Abstract
In this paper, we show a mathematical justification of the data assimilation of nudging type in \(L^p\)-\(L^q\) maximal regularity settings. We prove that the approximate solution of the primitive equations constructed by the data assimilation converges to the true solution with exponential order in the Besov space \(B^{2/q}_{q,p}(\Omega )\) for \(1/p + 1/q \le 1\) on the periodic layer domain \(\Omega = \mathbb {T}^2 \times (-h, 0)\).
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References
Cao, C., Titi, E.S.: Global well-posedness of the three-dimensional viscous primitive equations of large scale ocean and atmosphere dynamics. Ann. Math. 166(1), 245–267 (2007)
Guillén-González, F., Masmoudi, N., Rodríguez-Bellido, M.A.: Anisotropic estimates and strong solutions of the primitive equations. Differ. Integral Equ. 14(1), 1381–1408 (2001)
Kukavica, I., Ziane, M.: On the regularity of the primitive equations of the ocean. Nonlinearity 20(12), 2739–2753 (2007). https://doi.org/10.1088/0951-7715/20/12/001
Hieber, M., Kashiwabara, T.: Global strong well-posedness of the three dimensional primitive equations in \(l^p\)-spaces. Arch. Rational Mech. Anal. 1077-1115 (2016)
Giga, Y., Gries, M., Hieber, M., Hussein, A., Kashiwabara, T.: Analyticity of solutions to the primitive equations. Math. Nachr. 293(2), 284–304 (2020)
Azouani, A., Olson, E., Titi, E.S.: Continuous data assimilation using general interpolant observables. J. Nonlinear Sci. 24(2), 277–304 (2014)
Albanez, D.A.F., Nussenzveig, L.H.J., Titi, E.S.: Continuous data assimilation for the three-dimensional Navier-Stokes-\(\alpha \) model. Asymptot. Anal. Asymptotic Anal. 97(1–2), 139–164 (2016)
Pei, Y.: Continuous data assimilation for the 3D primitive equations of the ocean. Commun. Pure Appl. Anal. 18(2), 643–661 (2019)
Prüss, J., Simonett, G.: Moving Interfaces and Quasi linear Parabolic Evolution Equations, Monographs in Mathematics, 105, Birkhäuser, Springer, Cham, xix+609 (2016)
Hieber, M., Hussein, A., Kashiwabara, T.: Global strong \(L^p\) well-posedness of the 3D primitive equations with heat and salinity diffusion. J. Differ. Equ. 261, 6950–6981 (2016)
Engel, K.J., Nagel, R.: One-Parameter Semigroups for Linear Evolution Equations. Graduate Texts in Mathematics, vol. 194, Springer, New York (2000)
Kunstmann, P.C., Weis, L.: Maximal \(L_p\)-regularity for parabolic equations. Fourier multiplier theorems and \(H^\infty \)-functional calculus, Functional analytic methods for evolution equations, Lecture Notes in Math. 65–311, 2004. Springer, Berlin (1855)
Lasiecka, I., Wilke, M.: Maximal regularity and global existence of solutions to a quasilinear thermoelastic plate system. Discrete Contin. Dyn. Syst. 33(11–12), 5189–5202 (2013)
Prüss, J., Wilke, M.: Addendum to the paper “On quasilinear parabolic evolution equations in weighted Lp-spaces II’’, MR 3250797. J. Evol. Equ. 17(4), 1381–1388 (2017)
Prüss, J., Simonett, G.: Maximal regularity for evolution equations in weighted \(L^p\)-spaces. Arch. Math. (Basel) 82(5), 415–431 (2004)
Sohr, H.: The Navier–Stokes equations, Birkhäuser Advanced Texts: Basler Lehrbücher., Birkhäuser Advanced Texts: Basel Textbooks, Birkhäuser Verlag, Basel, x+367 (2001)
Acknowledgements
The author would like to thank Prof. Takahito Kashiwabara of the University of Tokyo and the members of Data Assimilation Research Team in RIKEN for helpful discussions and comments for this research. The author would also like to thank the anonymous referees for their careful reading and valuable comments. The author was partly supported by RIKEN Pioneering Project “Prediction for Science” and JSPS Grant-in-Aid for Young Scientists (No. 22K13948).
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Appendices
Appendix A: \(L^2_t H^3_x\) Estimate for the Solution to the Primitive Equations
In this appendix, we show the \(L^2_t H^3_x\) a priori estimate
for all \(t>0\) if \(f \in L^2_t H^1_x ((0, \infty ) \times \Omega )\). Although Giga et al. [5] proved \(L^\infty _t H^2_x\)-estimates and the lower order estimates, they did not show \(L^2_t H^3_x\)-a priori estimates. Let \(\psi \in H^1_t L^2_{\overline{\sigma }, x}((0, \infty ) \times \Omega ) \cap L^2_t H^2_{\sigma , x} ((0, \infty )\times \Omega )\) be a solution of the hydrostatic Stokes equations
with boundary conditions (2). Note that we have the local well-posedness for the primitive equation from [5]. The local solution v is embedded into \(C(0,T_0; H^2_{\overline{\sigma }}(\Omega )^2)\) for some small \(T_0>0\). A priori estimates are used to extend the local solution globally. Therefore, without loss of generality, we can assume (A3). Assume that \(\psi \) satisfies
for all \(t > 0\). We denote \(D^h_j \psi (x) = (\psi (x + h e_j) - \psi (x))/h\) for \(j = 1, 2, 3\) and \(h > 0\). Then \(D^h_j \psi \) satisfies (A2) with an external force \(D^h_j g\) and initial data \(D^h_j \psi _0\). We find that
Since the right-hand side is uniform with respect to \(h>0\), we take a \(\limsup \) to get
The reader is referred to Section 3.1.5 and 4.2.7 of the book [16] by Sohr. Therefore, we see that
The boundedness of the first term was shown in [5]. The Sobolev inequalities and the interpolation inequalities yield
In the same way, we see that
Using the Young inequality, we obtain (A1).
Appendix B: Remarks for Semi-Group Based Approach
The main result of this paper is a mathematical justification of the DA in \(L^p\)-\(L^q\) based maximal regularity settings. However, the analytic semi-group based approach as used by Hieber and Kashiwabara [4] can be applicable. As in [4], we set
We also set \(X_q = \left\{ \varphi \in H^{2/q, q}_{\overline{\sigma }}(\Omega )^2 \, ; \, \varphi \vert _{\Gamma _b = 0} \right\} \). Using the same kind of method based on analytic semi-group theory as [4, 10], we can show
Theorem B.1
Let \(1< p < \infty \) and \(0< \alpha < 1\). Let \(v_0 \in X_q\) be an initial datum. Let \(f \in H^1_{loc} (0, \infty ; L^q(\Omega )^2)\) satisfy
for some constant \(\gamma _0 > 0\). Assume that \(v \in C(0, \infty ; X_q)\) is the solution to (1), which is obtained by Hieber et al. [10] with zero temperature and salinity, satisfying
for some constant \(C_0>0\) and \(\gamma _1 < \gamma _0\). Then there exist \(\mu _0, \delta _0>0\) such that if \(\mu \ge \mu _0\) and \(\delta \le \delta _0\), there exists a unique solution \(V \in C(0, \infty ;X_{1/q, p, q})\) to (4) such that
for some constants \(\gamma _0< \mu _*< \gamma _1\) and \(C>0\). Moreover, V satisfies
Remark 5
The assumption on the regularity for the initial data in Theorem B.1 is stronger than Theorem 1 since \(H^{2/q, q}(\Omega ) \hookrightarrow B^{2/q}_{q, p}(\Omega )\) for \(p > 2\).
We show the local well-posedness in \(C(0,T_*; L^q(\Omega )^2)\)-framework with the analytic semi-group \(e^{- t \tilde{A}_{\mu , q}}\) and the Fujita-Kato principle. The mild solution is given by
Lemma B.2
Let \(T>0\), \(0 \le \tilde{\mu } \le \mu _*\), and \(V_0, v_0 \in H^{2/q, q}(\Omega )^2\). Let \(F \in C(0, T; L^q(\Omega )^2)\) satisfy
for some constant \(\gamma _0 > 0\). Let v satisfy the same assumptions as Theorem B.1. Then, there exists \(T_0 > 0\) such that if \(T \le T_0\), the integral Eq. (B6) admit the unique solution \(V \in C(0,T; H^{2/q, q}_{\overline{\sigma }}(\Omega )^2)\) such that
Moreover, there exists \(\varepsilon _0>0\) such that if
it can be taken \(T = \infty \).
Proof
The proof is based on Proposition 5.2 in [4]. We prove that
is a contraction mapping if T is small or \(v_0\) and F are small. We find from Proposition 6 that
We also find from Propositions 4 and 6 that
Similarly we have
Since \(e^{- t \tilde{A}_{\mu , q}}\) is analytic for t, we can observe that
Moreover, since \(D(\tilde{A}_{\mu , q})\) is densely embedded into \(H^{s, q}(\Omega )^2\) for \(s \in [0, 2)\), we see that
We find from Proposition 4 that
and
Combining the above estimates, we obtain the quadratic inequality
We assume that \(\Vert v \Vert _{\widetilde{{\mathcal {S}}}_{\tilde{\mu }, q, T}} \le \frac{1}{2C_1}\) is sufficiently small.
The quadratic estimate implies that, if we take \(T>0\) so small or \(\Vert V_0 \Vert _{H^{2/q, q}(\Omega )^2}\) and \(\sup _{0< s < t} e^{\tilde{\mu }s} s^{1 - \frac{1}{q}} \Vert F (s) \Vert _{L^q(\Omega )^2}\) so small that
then
We find that \(N (\cdot , v)\) is a self-mapping on \(\left\{ V \in \widetilde{{\mathcal {S}}}_{\tilde{\mu }, q, T} \, ; \, \Vert V \Vert _{\widetilde{{\mathcal {S}}}_{\tilde{\mu }, q, T}} < R_* \right\} \). We take R and \(\Vert v \Vert _{\widetilde{{\mathcal {S}}}_{\tilde{\mu }, q, T}}\) sufficiently sufficiently small again. Then \(N (\cdot , v)\) is a contraction mapping. Banach’s fixed point theorem implies that there exists a unique mild solution V to (B6) in \(\widetilde{{\mathcal {S}}}_{\tilde{\mu }, q, T}\). The estimate (B8) implies that \(N (V, v) \in {\mathcal {S}}_{\tilde{\mu }, q, T}\), so \(V \in {\mathcal {S}}_{\tilde{\mu }, q, T}\). \(\square \)
We improve the regularity of the solution V to (B6) for regular F.
Proposition B.3
Let \(0 \le \tilde{\mu } \le \mu _*\), \(T > 0\), and \(1< q < \infty \). Let \(f \in C^\alpha (0, T; L^q(\Omega )^2)\) such that
for \(0< \alpha < 1\) and \(\beta , \gamma > 0\). Set \(\phi \) such that
Then \(\phi \) satisfies
and
for some constant \(C > 0\). In particular, if \(\mu _*\le \gamma \), it follows that
Proof
Since the proof is quite parallel as Lemma 5.6 in [4], we omit the details here. \(\square \)
Proof of Theorem B.1
By Proposition 7 for \(p = q = 2\), we first deduce that there exists an \(L^2\)-solution \(V \in C(0, \infty ; H^1(\Omega )^2) \cap C(0, T; D(\tilde{A}_{2, \mu }))\) such that
for some constant \(C>0\). Moreover, we repeat the same argument as in the proof of Theorem 1 for \(p = q = 2\) to see that there exist small \(\varepsilon > 0\) and large \(T_*> 0\) such that \(\Vert V (T_*) \Vert _{D(\tilde{A}_{2, \mu })} \le \varepsilon \). Applying Lemma B.2, we have \(V \in {\mathcal {S}}_{q, {\mu _*}, \infty }\). By the assumptions for f and Proposition 6, we see that
as \(t \rightarrow \infty \). We use Proposition B.3 to conclude that
Note that if we take \(\mu \) sufficiently large, the decay rate \(e^{- \mu _*t /2}\) is larger than that of \(\Vert \partial _t v (t) \Vert _{L^2(\Omega )^2} + \Vert v(t) \Vert _{D(A_2)}\). Proposition B.2 implies that there exists a unique solution in \({\mathcal {S}}_{q, \mu _*, T_*}^\prime \) for small \(T_*^\prime > 0\) and all \(1< q < \infty \). We consider the case \(q > 2\). In this case, we have \(V(t) \in H^{1 + 1/q,q}(\Omega )^2 \hookrightarrow H^1(\Omega )^2\) for \(0< t < T_*^\prime \). We can extend V as \(H^1\)-solution with initial data \(V(T_*^\prime )\) such that
Since \(H^2(\Omega )^2 \hookrightarrow H^{2/q, q}(\Omega )^2\), we see that \(V \in {\mathcal {S}}_{q, \mu _*, \infty }\). By Proposition 6, we have the same order decay estimate as (B10) even for \(L^q\) cases and conclude that
for \(q > 2\). We consider the case \(q < 2\). Since \(f \in L^2(0, \infty ;L^2(\Omega )^2)\) we find from the same type of bootstrapping argument as in [10] that V is also an \(L^2\)-solution satisfying (B12). Since \(D(\tilde{A}_{\mu _*, 2}) \hookrightarrow X_q\), we can extend the solution V globally in \(X_q\) and find that V satisfies (B11). We proved the theorem. \(\square \)
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Furukawa, K. Data Assimilation to the Primitive Equations with \(L^p\)-\(L^q\)-based Maximal Regularity Approach. J. Math. Fluid Mech. 26, 9 (2024). https://doi.org/10.1007/s00021-023-00843-2
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DOI: https://doi.org/10.1007/s00021-023-00843-2