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Update wave_sim-spectral.tex
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doc/wave_sim/wave_sim-spectral.tex

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@@ -665,12 +665,21 @@
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\paragraph{(ii) Maximum Entropy (MEM).}
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Choose $D$ to maximize Shannon entropy subject to matching measured harmonics (constraints):
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\begin{align}
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\max_{D\ge0}\quad & \mathcal{H}[D] = -\int_{0}^{2\pi} D\ln D\, d\theta,\\
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\text{s.t.}\quad & \int D\,d\theta=1,\quad
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\int D \cos n\theta\, d\theta = a_n,\quad
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\int D \sin n\theta\, d\theta = b_n,\; n=1,\ldots,N_h.
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\end{align}
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\begin{equation}
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\begin{aligned}
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\max_{D\ge 0}\quad
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& \mathcal{H}[D]
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= -\int_{0}^{2\pi} D \ln D \, d\theta,
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\\
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\text{s.t.}\quad
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& \int D\, d\theta = 1,
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\\
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& \int D \cos(n\theta)\, d\theta = a_n,
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\\
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& \int D \sin(n\theta)\, d\theta = b_n,
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\qquad n=1,\ldots,N_h.
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\end{aligned}
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\end{equation}
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The solution has the exponential family form
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\begin{equation}
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D(\theta)\propto
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\paragraph{(iii) Maximum Likelihood/Beamforming (MLM/EMLM).}
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For an array with steering $\mathbf{a}(\theta;f)$ and CSD $\mathbf{C}(f)$, the classic Capon/MLM estimator is
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\begin{equation}
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\widehat{D}_{\text{MLM}}(f,\theta)
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= \frac{1}{\mathbf{a}(\theta;f)^{\mathrm{H}}\,
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\mathbf{C}(f)^{-1}\,\mathbf{a}(\theta;f)}\;\bigg/ \;
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\int_{0}^{2\pi}\frac{d\varphi}{\mathbf{a}(\varphi;f)^{\mathrm{H}}\,
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\mathbf{C}(f)^{-1}\,\mathbf{a}(\varphi;f)}.
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\begin{aligned}
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\widehat{D}_{\text{MLM}}(f,\theta)
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&=
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\frac{
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\displaystyle
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\frac{1}{
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\mathbf{a}(\theta;f)^{\mathrm{H}}
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\mathbf{C}(f)^{-1}
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\mathbf{a}(\theta;f)
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}
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}{
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\displaystyle
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\int_{0}^{2\pi}
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\frac{d\varphi}{
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\mathbf{a}(\varphi;f)^{\mathrm{H}}
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\mathbf{C}(f)^{-1}
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\mathbf{a}(\varphi;f)
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}
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}.
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\end{aligned}
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\end{equation}
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optionally corrected for bias/noise in EMLM. This provides high directional resolution when aperture and SNR are adequate.
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\paragraph{Outputs and Integral Measures.}
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From $\widehat{S}(f,\theta)$ compute directional moments and spreads:
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\begin{align}
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\bar{\theta}(f) &= \arg\!\Big(\int e^{\mathrm{i}\theta} D(f,\theta)\, d\theta\Big),
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&
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\sigma_\theta^2(f) &= 2\Big(1-\big|\int e^{\mathrm{i}\theta} D(f,\theta)\, d\theta\big|\Big),\\
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m_n &= \int f^n \bigg(\int S(f,\theta)\,d\theta\bigg)\, df,
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&
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H_s &= 4\sqrt{m_0},\quad T_z=\sqrt{m_0/m_2},\quad T_{-10}=m_{-1}/m_0.
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\bar{\theta}(f)
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&= \arg\!\left(
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\int e^{\mathrm{i}\theta} D(f,\theta)\, d\theta
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\right),
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\\
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\sigma_\theta^2(f)
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&= 2\left(
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1-\left|
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\int e^{\mathrm{i}\theta} D(f,\theta)\, d\theta
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\right|
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\right),
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\\
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m_n
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&= \int f^n
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\left(
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\int S(f,\theta)\, d\theta
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\right)\, df,
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\\
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H_s &= 4\sqrt{m_0},
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\qquad
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T_z = \sqrt{m_0/m_2},
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\qquad
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T_{-10} = m_{-1}/m_0.
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\end{align}
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Directional partitions (wind sea vs.\ swells) can then be obtained by algorithms in \Cref{sec:wave-partitioning}.
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\end{thebibliography}
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\end{document}
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\end{document}

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