sabaka et al., 2004) while the secondary, induced, field is calculated from those primary coefficients using the same 3D mantle conductivity model as for the magnetospheric induced field.
These coefficients are related to primary coefficients (q_{nsp}^{m(c,s)}) and (s_{nsp}^{m(c,s)}) through a transfer function that is best expressed by using complex spherical harmonics and associated complex model coefficients.
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Note that there are only N = tmax/h primary coefficient vectors, each corresponding to a Spline knot on the curve; the other coefficient values are deduced using some prescribed boundary conditions.
where S S i is a measure of severity of stroke at initial diagnosis (GCS or NIHSS), X i is a vector of other relevant risk factors (i.e., demographic and case-mix adjustments listed earlier) for the ith patient and the primary coefficient of interest is β1 which provides the odds ratio for admission to SU (by center c and outcome o).
The primary coefficient of interest was β3, which captured the effect of the PBF program on the outcome Y.
The primary coefficient of interest is the triple interaction term (β7), which captures the difference in the impact of the program between the poor and the non-poor.
The primary coefficient of interest will be the time by group (control vs. intervention) interaction, which will indicate the degree of differential change across time between the control and intervention groups.
In this work, three new parameters, osmotic pressure coefficient, primary filtration coefficient and secondary selectivity rate, were introduced to replace the reflection coefficient in the K K equations.
As discussed earlier, aligned double quantization with step q1 followed by q2 maps the set of primary DCT coefficients c1 to the same secondary coefficients c2.
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