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The thermosteric sea-level rise component is calculated from the ocean density derived from the model's temperature and salinity fields.
The shadowing effect of the direct signal component is calculated using Kirchhoff diffraction equation.
Seasonal component is calculated by averaging the de-trended values for that particular time of all the days.
This variable gain component is calculated from the amplification necessary to reach a maximum amplitude within a gate to a pre-set value.
The CN size distribution spectrum for a single chemical component is calculated as prognostic variables for each of the model's spatial grid points.
Further, the energy of each component is calculated using Parseval's theorem, and the component in which mode shape exists is worked upon.
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The pressure schedule, the overall forming time and the final thickness distribution in the formed component were calculated.
The Fourier amplitude spectrum (FAS) for each component was calculated.
Values for each magnetic component are calculated within successive 30-day periods.
Values for each magnetic component are calculated within within successive 30-day periods.
The concentration of each component was calculated using the calibration model.
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