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A coarse-grid correction improves a fine-grid approximation by solving a smaller equation for the part of its approximation error representable on a coarse mesh. Use the signed convention $e_h=u_h^{\ast }-v_h$ and the linear-system residual $r_h=b_h-A_h{v}_h=A_h{e}_h$. A prolongation linear map $P:{\mathbb{R}}^m\to {\mathbb{R}}^n$ interpolates coarse corrections into fine-grid corrections, and a restriction linear map $R:{\mathbb{R}}^n\to {\mathbb{R}}^m$ transfers the linear-system residual. Solve $A_H{z}_H=R{r}_h$ exactly or approximately and update $v_h\leftarrow v_h+P{z}_H$. The plus sign follows from defining the approximation error as exact minus approximate. It is the correction equation's right-hand side $R{r}_h$, rather than merely restricted solution values, that determines the update.

For the multigrid method model $A_h=h^{-2}\mathrm{tridiag}(-1,2,-1)$, take $n=2m+1$, so $H=2h$ and the coarse nodes coincide with every second fine node. Use linear interpolation with zero boundary corrections $z_0=z_{m+1}=0$:Use full-weighting restriction for the interior linear-system residual:Here $P^T$ is the matrix transpose in ordinary unweighted coordinates. With these specific transfers, the Galerkin coarse-grid operator isThus it equals the rediscretized Poisson equation operator on this constant-coefficient one-dimensional mesh. The equality is special to the stated model and transfers. In particular, dropping $h^{-2}$ from the fine matrix while using $H^{-2}$ on the coarse mesh changes the correction unless the right-hand sides and transfers are rescaled consistently.

Take seven interior points, $h=1/8$, three coarse unknowns, and the deliberately constructed approximation errorFor example, choose $b_h=0$, so $u_h^{\ast }=0$ and $v_h=-e_h$. Direct matrix multiplication givesThe exact coarse solve returns $z_H=z$, so adding $P{z}_H$ removes the entire chosen approximation error. A broad triangular error can have a sharply localized linear-system residual: the latter measures discrete curvature, not error height. This is why the two should not be confused. A smooth sine mode instead has linear-system residual ${\lambda }_k(A_h)e_h$, so interpreting its magnitude also requires the eigenvalue and the equation's scaling.

The algebra explains the exact cancellation beyond this example. Assume $P$ has linearly independent columns and choose an invertible Galerkin coarse-grid operator $A_H=R{A}_{h}P$. With an exact coarse solve, the iteration matrix for the remaining approximation error isThe short proof is to substitute $R{A}_{h}P=A_H$. Thus every vector in the column space of $P$ is eliminated, and the corrected linear-system residual restricts to zero. These are exact projection identities, not a statement that every visually smooth vector belongs to that column space. If $A_h$ is a symmetric matrix and a positive-definite matrix, and $R=c{P}^T$ with $c>0$, then $A_H$ is also a positive-definite matrix. Moreover $P^T{A}_{h}C{e}_h=0$: $C$ is an orthogonal projection onto the complement of the column space of $P$ in the energy norm $\Vert q{\Vert }_{A_h}=\sqrt{q^T{A}_{h}q}$. Equivalently, the added correction is the best approximation to $e_h$ from that column space in this energy norm. Without these symmetry and transfer assumptions, the projection need not be orthogonal.^[ref]

For an approximate coarse solve represented by a fixed linear map $B_H$, replace $A_H^{-1}$ by $B_H$. ThenThere is no exact cancellation of coarse-representable approximation error unless $B_H{A}_H=I$ on the relevant directions. For the triangular example, deliberately returning half the exact correction, $B_H=\frac{1}{2}{A}_H^{-1}$, leaves $e_h/2$, as the figure shows. This controlled mathematical comparison illustrates an incomplete coarse solve; it is not a measured performance result or a prescription for a geometric multigrid V-cycle. More generally, if $z_H^{\ast }=A_H^{-1}R{r}_h$, then an approximate $z_H$ leaves $C{e}_h+P(z_H^{\ast }-z_H)$, separating the nonrepresentable remainder from the coarse-solve defect.

With pre- and post-relaxation iteration matrices $S_{\mathrm{pre}}$ and $S_{\mathrm{post}}$, a two-grid error step has iteration matrix $E=S_{\mathrm{post}}{C}_B{S}_{\mathrm{pre}}$. A geometric multigrid V-cycle supplies $B_H$ by one recursive coarse cycle from zero, with a direct solve only at the bottom. Effective smoothing, a coarse column space that approximates the surviving approximation error, and a sufficiently accurate coarse correction must work together. Coarsening alone supplies no convergence guarantee, and correcting an arbitrary fine-grid vector exactly would require a coarse column space large enough to contain it.

The multigrid method addresses a characteristic failure of single-grid relaxation: its cheapest updates rapidly remove oscillatory error but barely change smooth error. For example, the one-dimensional Poisson equation matrix has diagonal $2/h^2$. The weighted Jacobi method with weight $\omega$ has Fourier error factorAt low physical frequency, $\theta =O(h)$ and this factor is $1-O(h^2)$, requiring $O(h^{-2})$ sweeps for a fixed error reduction. With $\omega =2/3$, high grid frequencies $\pi /2\le |\theta |\le \pi$ are multiplied by at most $1/3$ in modulus. Smooth error on a fine mesh is well represented on a coarser mesh, where it is relatively more oscillatory and hence cheaper to remove. These two complementary mechanisms motivate smoothing and coarse-grid correction.

Write the discrete problem as $A_h{u}_h=f_h$. For an approximation $v_h$, the residual is $r_h=f_h-A_h{v}_h$ and the error $e_h=u_h-v_h$ satisfies $A_h{e}_h=r_h$. It is this error equation that is transferred to a coarse grid; restricting the approximate solution alone would not solve the missing error. With prolongation $P$ and restriction $R$, solveFor nested Cartesian grids with $H=2h$, linear interpolation copies a coarse value at a coincident fine node and averages the two nearest coarse values at an intermediate node. Its two-dimensional counterpart is bilinear interpolation. Full-weighting restriction uses weights $(1,2,1)/4$ in one dimension andin two dimensions. With these choices $R=2^{-d}{P}^T$ in ordinary coordinate inner products. A Galerkin coarse-grid operator is $A_H=R{A}_{h}P$; alternatively one can rediscretize the PDE on the coarse mesh when that choice remains compatible with the transfers.

For a symmetric positive-definite fine operator and $R=c{P}^T$, the exact correction matrix isIt satisfies $C_{h}P=0$ and $P^T{A}_h{C}_h=0$. Thus it removes the coarse-space component of the error and is an orthogonal projection in the energy inner product. With pre- and post-smoothing matrices $S_{\mathrm{pre}},S_{\mathrm{post}}$, the exact two-grid error matrix is $S_{\mathrm{post}}{C}_h{S}_{\mathrm{pre}}$. Effective smoothing on the complementary space and accurate coarse representation of smooth error are both needed for contraction.

A concrete harmonic calculation makes the mechanism quantitative. On the one-dimensional constant-coefficient problem, couple the two harmonics $\theta$ and $\theta +\pi$, put $s={\sin }^2(\theta /2)$ and $c=1-s$, and use the above transfers. Linear interpolation has harmonic weights $(c,s{)}^T$, while the fine operator has diagonal symbol $4\mathrm{diag}(s,c)/h^2$. Therefore its Galerkin correction on this pair isOne pre- and one post-sweep of weighted Jacobi with $\omega =2/3$ gives $E=SCS$, $S=\mathrm{diag}(1-4s/3,1-4c/3)$. This rank-one matrix has eigenvalues zero andThe two-grid Poisson factor with weighted Jacobi is therefore mesh-independent in this model. A periodic constant nullspace must first be removed; a Dirichlet problem has no such nullspace. This is evidence for the design, not a claim that the same factor applies to every PDE or every smoother.

The geometric multigrid V-cycle replaces the exact coarse solve by one recursively defined coarse cycle. A complete implementation on level $\ell$ proceeds as follows:

Boundary values of the solution are imposed on the fine level; the error equation has homogeneous boundary conditions when those values were already imposed exactly. Residuals must be computed after pre-smoothing, not before. The zero initialization on each recursive error solve makes the cycle an error correction rather than an accidental addition of an old coarse solution. For an energy-symmetric cycle usable in conjugate gradient method, choose compatible adjoint transfers and symmetric smoothing, such as forward Gauss-Seidel before correction and its backward sweep afterward.

With bounded stencil size and fixed sweep counts, a sweep, residual calculation or transfer costs $O(N_{\ell })$. Uniform coarsening gives $N_{\ell -1}\approx 2^{-d}{N}_{\ell }$, soIf the full V-cycle has an error reduction factor $q<1$ independent of mesh size, reducing an arbitrary initial algebraic error by a factor $\epsilon$ takes $O(\log (1/\epsilon ))$ cycles and $O(N\log (1/\epsilon ))$ work. Linear work per cycle alone does not prove the mesh-independent factor; it rests on the smoothing and approximation properties just illustrated. Full multigrid starts on a coarse mesh, interpolates its solution to each successive finer mesh, and uses a few cycles per level. When the interpolation accuracy and cycle contraction match the discretization error, this reaches discretization-level accuracy in $O(N)$ work.

Performance depends on the operator. Strong anisotropy can leave error oscillatory in one direction but weakly penalized by the differential operator, defeating point smoothing; line or plane relaxation and selective coarsening address this. Large coefficient jumps demand compatible coarse spaces. Nonrectangular meshes motivate algebraic rather than purely geometric coarsening. Nonlinear problems use a full-approximation formulation instead of the linear residual correction verbatim. Singular Neumann or periodic operators need right-hand-side compatibility and consistent nullspace treatment on every level. Multigrid is fast because its components address different error scales, not because coarsening alone guarantees a good solver.

A multigrid method alternates local error damping with correction on coarser grids. For clarity write $A_h=h^{-2}$ times the five-point stencil and $A_h{u}_h=f_h$, incorporating Dirichlet boundary data into the right side. One two-grid cycle proceeds as follows.

The coarse solve is performed recursively, with a direct solve on the smallest grid, giving a V-cycle. Smoothing treats oscillations that are cheap for local relaxation to remove; coarse-grid correction treats errors that appear smooth on the fine grid. The scaling of the residual and coarse operator must agree if one instead uses the paper's unscaled stencil.

Use the fine matrix $A_h$ and right-hand side from part (b), with diagonal $D_h$. Starting from an iterate $v$, take $\nu$ weighted Jacobi smoothing stepsForm the residual $r_h=b_h-A_{h}v$. For coarse interior indices $j=1,\dots ,m/2-1$, use full-weighting restrictionThe prolongation operator matrix $P$ is linear interpolation of a coarse correction: $(Pe{)}_{2j}=e_j$ and $(Pe{)}_{2j+1}=(e_j+e_{j+1})/2$, with zero endpoint corrections. Thus $R=P^T/2$. Choose the Galerkin coarse-grid operator $A_c=R{A}_{h}P$, solve $A_c{e}_c=R{r}_h$ exactly, and correct $v\leftarrow v+P{e}_c$. The entries of $A_h$, $R$ and $P$ above specify every matrix in the cycle. A rediscretized coarse operator is another standard choice if used consistently.

For a nonsingular coarse operator, the fine-grid iteration matrix of this pre-smoothed two-grid cycle isThe purpose of under-relaxation is to damp fine-grid oscillations, leaving smoother error for coarse-grid correction. For the diffusion-dominated one-dimensional operator, $\omega =2/3$ is the usual effective choice; the high-frequency symbol $1-\omega (1-\cos \xi )$ then has modulus at most $1/3$ for $\pi /2\le |\xi |\le \pi$. Coefficients and convection can change the best parameter, so this is a motivated choice rather than a universal optimum. Under the diagonal-dominance condition, the unweighted Jacobi matrix already has norm less than one in the maximum norm, and its convex combination with the identity remains convergent for $0<\omega <1$.

A prolongation operator transfers a coarse-grid correction to a finer mesh. For nested one-dimensional grids of spacings $2h$ and $h$, linear interpolation sets $(Pe{)}_{2j}=e_j$ and $(Pe{)}_{2j+1}=(e_j+e_{j+1})/2$, with zero endpoint values for homogeneous correction boundary conditions. The associated full-weighting restriction is $R=P^T/2$, and the Galerkin coarse-grid operator is $R{A}_{h}P$. The correction equation acts on the residual so that a coarse representation of the error can improve the fine-grid approximation.

For the one-dimensional Poisson equation, use linear interpolation, full-weighting restriction, an exact coarse solve, and one pre- and one post-sweep of weighted Jacobi with weight $2/3$. On a pair of harmonics $\theta ,\theta +\pi$, put $s={\sin }^2(\theta /2)$ and $c=1-s$. The coarse correction is $C=\left(\begin{array}{cc}s& -c\\ -s& c\end{array}\right)$, and the smoother is $S=\mathrm{diag}(1-4s/3,1-4c/3)$. The rank-one error operator $SCS$ has nonzero eigenvalue $s(1-4s/3{)}^2+c(1-4c/3{)}^2=1/9$. This exact harmonic calculation illustrates mesh-independent two-grid contraction for the constant-coefficient model; it is not an unconditional result for arbitrary operators or transfer choices.