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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 97 (1989), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: When travel times of group velocities of fundamental mode Rayleigh waves are expressed by means of some functional expansion, spherical harmonics in our case, the singularities appearing in the system of equations lead to the non-uniqueness of the developments. In accordance with a theory about the generation of compatible solutions, different sets of spherical harmonic coefficients are obtained, all of them fitting the experimental travel times with the same accuracy. Due to the linearity between the travel-time data and the spherical harmonic coefficients, the generation and testing of the compatible solutions becomes a very easy process. Imposing physical constraints on the group velocity maps significantly reduces the number of compatible models. Comparison of different compatible models allows an assessment of uncertainty in the group velocity distribution.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 100 (1990), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Several attenuation studies have established a frequency dependence law of the anelastic attenuation factor Q in the form Q=Qo(f/fo)v for the approximate 1–10 Hz frequency range. We propose a method that leads to the determination of Qo, which is a function of the reference frequency fo, and the real exponent v with a single station. to carry out the problem we determine a set of master curves as a function of v. We discuss the method, and the different features of the master curves, when it is applied to the complicated regions of the Iberian Peninsula and to several instruments with different responses. Using this new method and the seismographic stations available in the Iberian Peninsula we have mapped iso-Q0 lines, at a reference frequency of 1 Hz, applying inversion methods. the Q0 values determined for Iberia vary between about 100 and about 600. Values close to 100 correspond to the southern part of Iberia. In general, Qo values increase from south to north with values about 600 near the NW part of Iberia. the Pyrenees Mountains and adjacent areas present Q0 values between about 200 and about 350. These results suggest a strong Q0 lateral variation in Iberia. A considerable frequency dependence of coda-Q has also been determined. the v values vary between 0.3 and 0.8. the Q0 values obtained in the Iberian Peninsula show very good agreement with several Q0 values obtained in other regions of the world. Comparison between the iso-Q0 lines and other geophysical parameters, like regional variations of Pn velocities, heat flow, isoseimal intensity distribution and crustal thickness, indicates that lower Q0 values are associated with higher isoseismal intensity attenuation, higher heat flow, lower Pn velocities and thinner crust.
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 141 (1993), S. 83-100 
    ISSN: 1420-9136
    Keywords: P-waveform inversion ; annealing algorithm ; local stress tensor
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The determination of a local lithospheric stress pattern from low magnitude seismic activity recorded at a loca array is attempted by means of numerical simulations that include waveform inversion and annealing inversion techniques. A set of flat stratified layers are assumed for the propagating medium. The tests show that the annealing algorithm is a useful tool in this kind of study where collected seismic activity at local arrays could help us better understand local stress distributions in the lithosphere. Although real data recorded at local seismic arrays should be processed, assuming more realistic crust and upper mantle models, many characteristics of the annealing process described here could be used when studying real problems.
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  • 4
    ISSN: 1420-9136
    Keywords: Deviatoric stress tensor computation ; constitutive frictional law ; critical orientation of lithospheric fractures
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The principal stress axes and eigenvalue ratios of the stress tensors from two active seismic regions in Alaska (eastern Aleutian Arc and eastern Gulf of Alaska) are computed. These results are obtained using focal mechanisms of earthquakes with magnitudes ranging from 5.5 to 8.2 and show for both regions slightly different compressional states with an orientation of the pressure axis of N26°W for the eastern Gulf of Alaska and N27°W for the east Aleutian Arc. The eigenvalue ratios for the eastern Gulf of Alaska and east Aleutian Arc are 0.84 and 0.99, respectively. The algorithm used in computations allows us to detect some focal mechanisms which are incoherent with respect to the obtained stress tensors. These incoherences are explained in terms of some tectonic features of the region. The orientations of possible pre-existing fractures which would need an unrealistically high maximum shear stress to start a slip on their fault planes are also investigated. These critical orientations depend on a constitutive frictional law as well as on eigenvalue ratios and eigenvectors of the stress tensors. The orientation, which is given in our case by the angle between the normal vector to a fracture and the regional tensional axis, is approximately 59° for the eastern Aleutian Arc. This angle ranges from 49° to 59° for the eastern Gulf of Alaska. It must be pointed out that fractures which need unrealistically high shear stress to start slip on their fault planes are defined by a very narrow band of possible angles between tensional direction and the normal vector to fault plane.
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 137 (1991), S. 113-132 
    ISSN: 1420-9136
    Keywords: Travel time inversion ; information theory
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The total inversion algorithm and some elements of Mathematical Information Theory are used in the treatment of travel-time data belonging to a seismic refraction experiment from the southern segment (Sardinia Channel) of the European Geotraverse Project. The inversion algorithm allows us to improve a preliminary propagating model obtained by means of usual trial and error procedure and to quantify the resolution degree of parameters defining the crust and upper mantle of such a model. Concepts related to Mathematical Information Theory detect some seismic profiles of the refraction experiment which give the most homogeneous coverage of the model in terms of number of trajectories crossing it. Finally, the efficiency of the inversion procedure is quantified and the uncertainties regarding knowledge of different parts of the model are also evaluated.
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 138 (1992), S. 229-247 
    ISSN: 1420-9136
    Keywords: Objective classification algorithm ; local lithospheric stress distribution
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Classification of populations of focal mechanisms are commonly used as a step in retrieving states of stress in the lithosphere. Although such classifications are usually made according to subjective criteria, an objective one based on a classification algorithm is presented. The procedure is based on two steps. First, each mechanism is characterized by the components of its principal tensional and compressional axes and then objectively classified accordingly. Second, each mechanism is characterized by its geographic coordinates (latitude and longitude) after which each group obtained in the first step is divided into new groups according to geographic coordinates. The classification algorithm, together with a standard inversion algorithm, is applied to data from aftershocks belonging to the Irpinia (southern Italy) Earthquake of November 23, 1980. A few incompatible groups of focal mechanisms obtained by the classification algorithm show a spatial overlap. Nevertheless, the new methodology allows us to present a more accurate description of a local state of stress for an aftershock area than the stress pattern obtained from subjective classifications. The new stress pattern is compared with principal stress axes deduced from the main event and two local states of stress deduced previously from the aftershock mechanisms.
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 134 (1990), S. 117-133 
    ISSN: 1420-9136
    Keywords: Seismic refraction ; travel times and waveforms joint inversion ; annealing algorithms
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract An algorithm of annealing is applied to a joint inversion of travel times and waveforms belonging to a synthetically generated seismic refraction experiment. The medium (crust and upper mantle) is modelled by a set of plane stratified layers and a halfspace. The obtained structure (elastic parameters and depth of layers) shows that, in spite of contaminating seismic noise and poor knowledge of the seismic source, annealing methods are a good tool in these kinds of inversion problems. We think that many characteristics of the annealing process described here could be used with real data and more sophisticated media for the crust and upper mantle of the earth than the present example.
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Theoretical and applied climatology 49 (1994), S. 201-212 
    ISSN: 1434-4483
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary A principal component analysis (PCA) based on a network including 179 pluviometric gauges is attempted in order to describe the main patterns governing precipitation in Catalonia (NE Spain). This PCA procedure is applied to the interstation covariance matrix and component loadings are then deduced from it and extensively interpreted. PCA results are used immediately after in a Davis and Kalkstein clustering process, leading to a rainfall division. The homogeneity of the different groups obtained is tested by means of the analysis of their spatial and temporal within-group variances.
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Theoretical and applied climatology 60 (1998), S. 111-120 
    ISSN: 1434-4483
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary A formulation, similar to the procedure employed in seismic risk analysis, has allowed us to quantify probabilities concerning repeated long episodes of dry days for an arbitrary number of years and their return periods. This formulation is based on both a cumulative expression, similar to the well known Gutemberg-Richter seismic law, and the Poisson distribution. We will assume that this latter distribution is applicable, provided that some constraints affecting the length of the dry episodes and their average number recorded on a year are satisfied. In comparison with other methodologies, based on either Markov chains or Gumbell and Jenkinson formulations, we have been able to quantify probabilities concerning repeated long episodes, including extreme events, contributing significantly to the generation of drought episodes. The formulations that we introduce has been applied to sets of dry episodes obtained from daily pluviometric recordings belonging to 69 gauges of the Instituto Nacional de Meteorología located in Catalonia (NE Spain). The results obtained in terms of return period maps, return period-length curves and probabilities for repeated episodes and for an arbitrary number of years are in agreement with previous pluviometric studies and the spatial diversity of the region due to its orographic complexity. The more relevant synoptic situations causing the long dry episodes are summarized and briefly described.
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Theoretical and applied climatology 59 (1998), S. 29-49 
    ISSN: 1434-4483
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary Catalonian daily precipitation patterns were obtained by means of S-mode Principal Component Analysis (PCA) applied to subsets built up according to synoptic surface airflow. Daily data from November to April 1990–1994 from 45 raingauge sites in Catalonia without missing data were used. Eight circulation classes for days in this period were considered. A Precipitation Activity Index (PAI) was calculated for each station and class, leading to the determination of the highest activity regions for each subset. In addition, we determined which circulation type produced most precipitation at each station of the network. Separate PCAs were performed for each of the eight classes considered and the first four Varimax rotated solutions were interpreted for each circulation type. The physical meaning of the rest of the factors were omitted as they were associated with local behaviour. Finally, some concluding remarks on the cyclogenic properties of the Western Mediterranean Basin and the diversity of the extracted patterns are presented and supported by the authors experience in forecasting in Catalonia.
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