Adjoint state method

The adjoint state method is a numerical method for efficiently computing the gradient of a function or operator in a numerical optimization problem.[1] It has applications in geophysics, seismic imaging, photonics and more recently in neural networks.[2]

The adjoint state space is chosen to simplify the physical interpretation of equation constraints.[3]

Adjoint state techniques allow the use of integration by parts, resulting in a form which explicitly contains the physically interesting quantity. An adjoint state equation is introduced, including a new unknown variable.

The adjoint method formulates the gradient of a function towards its parameters in a constraint optimization form. By using the dual form of this constraint optimization problem, it can be used to calculate the gradient very fast. A nice property is that the number of computations is independent of the number of parameters for which you want the gradient. The adjoint method is derived from the dual problem[4] and is used e.g. in the Landweber iteration method.[5]

The name adjoint state method refers to the dual form of the problem, where the adjoint matrix is used.

When the initial problem consists of calculating the product and must satisfy , the dual problem can be realized as calculating the product (), where must satisfy . And is called the adjoint state vector.

General case

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The original adjoint calculation method goes back to Jean Cea,[6] with the use of the Lagrangian of the optimization problem to compute the derivative of a functional with respect to a shape parameter.

For a state variable , an optimization variable , an objective functional is defined. The state variable is often implicitly dependent on through the (direct) state equation (usually the weak form of a partial differential equation), thus the considered objective is . Usually, one would be interested in calculating using the chain rule:

Unfortunately, the term is often very hard to differentiate analytically since the dependance is defined through an implicit equation. The Lagrangian functional can be used as a workaround for this issue. Since the state equation can be considered as a constraint in the minimization of , the problem

has an associate Lagrangian functional defined by

where is a Lagrange multiplier or adjoint state variable and is an inner product on . The method of Lagrange multipliers states that a solution to the problem has to be a stationary point of the lagrangian, namely

where is the Gateaux derivative of with respect to in the direction . The last equation is equivalent to , the state equation, to which the solution is . The first equation is the so-called adjoint state equation,

because the operator involved is the adjoint operator of , . Resolving this equation yields the adjoint state . The gradient of the quantity of interest with respect to is (the second equation with and ), thus it can be easily identified by subsequently resolving the direct and adjoint state equations. The process is even simpler when the operator is self-adjoint or symmetric since the direct and adjoint state equations differ only by their right-hand side.

Example: Linear case

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In a real finite dimensional linear programming context, the objective function could be , for , and , and let the state equation be , with and .

The lagrangian function of the problem is , where .

The derivative of with respect to yields the state equation as shown before, and the state variable is . The derivative of with respect to is equivalent to the adjoint equation, which is, for every ,

Thus, we can write symbolically . The gradient would be

where is a third order tensor, is the dyadic product between the direct and adjoint states and denotes a double tensor contraction. It is assumed that has a known analytic expression that can be differentiated easily.

Numerical consideration for the self-adjoint case

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If the operator was self-adjoint, , the direct state equation and the adjoint state equation would have the same left-hand side. In the goal of never inverting a matrix, which is a very slow process numerically, a LU decomposition can be used instead to solve the state equation, in operations for the decomposition and operations for the resolution. That same decomposition can then be used to solve the adjoint state equation in only operations since the matrices are the same.

See also

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References

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  1. ^ Pollini, Nicolò; Lavan, Oren; Amir, Oded (2018-06-01). "Adjoint sensitivity analysis and optimization of hysteretic dynamic systems with nonlinear viscous dampers". Structural and Multidisciplinary Optimization. 57 (6): 2273–2289. doi:10.1007/s00158-017-1858-2. ISSN 1615-1488. S2CID 125712091.
  2. ^ Ricky T. Q. Chen, Yulia Rubanova, Jesse Bettencourt, David Duvenaud Neural Ordinary Differential Equations Available online
  3. ^ Plessix, R-E. "A review of the adjoint-state method for computing the gradient of a functional with geophysical applications." Geophysical Journal International, 2006, 167(2): 495-503. free access on GJI website
  4. ^ McNamara, Antoine; Treuille, Adrien; Popović, Zoran; Stam, Jos (August 2004). "Fluid control using the adjoint method" (PDF). ACM Transactions on Graphics. 23 (3): 449–456. doi:10.1145/1015706.1015744. Archived (PDF) from the original on 29 January 2022. Retrieved 28 October 2022.
  5. ^ Lundvall, Johan (2007). "Data Assimilation in Fluid Dynamics using Adjoint Optimization" (PDF). Sweden: Linköping University of Technology. Archived (PDF) from the original on 9 October 2022. Retrieved 28 October 2022.
  6. ^ Cea, Jean (1986). "Conception optimale ou identification de formes, calcul rapide de la dérivée directionnelle de la fonction coût". ESAIM: Mathematical Modelling and Numerical Analysis - Modélisation Mathématique et Analyse Numérique (in French). 20 (3): 371–402. doi:10.1051/m2an/1986200303711.
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  • A well written explanation by Errico: What is an adjoint Model?
  • Another well written explanation with worked examples, written by Bradley [1]
  • More technical explanation: A review of the adjoint-state method for computing the gradient of a functional with geophysical applications
  • MIT course [2]
  • MIT notes [3]