Spectral Stability of Traveling Water Waves: Analytic Dependence of the Spectrum
Abstract The motion of the free surface of an ideal fluid under the effects of gravity and capillarity arises in a number of problems of practical interest (e.g. open-ocean pollutant transport, deep-sea oil platform design, and the generation and propagation of tsunamis), and, consequently, the reli...
Ausführliche Beschreibung
Autor*in: |
Nicholls, David P. [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2007 |
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Schlagwörter: |
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Anmerkung: |
© Springer 2007 |
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Übergeordnetes Werk: |
Enthalten in: Journal of nonlinear science - New York, NY : Springer, 1991, 17(2007), 4 vom: 11. Juni, Seite 369-397 |
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Übergeordnetes Werk: |
volume:17 ; year:2007 ; number:4 ; day:11 ; month:06 ; pages:369-397 |
Links: |
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DOI / URN: |
10.1007/s00332-006-0808-8 |
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Katalog-ID: |
SPR004066952 |
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520 | |a Abstract The motion of the free surface of an ideal fluid under the effects of gravity and capillarity arises in a number of problems of practical interest (e.g. open-ocean pollutant transport, deep-sea oil platform design, and the generation and propagation of tsunamis), and, consequently, the reliable and accurate numerical simulation of these "water waves" is of central importance. In a pair of recent papers the author, in collaboration with F. Reitich (Proc. Roy. Soc. Lond., A, 461(2057): 1283-1309 (2005); Euro. J. Mech. B/Fluids, 25(4): 406-424 (2006)), has developed a new, efficient, stable and high-order Boundary Perturbation scheme (the method of Transformed Field Expansions) for the robust numerical simulation of traveling solutions of the water wave equations. In this paper we extend this Boundary Perturbation technique to address the equally important topic of dynamic stability of these traveling wave forms. More specifically, we describe, and provide the theoretical justification for, a new numerical algorithm to compute the spectrum of the linearized water-wave problem as a function of a parameter, ε, meant to measure the amplitude of the traveling wave. In order to demonstrate the utility of this new method, we also present a sample calculation for two-dimensional waves in water of infinite depth subject to quite general two-dimensional perturbations. | ||
650 | 4 | |a Gravity Wave |7 (dpeaa)DE-He213 | |
650 | 4 | |a Water Wave |7 (dpeaa)DE-He213 | |
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650 | 4 | |a Spectral Stability |7 (dpeaa)DE-He213 | |
650 | 4 | |a Water Wave Problem |7 (dpeaa)DE-He213 | |
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10.1007/s00332-006-0808-8 doi (DE-627)SPR004066952 (SPR)s00332-006-0808-8-e DE-627 ger DE-627 rakwb eng Nicholls, David P. verfasserin aut Spectral Stability of Traveling Water Waves: Analytic Dependence of the Spectrum 2007 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer 2007 Abstract The motion of the free surface of an ideal fluid under the effects of gravity and capillarity arises in a number of problems of practical interest (e.g. open-ocean pollutant transport, deep-sea oil platform design, and the generation and propagation of tsunamis), and, consequently, the reliable and accurate numerical simulation of these "water waves" is of central importance. In a pair of recent papers the author, in collaboration with F. Reitich (Proc. Roy. Soc. Lond., A, 461(2057): 1283-1309 (2005); Euro. J. Mech. B/Fluids, 25(4): 406-424 (2006)), has developed a new, efficient, stable and high-order Boundary Perturbation scheme (the method of Transformed Field Expansions) for the robust numerical simulation of traveling solutions of the water wave equations. In this paper we extend this Boundary Perturbation technique to address the equally important topic of dynamic stability of these traveling wave forms. More specifically, we describe, and provide the theoretical justification for, a new numerical algorithm to compute the spectrum of the linearized water-wave problem as a function of a parameter, ε, meant to measure the amplitude of the traveling wave. In order to demonstrate the utility of this new method, we also present a sample calculation for two-dimensional waves in water of infinite depth subject to quite general two-dimensional perturbations. Gravity Wave (dpeaa)DE-He213 Water Wave (dpeaa)DE-He213 Free Boundary Problem (dpeaa)DE-He213 Spectral Stability (dpeaa)DE-He213 Water Wave Problem (dpeaa)DE-He213 Enthalten in Journal of nonlinear science New York, NY : Springer, 1991 17(2007), 4 vom: 11. Juni, Seite 369-397 (DE-627)268761736 (DE-600)1473165-4 1432-1467 nnns volume:17 year:2007 number:4 day:11 month:06 pages:369-397 https://dx.doi.org/10.1007/s00332-006-0808-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 17 2007 4 11 06 369-397 |
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10.1007/s00332-006-0808-8 doi (DE-627)SPR004066952 (SPR)s00332-006-0808-8-e DE-627 ger DE-627 rakwb eng Nicholls, David P. verfasserin aut Spectral Stability of Traveling Water Waves: Analytic Dependence of the Spectrum 2007 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer 2007 Abstract The motion of the free surface of an ideal fluid under the effects of gravity and capillarity arises in a number of problems of practical interest (e.g. open-ocean pollutant transport, deep-sea oil platform design, and the generation and propagation of tsunamis), and, consequently, the reliable and accurate numerical simulation of these "water waves" is of central importance. In a pair of recent papers the author, in collaboration with F. Reitich (Proc. Roy. Soc. Lond., A, 461(2057): 1283-1309 (2005); Euro. J. Mech. B/Fluids, 25(4): 406-424 (2006)), has developed a new, efficient, stable and high-order Boundary Perturbation scheme (the method of Transformed Field Expansions) for the robust numerical simulation of traveling solutions of the water wave equations. In this paper we extend this Boundary Perturbation technique to address the equally important topic of dynamic stability of these traveling wave forms. More specifically, we describe, and provide the theoretical justification for, a new numerical algorithm to compute the spectrum of the linearized water-wave problem as a function of a parameter, ε, meant to measure the amplitude of the traveling wave. In order to demonstrate the utility of this new method, we also present a sample calculation for two-dimensional waves in water of infinite depth subject to quite general two-dimensional perturbations. Gravity Wave (dpeaa)DE-He213 Water Wave (dpeaa)DE-He213 Free Boundary Problem (dpeaa)DE-He213 Spectral Stability (dpeaa)DE-He213 Water Wave Problem (dpeaa)DE-He213 Enthalten in Journal of nonlinear science New York, NY : Springer, 1991 17(2007), 4 vom: 11. Juni, Seite 369-397 (DE-627)268761736 (DE-600)1473165-4 1432-1467 nnns volume:17 year:2007 number:4 day:11 month:06 pages:369-397 https://dx.doi.org/10.1007/s00332-006-0808-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 17 2007 4 11 06 369-397 |
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10.1007/s00332-006-0808-8 doi (DE-627)SPR004066952 (SPR)s00332-006-0808-8-e DE-627 ger DE-627 rakwb eng Nicholls, David P. verfasserin aut Spectral Stability of Traveling Water Waves: Analytic Dependence of the Spectrum 2007 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer 2007 Abstract The motion of the free surface of an ideal fluid under the effects of gravity and capillarity arises in a number of problems of practical interest (e.g. open-ocean pollutant transport, deep-sea oil platform design, and the generation and propagation of tsunamis), and, consequently, the reliable and accurate numerical simulation of these "water waves" is of central importance. In a pair of recent papers the author, in collaboration with F. Reitich (Proc. Roy. Soc. Lond., A, 461(2057): 1283-1309 (2005); Euro. J. Mech. B/Fluids, 25(4): 406-424 (2006)), has developed a new, efficient, stable and high-order Boundary Perturbation scheme (the method of Transformed Field Expansions) for the robust numerical simulation of traveling solutions of the water wave equations. In this paper we extend this Boundary Perturbation technique to address the equally important topic of dynamic stability of these traveling wave forms. More specifically, we describe, and provide the theoretical justification for, a new numerical algorithm to compute the spectrum of the linearized water-wave problem as a function of a parameter, ε, meant to measure the amplitude of the traveling wave. In order to demonstrate the utility of this new method, we also present a sample calculation for two-dimensional waves in water of infinite depth subject to quite general two-dimensional perturbations. Gravity Wave (dpeaa)DE-He213 Water Wave (dpeaa)DE-He213 Free Boundary Problem (dpeaa)DE-He213 Spectral Stability (dpeaa)DE-He213 Water Wave Problem (dpeaa)DE-He213 Enthalten in Journal of nonlinear science New York, NY : Springer, 1991 17(2007), 4 vom: 11. Juni, Seite 369-397 (DE-627)268761736 (DE-600)1473165-4 1432-1467 nnns volume:17 year:2007 number:4 day:11 month:06 pages:369-397 https://dx.doi.org/10.1007/s00332-006-0808-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 17 2007 4 11 06 369-397 |
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10.1007/s00332-006-0808-8 doi (DE-627)SPR004066952 (SPR)s00332-006-0808-8-e DE-627 ger DE-627 rakwb eng Nicholls, David P. verfasserin aut Spectral Stability of Traveling Water Waves: Analytic Dependence of the Spectrum 2007 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer 2007 Abstract The motion of the free surface of an ideal fluid under the effects of gravity and capillarity arises in a number of problems of practical interest (e.g. open-ocean pollutant transport, deep-sea oil platform design, and the generation and propagation of tsunamis), and, consequently, the reliable and accurate numerical simulation of these "water waves" is of central importance. In a pair of recent papers the author, in collaboration with F. Reitich (Proc. Roy. Soc. Lond., A, 461(2057): 1283-1309 (2005); Euro. J. Mech. B/Fluids, 25(4): 406-424 (2006)), has developed a new, efficient, stable and high-order Boundary Perturbation scheme (the method of Transformed Field Expansions) for the robust numerical simulation of traveling solutions of the water wave equations. In this paper we extend this Boundary Perturbation technique to address the equally important topic of dynamic stability of these traveling wave forms. More specifically, we describe, and provide the theoretical justification for, a new numerical algorithm to compute the spectrum of the linearized water-wave problem as a function of a parameter, ε, meant to measure the amplitude of the traveling wave. In order to demonstrate the utility of this new method, we also present a sample calculation for two-dimensional waves in water of infinite depth subject to quite general two-dimensional perturbations. Gravity Wave (dpeaa)DE-He213 Water Wave (dpeaa)DE-He213 Free Boundary Problem (dpeaa)DE-He213 Spectral Stability (dpeaa)DE-He213 Water Wave Problem (dpeaa)DE-He213 Enthalten in Journal of nonlinear science New York, NY : Springer, 1991 17(2007), 4 vom: 11. Juni, Seite 369-397 (DE-627)268761736 (DE-600)1473165-4 1432-1467 nnns volume:17 year:2007 number:4 day:11 month:06 pages:369-397 https://dx.doi.org/10.1007/s00332-006-0808-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 17 2007 4 11 06 369-397 |
allfieldsSound |
10.1007/s00332-006-0808-8 doi (DE-627)SPR004066952 (SPR)s00332-006-0808-8-e DE-627 ger DE-627 rakwb eng Nicholls, David P. verfasserin aut Spectral Stability of Traveling Water Waves: Analytic Dependence of the Spectrum 2007 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer 2007 Abstract The motion of the free surface of an ideal fluid under the effects of gravity and capillarity arises in a number of problems of practical interest (e.g. open-ocean pollutant transport, deep-sea oil platform design, and the generation and propagation of tsunamis), and, consequently, the reliable and accurate numerical simulation of these "water waves" is of central importance. In a pair of recent papers the author, in collaboration with F. Reitich (Proc. Roy. Soc. Lond., A, 461(2057): 1283-1309 (2005); Euro. J. Mech. B/Fluids, 25(4): 406-424 (2006)), has developed a new, efficient, stable and high-order Boundary Perturbation scheme (the method of Transformed Field Expansions) for the robust numerical simulation of traveling solutions of the water wave equations. In this paper we extend this Boundary Perturbation technique to address the equally important topic of dynamic stability of these traveling wave forms. More specifically, we describe, and provide the theoretical justification for, a new numerical algorithm to compute the spectrum of the linearized water-wave problem as a function of a parameter, ε, meant to measure the amplitude of the traveling wave. In order to demonstrate the utility of this new method, we also present a sample calculation for two-dimensional waves in water of infinite depth subject to quite general two-dimensional perturbations. Gravity Wave (dpeaa)DE-He213 Water Wave (dpeaa)DE-He213 Free Boundary Problem (dpeaa)DE-He213 Spectral Stability (dpeaa)DE-He213 Water Wave Problem (dpeaa)DE-He213 Enthalten in Journal of nonlinear science New York, NY : Springer, 1991 17(2007), 4 vom: 11. Juni, Seite 369-397 (DE-627)268761736 (DE-600)1473165-4 1432-1467 nnns volume:17 year:2007 number:4 day:11 month:06 pages:369-397 https://dx.doi.org/10.1007/s00332-006-0808-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 17 2007 4 11 06 369-397 |
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Enthalten in Journal of nonlinear science 17(2007), 4 vom: 11. Juni, Seite 369-397 volume:17 year:2007 number:4 day:11 month:06 pages:369-397 |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR004066952</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230328150225.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201001s2007 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00332-006-0808-8</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR004066952</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s00332-006-0808-8-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Nicholls, David P.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Spectral Stability of Traveling Water Waves: Analytic Dependence of the Spectrum</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2007</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer 2007</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The motion of the free surface of an ideal fluid under the effects of gravity and capillarity arises in a number of problems of practical interest (e.g. open-ocean pollutant transport, deep-sea oil platform design, and the generation and propagation of tsunamis), and, consequently, the reliable and accurate numerical simulation of these "water waves" is of central importance. 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Spectral Stability of Traveling Water Waves: Analytic Dependence of the Spectrum Gravity Wave (dpeaa)DE-He213 Water Wave (dpeaa)DE-He213 Free Boundary Problem (dpeaa)DE-He213 Spectral Stability (dpeaa)DE-He213 Water Wave Problem (dpeaa)DE-He213 |
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spectral stability of traveling water waves: analytic dependence of the spectrum |
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Spectral Stability of Traveling Water Waves: Analytic Dependence of the Spectrum |
abstract |
Abstract The motion of the free surface of an ideal fluid under the effects of gravity and capillarity arises in a number of problems of practical interest (e.g. open-ocean pollutant transport, deep-sea oil platform design, and the generation and propagation of tsunamis), and, consequently, the reliable and accurate numerical simulation of these "water waves" is of central importance. In a pair of recent papers the author, in collaboration with F. Reitich (Proc. Roy. Soc. Lond., A, 461(2057): 1283-1309 (2005); Euro. J. Mech. B/Fluids, 25(4): 406-424 (2006)), has developed a new, efficient, stable and high-order Boundary Perturbation scheme (the method of Transformed Field Expansions) for the robust numerical simulation of traveling solutions of the water wave equations. In this paper we extend this Boundary Perturbation technique to address the equally important topic of dynamic stability of these traveling wave forms. More specifically, we describe, and provide the theoretical justification for, a new numerical algorithm to compute the spectrum of the linearized water-wave problem as a function of a parameter, ε, meant to measure the amplitude of the traveling wave. In order to demonstrate the utility of this new method, we also present a sample calculation for two-dimensional waves in water of infinite depth subject to quite general two-dimensional perturbations. © Springer 2007 |
abstractGer |
Abstract The motion of the free surface of an ideal fluid under the effects of gravity and capillarity arises in a number of problems of practical interest (e.g. open-ocean pollutant transport, deep-sea oil platform design, and the generation and propagation of tsunamis), and, consequently, the reliable and accurate numerical simulation of these "water waves" is of central importance. In a pair of recent papers the author, in collaboration with F. Reitich (Proc. Roy. Soc. Lond., A, 461(2057): 1283-1309 (2005); Euro. J. Mech. B/Fluids, 25(4): 406-424 (2006)), has developed a new, efficient, stable and high-order Boundary Perturbation scheme (the method of Transformed Field Expansions) for the robust numerical simulation of traveling solutions of the water wave equations. In this paper we extend this Boundary Perturbation technique to address the equally important topic of dynamic stability of these traveling wave forms. More specifically, we describe, and provide the theoretical justification for, a new numerical algorithm to compute the spectrum of the linearized water-wave problem as a function of a parameter, ε, meant to measure the amplitude of the traveling wave. In order to demonstrate the utility of this new method, we also present a sample calculation for two-dimensional waves in water of infinite depth subject to quite general two-dimensional perturbations. © Springer 2007 |
abstract_unstemmed |
Abstract The motion of the free surface of an ideal fluid under the effects of gravity and capillarity arises in a number of problems of practical interest (e.g. open-ocean pollutant transport, deep-sea oil platform design, and the generation and propagation of tsunamis), and, consequently, the reliable and accurate numerical simulation of these "water waves" is of central importance. In a pair of recent papers the author, in collaboration with F. Reitich (Proc. Roy. Soc. Lond., A, 461(2057): 1283-1309 (2005); Euro. J. Mech. B/Fluids, 25(4): 406-424 (2006)), has developed a new, efficient, stable and high-order Boundary Perturbation scheme (the method of Transformed Field Expansions) for the robust numerical simulation of traveling solutions of the water wave equations. In this paper we extend this Boundary Perturbation technique to address the equally important topic of dynamic stability of these traveling wave forms. More specifically, we describe, and provide the theoretical justification for, a new numerical algorithm to compute the spectrum of the linearized water-wave problem as a function of a parameter, ε, meant to measure the amplitude of the traveling wave. In order to demonstrate the utility of this new method, we also present a sample calculation for two-dimensional waves in water of infinite depth subject to quite general two-dimensional perturbations. © Springer 2007 |
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title_short |
Spectral Stability of Traveling Water Waves: Analytic Dependence of the Spectrum |
url |
https://dx.doi.org/10.1007/s00332-006-0808-8 |
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score |
7.4006968 |