ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Ihre E-Mail wurde erfolgreich gesendet. Bitte prüfen Sie Ihren Maileingang.

Leider ist ein Fehler beim E-Mail-Versand aufgetreten. Bitte versuchen Sie es erneut.

Vorgang fortführen?

Exportieren
  • 1
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 126 (1996), S. 0 
    ISSN: 1365-246X
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie
    Notizen: We complete our series of studies on the duality between relatively high-frequency normal modes and seismic body waves by explicitly converting the normal-mode summation expressing the elastic response of a spherically symmetric earth model into a body-wave summation. The procedures in this conversion are discussed in detail for a crust-stripped version of model 1066A with a solid mantle, a fluid outer core and a solid inner core. The resulting body-wave responses, the Green tensors representing the various body waves, are in agreement with the well-documented results obtained using geometrical ray theory.The results derived for the spherically symmetric earth model are then used to obtain the first-order body-wave Green tensors in a laterally heterogeneous earth model based upon the Born approximation. The first-order effect of the coupling between normal-mode multiplets is shown to be equivalent to the single scattering of seismic body waves by the lateral heterogeneity, as expected from numerous previous studies. We present compact expressions for the scattering matrix and the body-wave Frechet kernels. A few numerical examples of the Frechet kernels for monochromatic body waves are also provided.
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 2
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 115 (1993), S. 0 
    ISSN: 1365-246X
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie
    Notizen: The usual JWKB ray-theoretical description of Love and Rayleigh surface wave propagation on a smooth, laterally heterogeneous earth model breaks down in the vicinity of caustics, near the source and its antipode. In this paper we use Maslov theory to obtain a representation of the wavefield that is valid everywhere, even in the presence of caustics. The surface wave trajectories lie on a 3-D manifold in 4-D phase space (θ, φ, kθ, kφ), where θ is the colatitude, φ is the longitude, and kθ and kφ are the covariant components of the wave vector. There are no caustics in phase space; it is only when the rays are projected onto configuration space (θ, φ), the mixed spaces (kθ, φ) and (θ, kφ), or momentum space (kθ, kφ), that caustics occur. The essential strategy is to employ a mixed-space or momentum-space representation in the vicinity of configuration-space caustics, where the (θ, φ) representation fails. By this means we obtain a uniformly valid Green's tensor and an explicit asymptotic expression for the surface wave response to a moment tensor source.
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 3
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 113 (1993), S. 0 
    ISSN: 1365-246X
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie
    Notizen: We present a JWKB theory which describes the propagation of seismic surface waves in a laterally heterogeneous, anisotropic waveguide. We introduce a local dispersion relation and local vertical eigenfunctions which depend explicitly on the direction of the local wavevector as a consequence of the anisotropy. the variation of amplitude along a surface wave ray path is determined by a conservation law for the surface wave energy. Apart from the usual dynamical phase, which is the integral of the local wavevector along a ray path, there is an additional variation in phase in a general anisotropic waveguide. This additional phase, which is an analogue of the Berry phase in adiabatic quantum mechanics, vanishes in a waveguide with a local vertical two-fold symmetry axis or a local horizontal mirror plane.
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 4
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 114 (1993), S. 0 
    ISSN: 1365-246X
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie
    Notizen: The geometrical theory of surface wave propagation on a laterally heterogeneous earth model diverges at caustics, where neighbouring rays cross. the caustics on a spherical earth are degenerate focal points at the source and its antipode; lateral heterogeneity removes this degeneracy and transforms the caustics into multiply cusped and folded curves. We investigate the geometric nature of these antipodal and source caustics using both linear ray-perturbation theory and exact ray tracing. the regions occupied by the R1-R2 and R2-R3 caustics extend as far as 20° from the antipode and 30° from source, respectively, even on a relatively smooth earth model such as M84A.
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 5
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 115 (1993), S. 0 
    ISSN: 1365-246X
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie
    Notizen: We derive asymptotic formulae for the toroidal and spheroidal eigenfrequencies of a SNREI earth model with two discontinuities, by considering the constructive interference of propagating SH and P-SV body waves. For a model with a smooth solid inner core, fluid outer core and mantle, there are four SH and 10 P-SV ray parameters regimes, each of which must be examined separately. The asymptotic eigenfrequency equations in each of these regimes depend only on the intercept times of the propagating wave types and the reflection and transmission coefficients of the waves at the free surface and the two discontinuities. If the classical geometrical plane-wave reflection and transmission coefficients are used, the final eigenfrequency equations are all real. In general, the asymptotic eigenfrequencies agree extremely well with the exact numerical eigenfrequencies; to illustrate this, we present comparisons for a crustless version of earth model 1066A.
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 6
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 121 (1995), S. 0 
    ISSN: 1365-246X
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie
    Notizen: We derive asymptotic expressions for the toroidal- and spheroidal-mode eigenfunctions of a SNREI earth model with two discontinuities. The ray-theoretical wavefunctions of high-frequency SH and P-SV waves are expressed in terms of scalar potentials for which WKBJ solutions are readily available. The normal-mode eigenfunctions are then derived from the wavefunctions using the correspondence between the toroidal modes and SH waves, and the spheroidal modes and P-SV waves. Both oscillatory and evanescent solutions are included to enhance the accuracy of the asymptotic eigenfunctions in the vicinity of the inner-core and core-mantle boundaries. The analytic expressions of the asymptotic eigenfunctions only involve simple sine, cosine and exponential functions which can be easily manipulated and evaluated, making the asymptotic eigenfunctions very useful for further normal-mode studies. Numerical comparison of the asymptotic and exact eigenfunctions shows that there is an excellent agreement for a crustless version of earth model 1066A. A mistake in our previous asymptotic eigenfrequency analysis, which ignored the geometrical spreading effect, has been corrected. The consistency between the asymptotic eigenfrequency and eigenfunction analyses is also addressed.
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 7
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 123 (1995), S. 0 
    ISSN: 1365-246X
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie
    Notizen: A necessary and sufficient condition for the validity of surface-wave ray theory is 〈inlineGraphic alt="inline image" href="urn:x-wiley:0956540X:GJI757:GJI_757_mu1" location="equation/GJI_757_mu1.gif"/〉≪ 1, where 〈inlineGraphic alt="inline image" href="urn:x-wiley:0956540X:GJI757:GJI_757_mu2" location="equation/GJI_757_mu2.gif"/〉 is the root-mean-square degree of the phase-velocity perturbation δc, and l is the degree of the equivalent mode nSl or nTl. This condition, which is independent of the number of orbits, is obtained by consideration of the Fresnel area along the surface-wave ray path between the source and receiver. We assess the accuracy of surface-wave ray theory by comparing the phase, arrival angle and amplitude anomalies obtained using the JWKB approximation with the corresponding quantities measured using ‘ground-truth’ synthetic coupled-mode seismograms on models of varying roughness. The JWKB results agree well with the coupled-mode results for model S12_WM13; on a contrived model with slightly rougher variations, however, the agreement deteriorates as the condition 〈inlineGraphic alt="inline image" href="urn:x-wiley:0956540X:GJI757:GJI_757_mu3" location="equation/GJI_757_mu3.gif"/〉≪ 1 is less well satisfied. The misfit of the ray approximation, which is dependent upon the quantity 〈inlineGraphic alt="inline image" href="urn:x-wiley:0956540X:GJI757:GJI_757_mu4" location="equation/GJI_757_mu4.gif"/〉, can be attributed to diffraction and other finite-frequency effects within the Fresnel area along the ray path; these effects are ignored by the JWKB theory but are fully accounted for by the coupled-mode summation. The wavefront smoothing produced by this Fresnel-area averaging limits the resolution of surface-wave inversion studies based upon the JWKB approximation.
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 8
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 109 (1992), S. 0 
    ISSN: 1365-246X
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie
    Notizen: We present a JWKB theory that describes the propagation of well-dispersed Love and Rayleigh wavegroups on a smooth, laterally heterogeneous Earth model. The analysis is based upon an averaged Lagrangian which yields local Love and Rayleigh eigenfunctions, local dispersion relations, and conservation laws for the surface wave energy. The local dispersion relations determine the surface wave trajectories, and the energy equations determine the surface wave amplitudes. The amplitude of a surface wavegroup varies in time as a result of both dispersion and geometrical spreading. The theory allows for smooth topography on the Earth's surface and any internal discontinuities, and incorporates the effect of self-gravitation.
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 9
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 109 (1992), S. 0 
    ISSN: 1365-246X
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie
    Notizen: We present a JWKB theory for the propagation of monochromatic Love and Rayleigh waves on a smooth, laterally heterogeneous Earth model. The analysis is based upon a slowly varying Lagrangian which yields local Love and Rayleigh eigenfunctions, local dispersion relations, and transport equations which determine the variation in surface wave amplitude along a ray. The amplitude of a monochromatic Love or Rayleigh wave varies only as a result of geometrical spreading; the amplitude diverges and the phase is shifted by /2 each time the wave passes through a caustic singularity, where the width of the ray tube vanishes. We obtain the JWKB surface wave Green's tensor and derive an explicit expression for the JWKB response to a moment tensor source. The theory allows for slowly varying topography of the Earth's surface and any internal discontinuities, and incorporates the effect of self-gravitation and slight anelasticity on surface wave propagation.
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 10
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 106 (1991), S. 0 
    ISSN: 1365-246X
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie
    Notizen: We investigate normal mode multiplet coupling along the fundamental spheroidal mode branch using three different numerical methods. A suite of 300 synthetic vertical accelerograms computed using the great-circle approximation and the first-order subspace-projection algorithm are compared with accurate accelerograms computed using a Rayleigh-Ritz variational method. In each case, the accelerograms are computed by summing the responses of the hybrid multiplets 0S10–10S55; the resulting waveforms correspond to mantle Rayleigh waves with periods between 150 and 600 s. The great-circle approximation correctly represents all but 5 per cent of the waveform variance produced by the degree-8 model of upper mantle heterogeneity M84A, for each of the sequentially arriving wavegroups R1-R6. For a contrived model with a modest amount of additional heterogeneity up to degree 20, the relative great-circle error is substantially greater, approximately 30 per cent. The first-order subspace-projection algorithm requires an order of magnitude more computer time than the great-circle approximation; however it is much more accurate. For the first arriving wavegroup R1, it correctly represents all but 2 per cent of the waveform variance produced by model M84A; this relative error decreases for subsequent wavegroups to less than 1 per cent for R2 and less than 0.2 per cent for R3. For the contrived degree-20 model, the relative subspace-projection error is 6 per cent for R1, 1.5 per cent for R2 and 0.9 per cent for R3; the relative error is less for the later arriving wavegroups because of the increasing effect of the lateral heterogeneity as well as the more rapid attenuation of the higher frequency multiplets that are not as well modelled by the approximation.
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
Schließen ⊗
Diese Webseite nutzt Cookies und das Analyse-Tool Matomo. Weitere Informationen finden Sie hier...