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Give the subspace filtration and the quotient filtration. If the degree- class of maps to zero, then with and . Thus and the class comes from . Inclusion is injective in every degree and the quotient map is surjective, proving the displayed short exact sequence of associated graded modules. Exactness can fail for arbitrarily chosen incompatible filtrations.
An Asian option whose averaging uses the geometric mean. In the constant-coefficient Black-Scholes model, the logarithm of the continuous geometric average is Gaussian with mean and variance , because . Its forward mean is . The discounted lognormal call formula gives its price. It is strictly cheaper than the terminal European call when and , since both its forward mean and log-variance are no larger, with strictly smaller variance. No unconditional comparison holds for arbitrary negative interest rates: for , sufficiently small positive strikes reverse the inequality.
If a traded payoff matrix has initial price vector with , there cannot be a negative-cost portfolio with nonnegative terminal payoff. Nevertheless a nonzero nonnegative attainable payoff supported only in zero-price states can cost zero and give an arbitrage. When every state has positive physical probability, excluding this possibility requires strictly positive Arrow state prices, not merely a nonnegative supporting vector.
Write a presheaf on as an arrow . Evaluation has the displayed chain, where , , and . The Hom-set bijections follow by solving the commuting-square equation. The functor has no right adjoint because it fails to preserve the initial object: is not .
The normalized information matrix for a homoscedastic linear regression model is the average outer product of its regressor vector. It is positive-definite precisely when the supported regressors span the parameter space. The full Fisher information matrix under normal errors is .
Use the north-pole stereographic projection and the cross-ratio convention . Antipodes have coordinates . Rotate the first point to the south pole, whose coordinate is zero: its antipode becomes infinity, while a point at spherical distance has projected modulus . Möbius invariance of the cross-ratio then gives the displayed identity. Antipodal endpoints require the extended-value interpretation.
For three Lie-algebra-valued functions of one variable, the Nahm equations areThey arise by taking a solution of the ASDYM equations with orientation , imposing independence of , and setting by a local Yang-Mills gauge transformation. Then , , and anti-self-duality of gauge curvature gives the displayed equations. The opposite orientation reverses their sign.
An isolated axisymmetric magnetic field cannot be sustained by ordinary resistive dynamo action with scalar positive magnetic diffusivity. Its poloidal magnetic flux function satisfies a homogeneous scalar advection-diffusion equation with no toroidal-to-poloidal source. The maximum principle excludes regeneration of that flux; after it decays the toroidal field has no lasting source either. This constrains the symmetry of the field. An axisymmetric flow may still generate a nonaxisymmetric field, and a turbulent mean-field electromotive force is not covered by the unmodified scalar-induction proof.
For a bounded conducting sphere with uniform magnetic diffusivity and an insulating exterior, an incompressible flow tangent to concentric spheres cannot sustain dynamo action. Neither the velocity nor the magnetic field needs to be axisymmetric. The radial magnetic scalar has a homogeneous advection-diffusion equation, so the poloidal field decays. Once it is absent, the toroidal magnetic potential also has a homogeneous scalar advection-diffusion equation. This is a theorem about spherical flow geometry, not about a general cylindrical flow with an axial component.
In the standard two-dimensional setting, with planar velocity and magnetic field independent of the third coordinate and homogeneous energy-closed boundary conditions, the in-plane magnetic potential is an advected diffusing scalar. Its quadratic integral decreases, preventing regeneration of a dynamo field. A third field component independent of that coordinate also obeys a passive advection-diffusion equation. A flow depending on two coordinates but possessing a third velocity component is not covered by this strictly planar formulation.
For a solenoidal three-component velocity depending on two periodic coordinates and a zero-mean magnetic field with the same dependence, the in-plane flux potential satisfies a homogeneous advection-diffusion equation. The Poincaré inequality gives . Integrating the vertical stretching term by parts bounds it by , where . Maximizing against resistive dissipation and integrating gives the displayed transient bound. Splitting off half the dissipation instead gives , proving vertical energy decays. This permits transient generation by a nonzero vertical velocity while excluding sustained fields in this zero-mean, z-independent periodic class.
For an ordered sequence of nested linear regression models , the sequential sum of squares for the th added term is . These are also called type-I sums of squares. They depend on term order when the design is not orthogonal. Dividing by the number of newly added coefficients and the full model's residual mean square gives the sequential F-test. A covariate added first is tested before adjustment for later terms, whereas a treatment added after the covariate is tested with that covariate already included.
An additive two-factor Gaussian model separates row and column effects. With one observation in each of cells, constraints fixing one row and column effect leave mean parameters and residual degrees of freedom. Balanced least squares gives fitted values equal to row mean plus column mean minus grand mean. With no cell replication, unrestricted interactions are confounded with residual error; the additive interpretation requires an assumption that those interactions are absent or negligible.
Multivariate analysis of variance compares mean vectors of several groups while accounting for correlations between their response variables. In the one-way normal model, independent observations share a positive-definite covariance matrix. Put and . Under equal means, these matrices have independent Wishart distributions with degrees of freedom and , respectively. This follows by separating the Gaussian data into orthogonal within-group and between-group projections. The Wilks lambda statistic tests equality of the means using both matrices, rather than independently testing each coordinate.
For and , the method of multiple scales gives the displayed amplitude-phase equations, together with constant leading phase. For , is constant and changes exponentially. For and positive amplitude, the integrable phase average is . Thus obeys with . The identically zero oscillator is inadmissible for logarithmic feedback, whose force is undefined there.
With the environment initially in , take to fix and , and rotate the span of by the displayed action and . This is a unitary operator. Its environment matrix elements and are the Kraus operators of the amplitude damping channel. Tracing out the environment multiplies the excited population by , transfers the remainder to the ground state, and multiplies off-diagonal entries by .
For risk-neutral stock dynamics , with and , let solve . A fixed downward trigger gives continuation value for . Optimizing over the trigger, or imposing smooth fit, gives the displayed boundary. The optimal value equals below and the continuation expression above. A verification argument uses its payoff majorization and nonpositive discounted generator. At and , the perpetual value is for positive spot, approached by triggers tending to zero rather than attained at a positive finite trigger.
Equal-density ion-neutral Alfvén dispersion relation by
Codex 0 Created 2026-10-14 Updated 2026-11-05
For equal ion and neutral mass densities, let , and use Fourier time dependence . Solenoidal displacements obey and . For nonzero frequency, the neutral equation gives . Substitution in the ion equation givesEquivalently, the growth rate obeys . A time-independent neutral displacement with zero velocity is a relabeling of a uniform fluid, not an additional wave root of the velocity/magnetic-field system.
For a regular category that is a small category, a regular functor to the Category of sets that reflects isomorphisms exists exactly when the category has almost total support for a regular category. Necessity follows because a nonempty image forces the object's support to be terminal, while an empty image makes all projections invertible and makes all equalizers of maps out of invertible. This proves that is strict initial. For sufficiency, use the capitalization theorem to map conservatively and regularly into a capital regular category, then take global sections of a capital regular category. Well-supported objects retain points; proper strict initial objects retain empty point sets. A bijection between nonempty point sets makes the image subobject entire and makes the kernel-pair diagonal entire, by well-pointedness. Thus the image arrow is both a regular epimorphism and a monomorphism, and is invertible. The capitalization theorem is a substantive existence input; this argument does not infer arbitrary large-category representability from small-category hypotheses.
Suppose is integrable and adapted, and is finite and adapted. Use the stopped predictable budget for adapted increments with an integer budget . The process is an integrable nonnegative supermartingale, because its budget decrement cancels the localized drift. It has a finite almost-sure limit. On the event that the total drift is smaller than , the stopping time is infinite, so itself converges. Taking the countable union over integer budgets proves finite almost sure convergence. No expectation of the total drift is needed.
Pinned article: Introduction to the OurBigBook Project
Welcome to the OurBigBook Project! Our goal is to create the perfect publishing platform for STEM subjects, and get university-level students to write the best free STEM tutorials ever.
Everyone is welcome to create an account and play with the site: ourbigbook.com/go/register. We belive that students themselves can write amazing tutorials, but teachers are welcome too. You can write about anything you want, it doesn't have to be STEM or even educational. Silly test content is very welcome and you won't be penalized in any way. Just keep it legal!
Intro to OurBigBook
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- topics: topics group articles by different users with the same title, e.g. here is the topic for the "Fundamental Theorem of Calculus" ourbigbook.com/go/topic/fundamental-theorem-of-calculusArticles of different users are sorted by upvote within each article page. This feature is a bit like:
- a Wikipedia where each user can have their own version of each article
- a Q&A website like Stack Overflow, where multiple people can give their views on a given topic, and the best ones are sorted by upvote. Except you don't need to wait for someone to ask first, and any topic goes, no matter how narrow or broad
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.
- to OurBigBook.com to get awesome multi-user features like topics and likes
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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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