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Copy file name to clipboardExpand all lines: doc/user/_theory/theory.rst
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@@ -117,7 +117,7 @@ This transform allows the frequency domain coefficients, :math:`B(\omega)`, to b
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Wave excitation force, :math:`F_{exc}(t)`
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~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
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The following method to compute the wave excitation force involves convolution between the excitation impulse response function:math:`K_{exc}(t)` and the wave elevation time sequence :math:`\eta(t)`:
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The following method to compute the wave excitation force involves convolution between the excitation Impulse Response Function (IRF):math:`K_{exc}(t)` and the wave elevation time sequence :math:`\eta(t)`:
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.. math::
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:label: f_ex
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By amalgamating these forces into the equation of motion, one can effectively model the behavior of a multibody oceanic system influenced by hydrodynamic forces.
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In HydroChrono, the force is computed through trapezoidal integration by discretizing at the time values given by the excitation IRF time array relative to the current simulation time step. Linear interpolation is done for the free surface elevation if a given time value is between two values of the time series of the precomputed free surface elevation.
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