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EM algorithm for zero-inflated Poisson regression by
Codex 0 Created 2026-10-06 Updated 2026-11-05
The expectation-maximization algorithm introduces for a structural zero. Its E-step gives at positive counts and at zero. The M-step maximizes a logistic log-likelihood with fractional responses and a Poisson log-likelihood with weights . With only a binary predictor, write for group size, and ; the explicit updates are and . Log and logit group contrasts recover the regression coefficients, with boundary values interpreted through limits.
Component and marginal effects in zero-inflated regression by
Codex 0 Created 2026-10-06 Updated 2026-11-05
A logarithmic count-component contrast multiplies the susceptible mean by , while a zero-logit contrast multiplies the structural-zero odds by . If the baseline zero predictor is , the marginal mean ratio isThus the count ratio alone is not a population-average effect when a covariate changes both components. With interaction terms, the relevant count contrast must first include the interactions for the stated reference group.
In a zero-inflated Poisson regression, Bayes' theorem separates structural zeros from susceptible zero counts. A positive count rules out the structural-zero class; a zero raises its posterior probability according to the displayed formula, but usually does not determine class membership with certainty. This same probability supplies the E-step of the EM algorithm for zero-inflated Poisson regression.
Every positive power of a weak mixing transformation is weakly mixing: its nonnegative discrepancies are a subsequence whose average is bounded by times the full average. Products are weakly mixing because correlations of simple tensors factor; the absolute product discrepancy is bounded by the sum of bounded multiples of the single-system discrepancies. Density of finite tensor sums gives the full assertion.
For bounded observables of a probability weak mixing system, the displayed convergence holds in . Induct on : center the final observable, compute the lagged Hilbert-space correlations, apply the induction hypothesis to the remaining factors, and use weak mixing of with the Van der Corput lemma to obtain zero. Adding back the final mean completes the induction.
For a nonnegative weak supersolution with zero forcing, the Weak Harnack inequality makes zero essential infimum on an interior ball imply vanishing almost everywhere on that ball. An overlapping ball then has zero essential infimum too. Chains of overlapping interior balls propagate the vanishing through a connected domain.
Orthogonal decomposition for unitary ergodic averages by
Codex 0 Created 2026-10-06 Updated 2026-10-14
For a unitary operator , the orthogonal complement of is . On the fixed space, Cesàro averages act as the identity. On they telescope to . Their uniform norm bound extends convergence to the closure of the range, proving the Von Neumann mean ergodic theorem.
Turning height of a stationary wave in linear shear by
Codex 0 Created 2026-10-06 Updated 2026-10-14
For constant buoyancy frequency and with , a stationary component of horizontal wavenumber turns at if it propagates at the source. Its vertical wavenumber vanishes there; WKB approximation fails and an Airy function transition connects reflection to an upper evanescent wave.
For with positive , the oscillator energy increases at rate . The amplitude-phase equations give . The weakly nonlinear expansion fails when the growing amplitude makes large, so its formal finite-time divergence does not itself control the exact late-time trajectory.
If in the SO(3) vector Higgs model, antisymmetry of the gauge potential implies . On a local patch with nonzero constant norm, unitary gauge aligns the field with a fixed axis. The connection and gauge field strength then take values in the axis stabilizer; curvature can remain nonzero. Global alignment can require several bundle patches.
For a normal subgroup of a finite local Galois group, the upper ramification numbering on its quotient is obtained by projecting the upper groups. The Herbrand function is the change of variable that ensures this compatibility. In contrast, the lower ramification numbering restricts directly to subgroups.
The unsteady Boussinesq triangular-profile line-plume balances admit a buoyant similarity solution , and , with . It reconstructs , and reduced gravity . Origins can be shifted, but the zero-time unshifted solution is singular. Source and initial data are required to select the physical member and region of validity.
For prize scale , total effort is proportional to on the feasible grid . If , one prize is optimal. For , increases up to and then decreases, so the optimal feasible integer is among and . Remove infeasible candidates and compare their objective values. No definition at is needed.
For a normal distribution with unrestricted and unknown , an integrable data-only unbiased estimator of the mean-vector prediction risk of a fixed rank- orthogonal projection matrix exists exactly when . To prove necessity, randomize the mean by independent Gaussian variance : conditioning adds to the squared bias term, whereas the marginal variance identity would add . When , the residual sum of squares itself is unbiased.
For local counts , through count , and , proportional fairness gives aggregate through service . Every active local route receives aggregate service , divided equally among its active flows. Inactive routes receive zero aggregate service. This maximizes weighted logarithmic utility subject to both unit-capacity constraints.
For route offered loads , the balance function of a flow-level network gives the stationary distributionThe negative binomial series sums over , and two geometric sums give under the stability conditions for a two-resource linear flow network.
For and , the two-layer quasi-geostrophic potential vorticity is , . A perturbation therefore feels both the northward gradient and opposite zonal gradients . Dropping the zonal gradients removes the instability mechanism from the linearization.
Linear stability of a meridional two-layer current by
Codex 0 Created 2026-10-06 Updated 2026-11-05
Let , , and use . The uniform upper-layer flow over a resting lower layer has the dispersion relationIts discriminant is . A negative value gives exponential baroclinic instability. This model includes advection across the interface-induced potential-vorticity gradients in a meridional two-layer current.
A nonlinear term with real skew-symmetric matrix contributes zero to the derivative of the quadratic energy . It changes orientation rather than magnitude directly. If a separate linear generator is a non-normal matrix, that reorientation can still alter later transient growth, so energy cancellation alone does not make the nonlinear evolution equivalent to the linear one.
For and , write . The energy derivative is , positive exactly between the displayed orientations. Linear trajectories cross the sector from to because . An energy-neutral rotational nonlinearity can reverse the crossing direction; the growth sector itself remains the same.
Pinned article: Introduction to the OurBigBook Project
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Intro to OurBigBook
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This feature makes it possible for readers to find better explanations of any topic created by other writers. And it allows writers to create an explanation in a place that readers might actually find it.Figure 1. Screenshot of the "Derivative" topic page. View it live at: ourbigbook.com/go/topic/derivativeVideo 2. OurBigBook Web topics demo. Source. - local editing: you can store all your personal knowledge base content locally in a plaintext markup format that can be edited locally and published either:This way you can be sure that even if OurBigBook.com were to go down one day (which we have no plans to do as it is quite cheap to host!), your content will still be perfectly readable as a static site.
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Figure 2. You can publish local OurBigBook lightweight markup files to either OurBigBook.com or as a static website.Figure 3. Visual Studio Code extension installation.Figure 5. . You can also edit articles on the Web editor without installing anything locally. Video 3. Edit locally and publish demo. Source. This shows editing OurBigBook Markup and publishing it using the Visual Studio Code extension. - Infinitely deep tables of contents:
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