Covariant Lyapunov Vectors and Finite-Time Normal Modes for Geophysical Fluid Dynamical Systems
Abstract
:1. Introduction
- To establish the relationships between long-time FTNMs and CLVs, and their growth rates, for aperiodic, as well as periodic, chaotic dynamical systems;
- To deduce these properties for systems with degenerate as well as nondegenerate Lyapunov spectra;
- To examine and propose methods for the calculation of CLVs and Lyapunov exponents that allow for degenerate Lyapunov spectra.
2. Dynamical Equations
3. Eigenvectors and Eigenvalues of the Propagator
3.1. Finite-Time Normal Modes
3.2. Finite-Time Adjoint Modes
4. Floquet Vectors
5. Singular Vectors
6. Lyapunov Vectors and Exponents and the Oseledec Theorem
7. Relationships between Covariant Lyapunov Vectors and Orthogonal Lyapunov Vectors
7.1. Construction of Orthonormal Lyapunov Vectors from Covariant Lyapunov Vectors
7.2. Construction of Covariant Lyapunov Vectors from Orthonormal Lyapunov Vectors
7.3. Degenerate Orthonormal Lyapunov Vectors
8. Dynamics in FTNM-Space
Tangent Linear Equation and Propagator in FTNM-Space
9. Covariant Lyapunov Vectors for Periodic Systems
9.1. Dynamics of SVs and OLVs in FTNM-Space
9.2. Construction of CLVs from OLVs in FTNM-Space
9.3. Construction of OLVs from CLVs in FTNM-Space
10. Covariant Lyapunov Vectors for Aperiodic Systems
10.1. Dynamics in FTNM-Space
10.2. Transformation to the Original Phase-Space
11. Calculation of Dynamical Vectors and Metric Entropy Production
11.1. Lyapunov Vectors
11.2. Degeneracy and Nondegeneracy
11.3. Finite-Time Normal Modes and Arnoldi Methods
11.4. Metric Entropy Production
12. Discussion and Conclusions
- 1.
- The covariant properties of FTNMs, , in the time interval are known and determined by , as in Equation (19). We show that they also satisfy the eigenvalue problem in Equation (21) where by definition as noted in Equation (22). The propagator is in general discontinuous at . In the case where it is continuous the FTNMs become Floquet vectors as noted in Equation (37). Indeed, in the efficient Arnoldi algorithm of Wei and Frederiksen [27], discussed in Section 11, the leading FTNMs are constructed by recycling perturbations from to .
- 2.
- In FTNM-space, the right, or initial, SVs and left, or final, SVs , for , are, like the FTNMs, and , proportional to the unit vectors as shown in Equations (73) and (74). This is because the propagator between and in FTNM-space is normal, in fact diagonal (Equation (65)). A particular consequence is that in FTNM-space the singular value exponents are equal to the real part of the FTNM exponents: as noted in Equation (76).
- 3.
- The relationships, based on the Oseledec theorem [72], for the construction of OLVs from CLVs (Equations (53) and (54)) and importantly the determination of CLVs from OLVs (Equations (58) and (59)) and their approximations by long-time SVs in Section 7 greatly simplify at critical times in FTNM-space as shown in Section 9 and Section 10. This is because of the diagonalization of the propagator in result 2 above.
- 4.
- In Appendix C, the propagator in the original -space and the propagator in FTNM-space have both been shown to be homologous to the stretching propagator with the transformation matrices subject to the Lyapunov condition in Equation (A55). This ensures that if the results of Oseledec’s [72] four theorems, including his multiplicative ergodic theorem 4, apply for a propagator in any of the phase-spaces then they hold for all these cohomologous propagator cocycles.
- 5.
- For periodic systems, the results 3 and 4 above have been used in Section 9 to deduce the links of FTNMs to OLVs and CLVs, from Equations (53) to (59), and the equivalence of Floquet vectors and CLVs. Moreover, the Lyapunov exponents , as given in Equation (92). This applies for systems with both real and complex Floquet exponents and nondegenerate and degenerate Lyapunov spectra.
- 6.
- In the case of aperiodic systems, including with degenerate Lyapunov spectra, the results 3 and 4 above have been used in Section 10 to show that in the interval , CLVs are closely approximated by FTNMs, , for large with equality as . Moreover, in FTNM-space the singular value exponent and FTNM growth rates are equal and approximate the Lyapunov exponent with equality as .
- 7.
- An alternative way of establishing the results in 5 and 6 is presented in Appendix E where FTNMs are orthogonalized using the Gram-Smidt method and the long-time limits of the orthonormal vectors are considered particularly in FTNM phase-space.
- 8.
- Finite-time generalizations of the Kolmogorov-Sinai entropy production [8,9] and the Kaplan-Yorke conjectured Hausdorff dimension [97] have been proposed based on the FTNM exponents. The expressions, like the FTNMs, are norm-independent and may be reasonably accurate for ensembles of perturbations as noted in Section 11 although it is possible that intramodal and intermodal interference effects could contribute to individual perturbation growth [79,80].
Funding
Data Availability Statement
Conflicts of Interest
Appendix A. Ordering of Eigenvalues and Eigenvectors
Appendix B. The Oseledec Multiplicative Ergodic Theorem
Appendix B.1. Lyapunov Exponents
Appendix B.2. Oseledec Operators
Appendix B.3. Oseledec Subspaces—Nondegenerate Case
Appendix B.4. Oseledec Subspaces—Degenerate Case
Appendix B.5. Oseledec Operators in FTNM-Space
Appendix C. Lyapunov Homologous Propagator Cocycles
Appendix D. Phase-Space Transformation of CLVs and Lyapunov Exponents
Appendix E. Orthogonalization of FTNMs and Asymptotic Behaviour
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Frederiksen, J.S. Covariant Lyapunov Vectors and Finite-Time Normal Modes for Geophysical Fluid Dynamical Systems. Entropy 2023, 25, 244. https://doi.org/10.3390/e25020244
Frederiksen JS. Covariant Lyapunov Vectors and Finite-Time Normal Modes for Geophysical Fluid Dynamical Systems. Entropy. 2023; 25(2):244. https://doi.org/10.3390/e25020244
Chicago/Turabian StyleFrederiksen, Jorgen S. 2023. "Covariant Lyapunov Vectors and Finite-Time Normal Modes for Geophysical Fluid Dynamical Systems" Entropy 25, no. 2: 244. https://doi.org/10.3390/e25020244
APA StyleFrederiksen, J. S. (2023). Covariant Lyapunov Vectors and Finite-Time Normal Modes for Geophysical Fluid Dynamical Systems. Entropy, 25(2), 244. https://doi.org/10.3390/e25020244