@@ -118,7 +118,7 @@ <h2 id="the-shared-object-one-schur-complement-two-readings">The shared
118118partition the variables into a block < span class ="math inline "> k</ span >
119119and a conditioning set < span class ="math inline "> c</ span > (its spatial
120120neighbours, or the other assets). The Schur complement < span
121- class ="math display "> \label{eq:schur }
121+ class ="math display "> \tag{1 }
122122 \mathsf S_k \;=\; R_{kk}-R_{kc}R_{cc}^{-1}R_{ck}</ span > carries the
123123same algebra into two meanings.</ p >
124124< p > < strong > Weather (a pseudo-likelihood term).</ strong > < span
@@ -151,20 +151,17 @@ <h2 id="the-shared-object-one-schur-complement-two-readings">The shared
151151statistician, a hedged residual risk for the investor.</ p >
152152< h5 id ="a-two-variable-example. "> A two-variable example.</ h5 >
153153< p > Take two standardized variables with correlation < span
154- class ="math inline "> \rho</ span > . The Schur complement < a
155- href ="#eq:schur " data-reference-type ="eqref "
156- data-reference ="eq:schur "> [eq:schur]</ a > is the scalar < span
157- class ="math inline "> \mathsf S=1-\rho^2</ span > . To the statistician it is
158- the variance of variable 2 conditional on variable 1, < span
154+ class ="math inline "> \rho</ span > . The Schur complement (1) is the scalar
155+ < span class ="math inline "> \mathsf S=1-\rho^2</ span > . To the statistician
156+ it is the variance of variable 2 conditional on variable 1, < span
159157class ="math inline "> \operatorname{Var}(y_2\mid y_1)=1-\rho^2</ span > —the
160158term the pseudo-likelihood scores. To the investor it is the variance of
161159variable 2 < em > net of its hedge</ em > by variable 1: with optimal hedge
162160ratio < span class ="math inline "> b=\rho</ span > , the residual < span
163161class ="math inline "> y_2-b\,y_1</ span > has variance < span
164162class ="math inline "> 1-\rho^2</ span > , the risk that remains after the
165- hedge. Identical number, two stories. Damping < a href ="#eq:damp "
166- data-reference-type ="eqref " data-reference ="eq:damp "> [eq:damp]</ a > gives
167- < span class ="math inline "> \mathsf S(\gamma)=(1-\gamma)\cdot
163+ hedge. Identical number, two stories. Damping (2) gives < span
164+ class ="math inline "> \mathsf S(\gamma)=(1-\gamma)\cdot
1681651+\gamma(1-\rho^2)=1-\gamma\,\rho^2</ span > : at < span
169166class ="math inline "> \gamma=1</ span > the full hedge / full conditioning,
170167at < span class ="math inline "> \gamma=0</ span > none (the marginal
@@ -181,7 +178,7 @@ <h2 id="the-shared-cure-damping-by-reliability">The shared cure: damping
181178class ="math inline "> \mathsf S_k</ span > overfit—and both apply the same
182179cure, a convex damping by < span
183180class ="math inline "> \gamma\in[0,1]</ span > : < span
184- class ="math display "> \label{eq:damp }
181+ class ="math display "> \tag{2 }
185182 b_k(\gamma)=\gamma\,b_k,\qquad \mathsf
186183S_k(\gamma)=(1-\gamma)\,R_{kk}+\gamma\,\mathsf S_k.</ span > At < span
187184class ="math inline "> \gamma=1</ span > this is full conditioning—the exact
@@ -190,14 +187,13 @@ <h2 id="the-shared-cure-damping-by-reliability">The shared cure: damping
190187block-diagonal composite likelihood, hierarchical risk parity.
191188Intermediate < span class ="math inline "> \gamma</ span > trusts the
192189estimated cross-coupling only partway. The weather and portfolio
193- extremes are the < em > same</ em > two endpoints of < a href ="#eq:damp "
194- data-reference-type ="eqref " data-reference ="eq:damp "> [eq:damp]</ a > .</ p >
190+ extremes are the < em > same</ em > two endpoints of (2).</ p >
195191< p > The optimal < span class ="math inline "> \gamma</ span > has a closed
196192form. For a single coupling of conditional < span
197193class ="math inline "> R^2</ span > equal to < span
198194class ="math inline "> \rho^2</ span > estimated from < span
199195class ="math inline "> n</ span > points, minimizing expected error gives the
200- < em > reliability</ em > < span class ="math display "> \label{eq:gstar }
196+ < em > reliability</ em > < span class ="math display "> \tag{3 }
201197 \gamma^\star=\frac{(n-2)\rho^2}{(n-2)\rho^2+(1-\rho^2)},</ span > a
202198Wiener/James–Stein shrinkage < span class ="citation "
203199data-cites ="james1961 ledoit2012 "> (James and Stein 1961; Ledoit and Wolf
@@ -214,9 +210,7 @@ <h2 id="the-shared-cure-damping-by-reliability">The shared cure: damping
214210< em > operation</ em > it scales. It is < em > not</ em > the raw off-diagonal
215211entries shrunk elementwise toward zero; it is the conditional regression
216212< span class ="math inline "> b_k</ span > and its Schur complement < span
217- class ="math inline "> \mathsf S_k</ span > , damped through < a
218- href ="#eq:damp " data-reference-type ="eqref "
219- data-reference ="eq:damp "> [eq:damp]</ a > —a structured,
213+ class ="math inline "> \mathsf S_k</ span > , damped through (2)—a structured,
220214positive-definiteness-preserving shrinkage of the < em > conditional</ em > .
221215Damping < span class ="math inline "> b_k</ span > by < span
222216class ="math inline "> \gamma</ span > scales the cross-covariance by < span
@@ -243,16 +237,15 @@ <h2 id="the-shared-cure-damping-by-reliability">The shared cure: damping
243237precursor < span class ="citation " data-cites ="cotton2025psl "> (Cotton
2442382025)</ span > , which did cite the Vecchia factorization—but only as a
245239computational device for the block-conditional likelihood, without
246- recognizing that the damping < a href ="#eq:damp "
247- data-reference-type ="eqref " data-reference ="eq:damp "> [eq:damp]</ a > is a
248- < em > regularized</ em > Vecchia conditioning, nor its place in the
249- scalable-Gaussian-process literature, nor that the same reliability is
250- precisely the knob of Schur-complementary allocation. (We have since
251- learned that ShrinkTM < span class ="citation "
252- data-cites ="chakraborty2025 "> (Chakraborty and Katzfuss 2025)</ span > was
253- independently arriving at the conditional shrinkage at the same time,
254- from the spatial side.) That these were one object went unnoticed when
255- the first note was written; surfacing it is the purpose of this one.</ p >
240+ recognizing that the damping (2) is a < em > regularized</ em > Vecchia
241+ conditioning, nor its place in the scalable-Gaussian-process literature,
242+ nor that the same reliability is precisely the knob of
243+ Schur-complementary allocation. (We have since learned that ShrinkTM
244+ < span class ="citation " data-cites ="chakraborty2025 "> (Chakraborty and
245+ Katzfuss 2025)</ span > was independently arriving at the conditional
246+ shrinkage at the same time, from the spatial side.) That these were one
247+ object went unnoticed when the first note was written; surfacing it is
248+ the purpose of this one.</ p >
256249< h2 id ="what-each-side-already-solved "> What each side already
257250solved</ h2 >
258251< p > Read as one operation, the two literatures are complementary rather
@@ -261,9 +254,8 @@ <h2 id="what-each-side-already-solved">What each side already
261254data-reference ="tab:sides "> 1</ a > ).</ p >
262255< div id ="tab:sides ">
263256< table >
264- < caption > The same Schur damping < a href ="#eq:damp "
265- data-reference-type ="eqref " data-reference ="eq:damp "> [eq:damp]</ a > , as
266- developed on each side.</ caption >
257+ < caption > The same Schur damping (2), as developed on each
258+ side.</ caption >
267259< thead >
268260< tr >
269261< th style ="text-align: left; "> </ th >
@@ -314,10 +306,9 @@ <h2 id="what-each-side-already-solved">What each side already
314306< em > learning</ em > the damping toward a fitted base < span
315307class ="citation " data-cites ="chakraborty2025 "> (Chakraborty and Katzfuss
3163082025)</ span > . The allocation side contributes the < em > closed form</ em >
317- < a href ="#eq:gstar " data-reference-type ="eqref "
318- data-reference ="eq:gstar "> [eq:gstar]</ a > and the recognition that the
319- same < span class ="math inline "> \gamma</ span > is an investment decision,
320- not only a regularizer. Neither side had both.</ p >
309+ (3) and the recognition that the same < span
310+ class ="math inline "> \gamma</ span > is an investment decision, not only a
311+ regularizer. Neither side had both.</ p >
321312< p > The two sides also shrink toward different < em > targets</ em > , and the
322313asymmetry is not arbitrary: each shrinks toward the structure it can
323314trust. A spatial field has a credible parametric model—a smooth Matérn
@@ -330,13 +321,9 @@ <h2 id="what-each-side-already-solved">What each side already
330321class ="math inline "> \gamma=0</ span > / HRP limit). Where weather has
331322structure to believe, finance has structure to doubt—so it is
332323unsurprising, in hindsight, that the spatial road centers on a base GP
333- while the allocation road errs toward zero coupling. The operation < a
334- href ="#eq:damp " data-reference-type ="eqref "
335- data-reference ="eq:damp "> [eq:damp]</ a > and its optimal intensity < a
336- href ="#eq:gstar " data-reference-type ="eqref "
337- data-reference ="eq:gstar "> [eq:gstar]</ a > are the same; only the prior
338- they lean on differs, in the direction each domain’s experience
339- warrants.</ p >
324+ while the allocation road errs toward zero coupling. The operation (2)
325+ and its optimal intensity (3) are the same; only the prior they lean on
326+ differs, in the direction each domain’s experience warrants.</ p >
340327< h2 id ="an-example-importing-vecchia-into-allocation "> An example:
341328importing Vecchia into allocation</ h2 >
342329< p > The clearest way to show the connection is useful is to carry a tool
@@ -349,9 +336,8 @@ <h2 id="an-example-importing-vecchia-into-allocation">An example:
349336< p > We apply Vecchia conditioning to daily asset returns—a setting with
350337no parametric base, using a correlation-based neighbour ordering of the
351338kind the spatial literature adopts when Euclidean distance is
352- unavailable—and compare three settings of the damping < a href ="#eq:damp "
353- data-reference-type ="eqref " data-reference ="eq:damp "> [eq:damp]</ a > :
354- undamped (< span class ="math inline "> \gamma=1</ span > , plain Vecchia /
339+ unavailable—and compare three settings of the damping (2): undamped
340+ (< span class ="math inline "> \gamma=1</ span > , plain Vecchia /
355341minimum-variance conditioning), the closed-form reliability < span
356342class ="math inline "> \gamma^\star</ span > , and a single intensity tuned on
357343a held-out split (the spatial community’s < em > fit-the-shrinkage</ em >
@@ -466,9 +452,8 @@ <h2 id="an-example-importing-vecchia-into-allocation">An example:
466452actually operates.</ p >
467453< h2 id ="the-reverse-import-robustifying-the-hedge "> The reverse import:
468454robustifying the hedge</ h2 >
469- < p > The transfer also runs the other way. The damping < a href ="#eq:damp "
470- data-reference-type ="eqref " data-reference ="eq:damp "> [eq:damp]</ a > can
471- be used as an < em > estimator</ em > — form each block’s hedge < span
455+ < p > The transfer also runs the other way. The damping (2) can be used as
456+ an < em > estimator</ em > — form each block’s hedge < span
472457class ="math inline "> b_k</ span > and Schur complement < span
473458class ="math inline "> \mathsf S_k</ span > , damp by < span
474459class ="math inline "> \gamma^\star</ span > , and reassemble the implied
@@ -506,18 +491,15 @@ <h2 id="discussion">Discussion</h2>
506491class ="math inline "> \gamma=0</ span > and < span
507492class ="math inline "> \gamma=1</ span > ends of the very damping that a
508493weather model applies to stay estimable is not a metaphor—it is the same
509- Schur complement < a href ="#eq:schur " data-reference-type ="eqref "
510- data-reference ="eq:schur "> [eq:schur]</ a > and the same convex combination
511- < a href ="#eq:damp " data-reference-type ="eqref "
512- data-reference ="eq:damp "> [eq:damp]</ a > , read once as a conditional
513- variance and once as a residual risk. Practical consequences run both
514- ways. Allocation can borrow the spatial machinery: neighbour/cluster
515- orderings and empirical-Bayes-fitted damping in place of a fixed < span
516- class ="math inline "> \gamma</ span > . Spatial modeling can borrow the
517- allocation reading: the closed-form reliability as a tuning-free
518- initializer, and the reminder that the damping is a decision with a
519- cost, not merely a prior. And both sit on one online primitive—a Schur
520- complement of a few neighbour blocks, damped by a
494+ Schur complement (1) and the same convex combination (2), read once as a
495+ conditional variance and once as a residual risk. Practical consequences
496+ run both ways. Allocation can borrow the spatial machinery:
497+ neighbour/cluster orderings and empirical-Bayes-fitted damping in place
498+ of a fixed < span class ="math inline "> \gamma</ span > . Spatial modeling can
499+ borrow the allocation reading: the closed-form reliability as a
500+ tuning-free initializer, and the reminder that the damping is a decision
501+ with a cost, not merely a prior. And both sit on one online primitive—a
502+ Schur complement of a few neighbour blocks, damped by a
521503reliability—maintainable incrementally in < span
522504class ="math inline "> O(p\,m^2)</ span > . This is the form in which the
523505online covariance library < code > precise</ code > < a href ="#fn1 "
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