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  • 1
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    In:  Nature, Warszawa, Elsevier Science Publishers B.V., vol. 435, no. 7044, pp. 937-939, pp. L24312, (ISSN: 1340-4202)
    Publication Date: 2005
    Keywords: Earthquake ; Tsunami(s) ; Teleseismic events ; Seismology ; Banda ; Aceh ; GRSN ; Source parameters ; Broad-band ; Seismic networks ; Source time function ; Krueger ; Kruger ; FROTH
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  • 2
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    In:  Geophysical Journal International, Stuttgart, Ferdinand Enke Verlag, vol. 152, no. 3, pp. 597-612, pp. L07611, (ISSN: 1340-4202)
    Publication Date: 2003
    Keywords: Shear waves ; Site amplification ; Velocity depth profile ; NOISE ; Seismic arrays ; GJI
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  • 3
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    In:  Bulletin of the Seismological Society of America, Taipei, AGU, vol. 95, no. 5, pp. 1787-1800, pp. B06304, (ISSN: 1340-4202)
    Publication Date: 2005
    Keywords: Seismology ; Autocorrelation ; Statistical investigations ; Micro-tremor (seismic noise) ; Shear waves ; Velocity depth profile ; Seismic arrays ; Modelling ; BSSA
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  • 4
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    In:  Proceedings of the AGU Fall Meeting, December 13-17, 1999, Rome, Universität Stuttgart, vol. 1034, no. 1, pp. 1075, (ISBN 3-933346-037)
    Publication Date: 1999
    Keywords: Seismic arrays ; NOISE ; Micro-tremor (seismic noise) ; Site amplification ; Horizontal to vertical spectral ratio ; Nakamura ; Spectrum ; noksp
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  • 5
    Publication Date: 2015-08-08
    Description: Permafrost inundated since the last glacial maximum is degrading, potentially releasing trapped or stabilized greenhouse gases, but few observations of the depth of ice-bonded permafrost (IBP) below the sea floor exist for most of the arctic continental shelf. We use spectral ratios of the ambient vibration seismic wave field, together with estimated shear wave velocity from the dispersion curves of surface waves, for estimating the thickness of the sediment overlying the IBP. Peaks in spectral ratios modelled for 3-layered 1D systems correspond with varying thickness of the unfrozen sediment. Seismic receivers were deployed on the sea bed around Muostakh Island in the central Laptev Sea, Siberia. We derive depths of the IBP between 3.7 and 20.7 m ±15 %, increasing with distance from the shoreline. Correspondence between expected permafrost distribution, modelled response and observational data suggest that the method is promising for the determination of the thickness of unfrozen sediment.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 6
    Publication Date: 2015-04-25
    Description: Mobility of glaciers such as rapid retreat or disintegration of large ice volumes produces a large variety of different seismic signals. Thus, evaluating cryospheric seismic events (e.g. changes of their occurrence in space and time) allows to monitor glacier dynamics. We analyze a one year data span recorded at the Neumayer seismic network in Antarctica. Events are automatically recognized using hidden Markov models. In this study we focused on a specific event type occurring close to the grounding line of the Ekström ice shelf. Observed waveform characteristics are consistent with an initial fracturing followed by the resonanceof a water filled cavity resulting in a so-called hybrid event. The number of events detected strongly correlates with dominant tide periods. We assume the cracking to be driven by existing glacier stresses trough bending. Voids are then filled by sea water, exciting the observed resonance. In agreement with this model, events occur almost exclusively during rising tides where cavities are opened at the bottom of the glacier, i.e. at the sea/ice interface.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 7
    Publication Date: 2012-02-16
    Description: SUMMARY The triggering or detection of seismic events out of a continuous seismic data stream is one of the key issues of an automatic or semi-automatic seismic monitoring system. In the case of dense networks, either local or global, most of the implemented trigger algorithms are based on a large number of active stations. However, in the case of only few available stations or small events, for example, like in monitoring volcanoes or hydrothermal power plants, common triggers often show high false alarms. In such cases detection algorithms are of interest, which show reasonable performance when operating even on a single station. In this context, we apply Hidden Markov Models (HMM) which are algorithms borrowed from speech recognition. However, many pitfalls need to be avoided to apply speech recognition technology directly to earthquake detection. We show the fit of the model parameters in an innovative way. State clustering is introduced to refine the intrinsically assumed time dependency of the HMMs and we explain the effect coda has on the recognition results. The methodology is then used for the detection of anthropogenicly induced earthquakes for which we demonstrate for a period of 3.9 months of continuous data that the single station HMM earthquake detector can achieve similar detection rates as a common trigger in combination with coincidence sums over two stations. To show the general applicability of state clustering we apply the proposed method also to earthquake classification at Mt. Merapi volcano, Indonesia.
    Print ISSN: 0956-540X
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
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  • 8
    Publication Date: 2014-05-22
    Description: We examine the use of ambient noise cross-correlation tomography for shallow site characterization using a modified two-step approach. Initially, we extract Rayleigh wave traveltimes from correlation traces of vertical component seismic recordings from a local network installed in Mygdonia basin, Northern Greece. The obtained Rayleigh wave traveltimes show significant spatial variability, as well as distance and frequency dependence due to the 3D structure of the area, dispersion and anelastic attenuation effects. The traveltime datasets are inverted through a surface wave tomography approach to determine group velocity maps for each frequency. The proposed tomographic inversion involves the use of approximate Fresnel volumes and inter-frequency smoothing constraints to stabilize the results. In the last step, we determine a final 3D velocity model using a node-based Monte-Carlo 1D dispersion curve inversion. The reliability of the final 3D velocity model is examined by spatial and depth resolution analysis, as well as by inversion for different model parameterizations. The obtained results are in very good agreement with previous findings from seismic and other geophysical methods. The new 3D V S model provides additional structural constraints for the shallow sediments and bedrock structure of the northern Mygdonia basin up to the depth of ~200-250 m. Present work results suggest that the migration of ambient tomography techniques from large scales (tens or hundreds of km) to local scales (few hundred meters) is possible but cannot be used as a black box technique for 3D modeling and detailed geotechnical site characterization.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 9
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    GFZ Data Services
    Publication Date: 2023-04-25
    Description: Abstract
    Description: The META-WT project was designed to perform a 4-weeks seismic experiment in Germany with a dense seismic array of ~400 three-component geophones that covered (1) a 2.5km x 2.5km wind farm area in Brandenburg, Germany, with almost 200 wind turbines (WTs) and a well-studied subsurface structure and (2) a 20-km long radial line from the center of the wind farm with one geophone every half-kilometer. The objective was to capture the spatio-temporal seismic wave-field signature of the wind farm from continuous recordings of ambient noise. Due to the dense interstation distance and proposed geometry the experiment allowed for analyzing both small-scale wave field characteristics at an unprecedented spatial resolution and the longer distance radiation pattern of the wind farm. Waveform data is available from the GEOFON data centre, under network code XF, and is embargoed until Jan 2025.
    Keywords: Broadband seismic waveforms ; Seismic monitoring ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS 〉 SEISMOLOGICAL STATIONS
    Type: Dataset , Seismic Network
    Format: ~400G
    Format: .mseed
    Format: XML
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  • 10
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 435 (2005), S. 937-939 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] On 26 December 2004, a moment magnitude Mw = 9.3 earthquake occurred along Northern Sumatra, the Nicobar and Andaman islands, resulting in a devastating tsunami in the Indian Ocean region. The rapid and accurate estimation of the rupture length and direction of such ...
    Type of Medium: Electronic Resource
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