Concerning the interaction of non-stationary cross-flow vortices in a three-dimensional boundary layer (Perfect)
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Das Bunte (1990)
EN PB NW
ISBN: 9781234313203 bzw. 1234313200, in Englisch, Rarebooksclub.com, Taschenbuch, neu.
Von Händler/Antiquariat, BuySomeBooks [52360437], Las Vegas, NV, U.S.A.
This item is printed on demand. Paperback. 44 pages. Original publisher: Hampton, Va. : National Aeronautics and Space Administration, Langley Research Center, 1990 OCLC Number: (GPO)apn1992-042705 Excerpt: . . . orders of magnitude and the symmetry of the governing equations becomeof different ( 2. 6 ) is lost. The structures which would govern these limiting cases are then not covered by the work of section 2 and it would be interesting to identify and analyse these structures. On the second branch of solutions ( labelled II on figure 3 ) it is immediately seen that only positive frequencies are found. In particular, we remark that as increases and approaches 0. 187 ( corresponding to a disturbance waveangle of 10. 6 ) the wavenumbers and frequency become small. This suggests the existence of a longer wavelength disturbance with a small wavespeed and this structure corresponds to that of the upper-branch mode investigated in ( 12 ). In this paper, small perturbations with wavenumbers O ( R, ) and wavespeeds O ( R- ) were shown to be possible at waveangles between approximately 10. 6 and 39. 6 . As decreases from p: in our current problem and becomes negative the convergence of the numerical scheme em-ployed becomes increasingly difficult to achieve and only the neutral solutions which can be reliably located by our method have been shown in figure ( 3 ). Indeed, for sufficiently negative the basic profile is monotonically increasing and has no point of inflexion. At these values of parameter, no neutral solutions of the sought type can exist and so it suggests the existence of some p, 0 at which our solutions cut out. It is seen from figure ( 2 ) that as decreases from zero the neutral disturbances have two critical layers up to the point where the basic velocity is no longer non-monotonic. Then the two critical layers must merge, cease to remain asymptotically distinct and a fresh analysis is required. Since the principal thrust of the present work is to study resonant triads we do n. . . This item ships from La Vergne,TN.
This item is printed on demand. Paperback. 44 pages. Original publisher: Hampton, Va. : National Aeronautics and Space Administration, Langley Research Center, 1990 OCLC Number: (GPO)apn1992-042705 Excerpt: . . . orders of magnitude and the symmetry of the governing equations becomeof different ( 2. 6 ) is lost. The structures which would govern these limiting cases are then not covered by the work of section 2 and it would be interesting to identify and analyse these structures. On the second branch of solutions ( labelled II on figure 3 ) it is immediately seen that only positive frequencies are found. In particular, we remark that as increases and approaches 0. 187 ( corresponding to a disturbance waveangle of 10. 6 ) the wavenumbers and frequency become small. This suggests the existence of a longer wavelength disturbance with a small wavespeed and this structure corresponds to that of the upper-branch mode investigated in ( 12 ). In this paper, small perturbations with wavenumbers O ( R, ) and wavespeeds O ( R- ) were shown to be possible at waveangles between approximately 10. 6 and 39. 6 . As decreases from p: in our current problem and becomes negative the convergence of the numerical scheme em-ployed becomes increasingly difficult to achieve and only the neutral solutions which can be reliably located by our method have been shown in figure ( 3 ). Indeed, for sufficiently negative the basic profile is monotonically increasing and has no point of inflexion. At these values of parameter, no neutral solutions of the sought type can exist and so it suggests the existence of some p, 0 at which our solutions cut out. It is seen from figure ( 2 ) that as decreases from zero the neutral disturbances have two critical layers up to the point where the basic velocity is no longer non-monotonic. Then the two critical layers must merge, cease to remain asymptotically distinct and a fresh analysis is required. Since the principal thrust of the present work is to study resonant triads we do n. . . This item ships from La Vergne,TN.
2
Symbolbild
Concerning the interaction of non-stationary cross-flow vortices in a three-dimensional boundary layer (1990)
EN PB NW
ISBN: 9781234313203 bzw. 1234313200, in Englisch, Taschenbuch, neu.
Von Händler/Antiquariat, BuySomeBooks [52360437], Las Vegas, NV, U.S.A.
This item is printed on demand. Paperback. Original publisher: Hampton, Va. : National Aeronautics and Space Administration, Langley Research Center, 1990 OCLC Number: (GPO)apn1992-042705 Excerpt: . . . orders of magnitude and the symmetry of the governing equations becomeof different ( 2. 6 ) is lost. The structures which would govern these limiting cases are then not covered by the work of section 2 and it would be interesting to identify and analyse these structures. On the second branch of solutions ( labelled II on figure 3 ) it is immediately seen that only positive frequencies are found. In particular, we remark that as increases and approaches 0. 187 ( corresponding to a disturbance waveangle of 10. 6 ) the wavenumbers and frequency become small. This suggests the existence of a longer wavelength disturbance with a small wavespeed and this structure corresponds to that of the upper-branch mode investigated in ( 12 ). In this paper, small perturbations with wavenumbers O ( R, ) and wavespeeds O ( R- ) were shown to be possible at waveangles between approximately 10. 6 and 39. 6 . As decreases from p: in our current problem and becomes negative the convergence of the numerical scheme em-ployed becomes increasingly difficult to achieve and only the neutral solutions which can be reliably located by our method have been shown in figure ( 3 ). Indeed, for sufficiently negative the basic profile is monotonically increasing and has no point of inflexion. At these values of parameter, no neutral solutions of the sought type can exist and so it suggests the existence of some p, 0 at which our solutions cut out. It is seen from figure ( 2 ) that as decreases from zero the neutral disturbances have two critical layers up to the point where the basic velocity is no longer non-monotonic. Then the two critical layers must merge, cease to remain asymptotically distinct and a fresh analysis is required. Since the principal thrust of the present work is to study resonant triads we do n. . . This item ships from La Vergne,TN.
This item is printed on demand. Paperback. Original publisher: Hampton, Va. : National Aeronautics and Space Administration, Langley Research Center, 1990 OCLC Number: (GPO)apn1992-042705 Excerpt: . . . orders of magnitude and the symmetry of the governing equations becomeof different ( 2. 6 ) is lost. The structures which would govern these limiting cases are then not covered by the work of section 2 and it would be interesting to identify and analyse these structures. On the second branch of solutions ( labelled II on figure 3 ) it is immediately seen that only positive frequencies are found. In particular, we remark that as increases and approaches 0. 187 ( corresponding to a disturbance waveangle of 10. 6 ) the wavenumbers and frequency become small. This suggests the existence of a longer wavelength disturbance with a small wavespeed and this structure corresponds to that of the upper-branch mode investigated in ( 12 ). In this paper, small perturbations with wavenumbers O ( R, ) and wavespeeds O ( R- ) were shown to be possible at waveangles between approximately 10. 6 and 39. 6 . As decreases from p: in our current problem and becomes negative the convergence of the numerical scheme em-ployed becomes increasingly difficult to achieve and only the neutral solutions which can be reliably located by our method have been shown in figure ( 3 ). Indeed, for sufficiently negative the basic profile is monotonically increasing and has no point of inflexion. At these values of parameter, no neutral solutions of the sought type can exist and so it suggests the existence of some p, 0 at which our solutions cut out. It is seen from figure ( 2 ) that as decreases from zero the neutral disturbances have two critical layers up to the point where the basic velocity is no longer non-monotonic. Then the two critical layers must merge, cease to remain asymptotically distinct and a fresh analysis is required. Since the principal thrust of the present work is to study resonant triads we do n. . . This item ships from La Vergne,TN.
3
Symbolbild
Concerning the interaction of non-stationary cross-flow vortices in a three-dimensional boundary layer (Perfect)
EN NW
ISBN: 9781234313203 bzw. 1234313200, in Englisch, neu.
Von Händler/Antiquariat, ABC Books [9235530], Lowfield Heath, CRAWL, United Kingdom.
Perfect. Original publisher: Hampton, Va.: National Aeronautics and Space Administration, Langley Research Center, 1990] OCLC Number: (GPO)apn1992-042705 Excerpt: . orders of.Shipping may be from our UK, US or Australian warehouse depending on stock availability. This item is printed on demand. 44 pages. 0.100.
Perfect. Original publisher: Hampton, Va.: National Aeronautics and Space Administration, Langley Research Center, 1990] OCLC Number: (GPO)apn1992-042705 Excerpt: . orders of.Shipping may be from our UK, US or Australian warehouse depending on stock availability. This item is printed on demand. 44 pages. 0.100.
4
Concerning the Interaction of Non-Stationary Cross-Flow Vortices in a Three-Dimensional Boundary Layer (2013)
EN NW
ISBN: 9781234313203 bzw. 1234313200, in Englisch, General Books LLC, General Books LLC, General Books LLC, neu.
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U. S. Government,Paperback, German-language edition,Pub by General Books LLC.
U. S. Government,Paperback, German-language edition,Pub by General Books LLC.
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