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The Inverse Problem of Velocity Reconstruction from Flow-Induced Magnetic Fields: Stability and Uniqueness

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Abstract

The reconstruction of velocity fields from flow-induced magnetic measurements is a fundamental inverse problem in magnetohydrodynamics, with broad applications in geophysics, astrophysics, and metallurgy. To address the nonlinearity of the governing equations, the magnetic induction equation is linearized around a known, space-dependent background magnetic field. This reveals a coupled parabolic–hyperbolic system in which magnetic diffusion interacts with velocity advection along the background field lines. By decoupling these mechanisms into a two-stage framework, sufficient conditions are established for both the uniqueness and stability of the velocity recovery. The main result proves that the non-uniqueness arising from unobservable velocity perturbations parallel to the background field is eliminated when the velocity trace on the inflow boundary is prescribed alongside magnetic observations. The analysis yields global uniqueness and a quantitative stability estimate of hybrid type: a Lipschitz contribution from the inflow trace combined with a weaker modulus from the parabolic observation, reflecting the mixed parabolic–hyperbolic structure of the problem. These theoretical findings are validated through three-dimensional numerical simulations that demonstrate the robustness of the decoupled reconstruction approach under noisy conditions.

Introduction

The motion of a conducting fluid through a magnetic field induces electric currents, which in turn generate secondary magnetic fields. This magneto-induction mechanism is described by the magnetic induction equation and underlies a wide range of phenomena in geophysics, astrophysics, space physics, and industrial applications; see, for example, [1, 2, 3, 4, 5]. In many of these settings, direct measurements of the fluid velocity are difficult or impractical because of the inaccessibility of the flow, the opacity of the medium, or the extreme physical conditions. Magnetic measurements therefore provide a potentially valuable indirect means of recovering the underlying fluid motion. This motivates the inverse problem of reconstructing a velocity field from magnetic field observations, which has received considerable attention in the literature; see, e.g., [6, 7, 8, 9].

The evolution of electromagnetic fields in a conducting medium is governed by Maxwell’s equations. Under the magnetohydrodynamic approximation, neglecting displacement currents and free-charge accumulation, and using Ohm’s law

J=σ(E+v×B),\mathbf J = \sigma(\mathbf E + \mathbf v \times\mathbf B),

one obtains the magnetic induction equation

∂tB−ηΔB=∇×(v×B),∇⋅B=0,η=1μ0σ,(1)\partial_t\mathbf B - \eta\Delta\mathbf B = \nabla\times(\mathbf v \times\mathbf B), \qquad\nabla\cdot\mathbf B = 0, \qquad\eta= \frac{1}{\mu_0\sigma}, \tag*{(1)}

where v\mathbf v denotes the fluid velocity, B\mathbf B the magnetic induction, σ>0\sigma> 0 the electrical conductivity, μ0>0\mu_0 > 0 the magnetic permeability, and η>0\eta> 0 the magnetic diffusivity; see [6, 7]. Throughout this work, we set η=1\eta= 1 by nondimensionalization.

We consider a connected bounded domain Ω⊂R3\Omega\subset\mathbb{R}^3 with sufficiently smooth boundary ∂Ω\partial\Omega, and a fixed time T>0T > 0. The magnetic field is subject to the boundary conditions

B⋅n=g1,n×(∇×B)=g2on (0,T)×∂Ω,(2)\mathbf B \cdot\mathbf n = g_1, \qquad\mathbf n \times(\nabla\times\mathbf B) = g_2 \quad\text{on } (0,T) \times\partial\Omega, \tag*{(2)}

where n\mathbf n denotes the outward unit normal, g1g_1 is a scalar-valued boundary datum, and g2g_2 is a tangential vector-valued datum. The first condition prescribes the normal component of the magnetic field and hence the magnetic flux through the boundary. The second prescribes the tangential component of its curl. Since

∇×B=μ0J,\nabla\times\mathbf B = \mu_0\mathbf J,

the latter condition is equivalent to prescribing the tangential component of the current density, up to the factor μ0\mu_{0}. These boundary conditions are natural in the analysis of magnetic diffusion operators and their associated boundary-value problems; see, for example, [10, 11]. In the Hodge-theoretic formulation, the homogeneous conditions

B⋅n=0,n×(∇×B)=0on ∂Ω\mathbf{B} \cdot\mathbf{n} = 0,\qquad\mathbf{n} \times(\nabla\times\mathbf{B}) = 0\quad\text{on }\partial\Omega

are the magnetic (absolute) boundary conditions for the Hodge Laplacian on divergence-free vector fields. Their physical interpretation depends on the electromagnetic model and the assumptions imposed on the wall; they should therefore not be identified indiscriminately with every formulation of a perfectly conducting boundary. For the latter distinction and the associated MHD boundary-value formulations, see [4, 12]. The boundary data must also satisfy the compatibility conditions imposed by the divergence constraint and the evolution equation.

The inverse problem studied here is to determine whether the velocity field v\mathbf{v} can be uniquely recovered from observations of the magnetic field. We represent the available measurements by an observation operator L\mathcal{L} acting on B\mathbf{B}, so that the data take the form

L(B).\mathcal{L}(\mathbf{B}).

Depending on the observation configuration, L\mathcal{L} may represent measurements over a subregion of the domain, over a restricted time interval, or other partial observations specified in the subsequent analysis. The central questions are whether the observations determine the velocity uniquely, which compatibility conditions are necessary for reconstruction, and how the geometric and boundary assumptions influence identifiability.

Velocity reconstruction from electromagnetic measurements has been investigated through analytical, numerical, and experimental approaches. The reconstruction problem using magnetic-field and electric-potential measurements was formulated in [6]. Non-uniqueness of the reconstruction problem was subsequently analyzed in [7], where a regularization based on minimizing the kinetic energy of the velocity field was proposed as a selection criterion. A contactless method for velocity reconstruction in electrically conducting fluids was developed in [13], and theoretical and experimental aspects of inverse problems in magnetohydrodynamics were further investigated in [14]. A finite-element-based Bayesian approach to reconstructing the longitudinal velocity component in electromagnetic flow tomography was proposed in [8], but no uniqueness or stability results are proved there. It is worth mentioning that recently, in [15], a Carleman estimate was established for the full MHD system; however, that work recovers a source term that is independent of the magnetic field or the velocity of the fluid.

More recently, [9] established uniqueness criteria for the linearized induction equation in whole-space and periodic settings with constant background magnetic field.

Contribution

We prove stability and uniqueness for velocity reconstruction in a bounded domain from partial parabolic observations of the magnetic field. Magnetic observations alone are not sufficient for uniqueness; prescribing the velocity on the inflow boundary together with the magnetic boundary conditions restores uniqueness under suitable conditions on the space-dependent background field and bounded-domain transport geometry. The problem has a hybrid parabolic-hyperbolic structure: magnetic diffusion is parabolic, while velocity transport along the background field is hyperbolic. This motivates a two-stage reconstruction and yields a hybrid stability estimate combining a Lipschitz contribution from the inflow trace with a weaker modulus from the parabolic observation. Unlike previous work in unbounded or periodic settings with constant background fields, we allow a space-dependent background field.

Organization of the paper

This paper is organized as follows. In Section 2, we present the linearized model around a background magnetic field, the existence result for the forward problem, and the statement of the inverse problem. In Section 3, we present the geometric and functional tools needed to announce and prove the main results for the inverse problem. In Section 4, we establish a well-posedness result for a curl–div system that is required in the proof of the main results. In Section 5, we state the main results for the inverse problem. In Section 6, we prove the main results, and in Section 7, we present the numerical validation of both the stability and uniqueness results.

The model

The nonlinearity of the induction equation makes direct analysis of the associated inverse problem difficult. Following the linearization strategy commonly used in inverse problems for magnetohydrodynamics [6, 7], we decompose the magnetic field as

B(t,x)=F(x)+b(t,x),(3)B(t,x)=F(x)+b(t,x), \tag*{(3)}

where FF is a known, time-independent background magnetic field and bb is the magnetic perturbation. We assume that the background field satisfies

F∈[C2(Ω‾)]3,∇⋅F=0,in Ω.(4)F\in[C^{2}(\overline{\Omega})]^{3}, \qquad\nabla\cdot F=0, \qquad\text{in }\Omega. \tag*{(4)}

Since BB and FF are divergence-free, the perturbation is also divergence-free:

∇⋅b=∇⋅B−∇⋅F=0.\nabla\cdot b=\nabla\cdot B-\nabla\cdot F=0.

Recall from the introduction that the total magnetic field satisfies the boundary conditions

B⋅n=g1,n×(∇×B)=g2,on (0,T)×∂Ω.(5)B\cdot n=g_{1}, \qquad n\times(\nabla\times B)=g_{2}, \qquad\text{on }(0,T)\times\partial\Omega. \tag*{(5)}

Because the decomposition (3) separates the known background field from the unknown perturbation, we impose the boundary condition on the total field BB in such a way that the prescribed background field FF satisfies the same boundary data

g1:=F⋅n,g2:=n×(∇×F).(6)g_{1}:=F\cdot n, \qquad g_{2}:=n\times(\nabla\times F). \tag*{(6)}

Consequently the perturbation satisfies homogeneous absolute boundary conditions

b⋅n=0,n×(∇×b)=0,on (0,T)×∂Ω.b\cdot n=0, \qquad n\times(\nabla\times b)=0, \qquad\text{on }(0,T)\times\partial\Omega.

This choice is natural: the background field already satisfies the perfectly-conducting-wall or symmetry boundary conditions, and the perturbation is the difference between the total field and this known background. Hence the boundary data of the total field are precisely those of the background, so the perturbation inherits boundary data. Physically, the linearized perturbation does not alter the normal magnetic flux or the tangential current density at the boundary.

Substituting (3) into the induction equation, using that FF is time-independent and satisfies (4), and dropping the bilinear term ∇×(v×b)\nabla\times(v\times b), we obtain the linearized system

∂tb−Δb=ΔF+∇×(v×F),in (0,T)×Ω,∇⋅b=0,in (0,T)×Ω,b⋅n=0,n×(∇×b)=0,on (0,T)×∂Ω,b∣t=0=b0,in Ω,(7)\begin{aligned} \partial_t b-\Delta b&=\Delta F+\nabla\times(v\times F), &&\text{in }(0,T)\times\Omega,\\ \nabla\cdot b&=0, &&\text{in }(0,T)\times\Omega,\\ b\cdot n&=0,\qquad n\times(\nabla\times b)=0, &&\text{on }(0,T)\times\partial\Omega,\\ b|_{t=0}&=b_0, &&\text{in }\Omega, \tag*{(7)} \end{aligned}

where b0=B0−Fb_0=B_0-F.

The Hodge Laplacian

It has been noted in several works, see, for example, [16, 17, 18], that, in Ω⊂R3\Omega\subset\mathbb{R}^{3}, the Laplace operator acting on vector fields,

−ΔHu:=−Δu=∇×(∇×u)−∇(∇⋅u),(8)-\Delta_Hu:=-\Delta u=\nabla\times(\nabla\times u)-\nabla(\nabla\cdot u), \tag*{(8)}

with the boundary conditions

u⋅n=0,n×(∇×u)=0on ∂Ω,(9)u\cdot n=0,\qquad n\times(\nabla\times u)=0 \qquad\text{on }\partial\Omega, \tag*{(9)}

is called the Hodge Laplacian.

We introduce the solenoidal Hilbert space

H:={u∈[L2(Ω)]3:∇⋅u=0 in Ω,u⋅n=0 on ∂Ω}.(10)\mathbb{H} := \left\{ u \in[L^{2}(\Omega)]^{3} : \nabla\cdot u = 0 \text{ in } \Omega,\quad u \cdot n = 0 \text{ on } \partial\Omega\right\}. \tag*{(10)}

Let

P:[L2(Ω)]3⟶H\mathbb{P} : [L^{2}(\Omega)]^{3} \longrightarrow\mathbb{H}

denote the Helmholtz–Leray orthogonal projection.

A key property of the Hodge realization is its compatibility with P\mathbb{P} in R3\mathbb{R}^{3}. More precisely, for uu in the domain of the Hodge Laplacian,

Pu∈D(ΔH),−PΔu=−ΔHPu=∇×(∇×u),(11)\mathbb{P}u \in D(\Delta_{\mathrm{H}}), \qquad-\mathbb{P}\Delta u = -\Delta_{\mathrm{H}}\mathbb{P}u = \nabla\times(\nabla\times u), \tag*{(11)}

and Pu\mathbb{P}u satisfies the same boundary conditions,

(Pu)⋅n=0,n×(∇×Pu)=0on ∂Ω.(12)(\mathbb{P}u) \cdot n = 0, \qquad n \times(\nabla\times\mathbb{P}u) = 0 \qquad\text{on } \partial\Omega. \tag*{(12)}

Thus, the compatibility is a property of the operator realizations and their domains, rather than an unrestricted commutation relation PΔ=ΔP\mathbb{P}\Delta= \Delta\mathbb{P} on [L2(Ω)]3[L^{2}(\Omega)]^{3}; see [18].

We consider the realization of the Hodge Laplacian on H\mathbb{H} with domain

D(ΔH):={u∈H:Δu∈[L2(Ω)]3,n×(∇×u)=0 on ∂Ω}.(13)D(\Delta_{\mathrm{H}}) := \left\{ u \in\mathbb{H} : \Delta u \in[L^{2}(\Omega)]^{3},\quad n \times(\nabla\times u) = 0 \text{ on } \partial\Omega\right\}. \tag*{(13)}

Since ∇⋅u=0\nabla\cdot u = 0 for every u∈D(ΔH)u \in D(\Delta_{\mathrm{H}}), we have

−ΔHu=−Δu=∇×(∇×u).(14)-\Delta_{\mathrm{H}}u = -\Delta u = \nabla\times(\nabla\times u). \tag*{(14)}

Hence the divergence-free constraint and the boundary conditions are incorporated directly into the Hodge–Laplacian realization. The evolution problem can therefore be formulated directly on H\mathbb{H}, without introducing an additional pressure term or an explicit Helmholtz projection.

Well-posedness

For the linearized induction system (7), we set

h(t)=ΔF+∇×(v(t)×F),t∈(0,T).(15)h(t) = \Delta F + \nabla\times(v(t) \times F), \qquad t \in(0,T). \tag*{(15)}

The Hodge–Laplacian realization ΔH\Delta_{\mathrm{H}} on H\mathbb{H} with absolute boundary conditions is self-adjoint and nonnegative. Consequently, ΔH\Delta_{\mathrm{H}} is maximal dissipative and generates an analytic C0C_{0}-semigroup on H\mathbb{H}; see, for example, [19 Theorem 7.1]. We have the following result [20 Theorem 3.2]

Theorem 2.1. Let T>0T > 0. Assume that Ω\Omega is sufficiently smooth and let

h∈L2(0,T;H),b0∈D(ΔH12).h \in L^{2}(0,T;\mathbb{H}), \qquad b_{0} \in D(\Delta_{\mathrm{H}}^{\frac{1}{2}}).

Then the problem (7) admits a unique strong solution

b∈L2([0,T];D(ΔH))∩H1(0,T;H).b \in L^{2}([0,T];D(\Delta_{\mathrm{H}})) \cap H^{1}(0,T;\mathbb{H}).

We therefore define the state space

Y:={b∈L2([0,T];D(ΔH))∩H1(0,T;H)}.(16)\mathbb{Y} := \left\{ b \in L^{2}([0,T];D(\Delta_{\mathrm{H}})) \cap H^{1}(0,T;\mathbb{H}) \right\}. \tag*{(16)}

Remark 2.2. By definition of the source term hh in (15), the source term is required to belong to H\mathbb{H}. Since

∇⋅h(t)=∇⋅(ΔF+∇×(v(t)×F))=(Δ(∇⋅F)+∇⋅(∇×(v(t)×F)))=0,a.e. on (0,T),\nabla\cdot h(t) = \nabla\cdot\left(\Delta F + \nabla\times(v(t) \times F)\right) = \left(\Delta(\nabla\cdot F) + \nabla\cdot\left(\nabla\times(v(t) \times F)\right)\right) = 0,\qquad\text{a.e. on } (0,T),

holds identically, the remaining condition h⋅n=0h \cdot n = 0 on ∂Ω\partial\Omega gives precisely the boundary condition

n⋅∇×(v(t)×F)=−n⋅ΔFon ∂Ω for a.e. on (0,T).n \cdot\nabla\times(v(t) \times F) = -n \cdot\Delta F \qquad\text{on } \partial\Omega\text{ for a.e. on } (0,T).

Statement of the inverse problem

We can now formulate the main inverse problem. Assume that vv can be written in a separated form

v(t,x)=α(t)u(x),v(t,x)=\alpha(t)u(x),

where α∈L2(0,T)\alpha\in L^{2}(0,T) is not zero on (0,T)(0,T) function that is supposed to be known.

Problem 2.3 (Inverse Problem: Recovering vv from observations L(y)\mathcal{L}(y)). Determine the spatial velocity vector field uu in Ω\Omega from the measurements modeled by the observation operator L(y)\mathcal{L}(y), supplemented by additional boundary measurements on uu as required for well-posedness.

First, observe that uniqueness of source recovery in Problem 2.3 cannot hold for arbitrary vv so that z∈Hz \in\mathbb{H} defined in 15. Indeed, the linear operator

u⟼∇×(u×F),(17)u \longmapsto\nabla\times(u \times F), \tag*{(17)}

possesses a nontrivial kernel. Specifically, let c(x)c(x) be a sufficiently smooth scalar function satisfying the transport equation ∇⋅(cF)=0\nabla\cdot(cF)=0, i.e.,

References

  1. [1]Peter Alan Davidson. An introduction to magnetohydrodynamics, volume 1. Cambridge university press Cambridge, 2001.
  2. [2]Johan P Goedbloed, Rony Keppens, and Stefaan Poedts. Magnetohydrodynamics of laboratory and astrophysical plasmas. Cambridge University Press; Cambridge, 2019.DOI
  3. [3]Donald A Gurnett and Amitava Bhattacharjee. Introduction to plasma physics: With space, laboratory and astrophysical applications. Cambridge University Press, 2017.DOI
  4. [4]Jean-Frédéric Gerbeau, Claude Le Bris, and Tony Lelièvre. Mathematical methods for the magnetohydrodynamics of liquid metals. Numerical Mathematics and Scie, 2006.DOI
  5. [5]Michael S Zhdanov. Geophysical inverse theory and regularization problems, volume 36. Elsevier, 2002.
  6. [6]Frank Stefani and Gunter Gerbeth. Velocity reconstruction in conducting fluids from magnetic field and electric potential measurements. Inverse Problems, 15(3):771–786, 1999.DOI
  7. [7]Frank Stefani and Gunter Gerbeth. A non-uniqueness theorem for the inverse problem of magnetic flow tomography. Inverse Problems, 16(4):1051–1059, 2000.
  8. [8]Ossi Lehtikangas, Kimmo Karhunen, and Marko Vauhkonen. Reconstruction of velocity fields in electromagnetic flow tomography. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 374(2070):20150334, 2016.DOI
  9. [9]Yacine Mokhtari, Christina Frederick, Yunan Yang, and Bjorn Engquist. Velocity reconstruction from flow-induced magnetic fields. arXiv preprint arXiv:2602.9297, 2026.arxiv.org/abs/2602.22097
  10. [10]Günter Schwarz. Hodge Decomposition: A Method for Solving Boundary Value Problems, volume 1607 of Lecture Notes in Mathematics. Springer, Berlin, 1995.DOI
  11. [11]Douglas N. Arnold, Richard S. Falk, and Ragnar Winther. Finite element exterior calculus, homological techniques, and applications. Acta Numerica, 15:1–155, 2006.DOI
  12. [12]Jeffrey P. Freidberg. Ideal Magnetohydrodynamics. Plenum Press, New York, 1987.DOI
  13. [13]Frank Stefani and Gunter Gerbeth. A contactless method for velocity reconstruction in electrically conducting fluids. Measurement Science and Technology, 11(6):758–765, 2000.DOI
  14. [14]Frank Stefani, Thomas Gundrum, Gunter Gerbeth, Uwe Günther, and Mingtian Xu. Inverse problems in magnetohydrodynamics: theoretical and experimental aspects. Inverse Problems in Science and Engineering, 14(4):411–422, 2006.DOI
  15. [15]Xin Huang and Masahiro Yamamoto. Carleman estimates for a linearized magnetohydrodynamic system and applications to inverse problems. Inverse Problems, 38(3):035005, 2022.arxiv.org/abs/1806.07576
  16. [16]G. Gerbeth, F. Stefani, and H. Vitense. Magnetic flow tomography. Flow Measurement and Instrumentation, 16(2-3):117–125, 2005.
  17. [17]Sylvie Monniaux and Zongwei Shen. Stokes problems in irregular domains with various boundary conditions. Handbook of Mathematical Analysis in Mechanics of Viscous Fluids, 59:1–42, 2016.
  18. [18]Anatole Gaudin. Hodge decompositions and maximal regularities for hodge laplacians in homogeneous function spaces on the half-space. Annales Henri Lebesgue, 7:1457–1534, 2024.arxiv.org/abs/2303.04026
  19. [19]Marius Mitrea and Sylvie Monniaux. On the analyticity of the semigroup generated by the stokes operator with neumann-type boundary conditions on lipschitz subdomains of riemannian manifolds. Transactions of the American Mathematical Society, 361(6):3125–3157, 2009.DOI
  20. [20]Enrico Magenes and Jacques-Louis Lions. Non-homogeneous boundary value problems and applications. Springer, 1972.
  21. [21]Pascal Azérad and Jérôme Pousin. Inégalité de poincaré courbe pour le traitement variationnel de l’équation de transport. Comptes rendus de l’Académie des sciences. Série 1, Mathématique, 322(8):721–727, 1996.
  22. [22]Julia Brunken, Kathrin Smetana, and Karsten Urban. (parametrized) first order transport equations: Realization of optimally stable petrov–galerkin methods. SIAM journal on scientific computing, 41(1):A592–A621, 2019.DOI
  23. [23]Masaki Imagawa and Daisuke Kawagoe. A revisit on well-posedness of a boundary value problem of a stationary advection equation without the separation condition. Journal of Mathematical Analysis and Applications, 551(2):129695, 2025.DOI
  24. [24]Rodrigo Duarte. An introduction to pointwise sparse domination. Expositions Mathematicae, 42(6):125605, 2024.arxiv.org/abs/2407.05911
  25. [25]Ana Alonso Rodriguez, Enrico Bertolazzi, Alberto Valli, et al. The curl-div system: theory and finite element approximation. Radon Series on Computational and Applied Mathematics, 24:1–43, 2019.
  26. [26]Yavar Kian, Diomba Sambou, and Eric Soccorsi. Logarithmic stability inequality in an inverse source problem for the heat equation on a waveguide. Applicable Analysis, 99(13):2210–2228, 2020.
  27. [27]Masahiro Yamamoto. Carleman estimates for parabolic equations and applications. Inverse Problems, 25(12):123013, 2009.DOI
  28. [28]Kenichi Sakamoto and Masahiro Yamamoto. Inverse heat source problem from time distributing overdetermination. Applicable Analysis, 88(5):735–748, 2009.DOI
  29. [29]Yavar Kian, Diomba Sambou, and Eric Soccorsi. Logarithmic stability inequality in an inverse source problem for the heat equation on a waveguide. Applicable Analysis, 99(13):2210–2228, 2020.
  30. [30]XINCHI Huang, O Yu Imanuvilov, and M Yamamoto. Stability for inverse source problems by carleman estimates. Inverse Problems, 36(12):125006, 2020.DOI
  31. [31]Oleg Yu Imanuvilov and Masahiro Yamamoto. Stability and uniqueness for inverse problems for parabolic equations with final overdetermination. Inverse Problems, 2026.
  32. [32]Masahiro Yamamoto. Carleman estimates for parabolic equations and applications to inverse problems. Inverse Problems, 25(12):123013, 2009.
  33. [33]Guang Lin, Zecheng Zhang, and Zhidong Zhang. Theoretical and numerical studies of inverse source problem for the linear parabolic equation with sparse boundary measurements. Inverse Problems, 38(12):125007, 2022.DOI
  34. [34]Francesco Ferrarresso and Luigi Provenzano. A note on the maxwell’s eigenvalues on thin sets. Proceedings of the Royal Society of Edinburgh Section A: Mathematics, pages 1–27, 2026.
  35. [35]Jean-Claude Saut and Bruno Scheurer. Sur l’unicité du problème de cauchy et le prolongement unique pour des équations elliptiques à coefficients non localement bornés. Journal of Differential Equations, 43(1):28–43, 1982.DOI
  36. [36]Augusto Cesar Galeão and Eduardo Gomes Dutra Do Carmo. A consistent approximate upwind petrov-galerkin method for convection-dominated problems. Computer Methods in Applied Mechanics and Engineering, 68(1):83–95, 1988.DOI
  37. [37]J-L Guermond and Luigi Quartapelle. On the approximation of the unsteady navier–stokes equations by finite element projection methods. Numerische mathematik, 80(2):207–238, 1998.DOI
  38. [38]Roger Temam. Navier-stokes equations: Theory and numerical analysis(book). Amsterdam, North-Holland Publishing Co.(Studies in Mathematics and Its Applications, 2:510, 1977.DOI
  39. [39]Michel C Delfour and J-P Zolésio. Shapes and geometries: metrics, analysis, differential calculus, and optimization. SIAM, 2011.
  40. [40]Andrew Majda and Xiaoming Wang. Nonlinear dynamics and statistical theories for basic geophysical flows. Cambridge University Press, 2006.DOI

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