GLORIA

GEOMAR Library Ocean Research Information Access

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
    Online-Ressource
    Online-Ressource
    Seismological Society of America (SSA) ; 2013
    In:  Seismological Research Letters Vol. 84, No. 3 ( 2013-05-01), p. 525-531
    In: Seismological Research Letters, Seismological Society of America (SSA), Vol. 84, No. 3 ( 2013-05-01), p. 525-531
    Materialart: Online-Ressource
    ISSN: 0895-0695 , 1938-2057
    Sprache: Englisch
    Verlag: Seismological Society of America (SSA)
    Publikationsdatum: 2013
    ZDB Id: 2403376-5
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 2
    In: Advances in Geosciences, Copernicus GmbH, Vol. 41 ( 2016-02-02), p. 43-63
    Kurzfassung: Abstract. RHUM-RUM is a German-French seismological experiment based on the sea floor surrounding the island of La Réunion, western Indian Ocean (Barruol and Sigloch, 2013). Its primary objective is to clarify the presence or absence of a mantle plume beneath the Reunion volcanic hotspot. RHUM-RUM's central component is a 13-month deployment (October 2012 to November 2013) of 57 broadband ocean bottom seismometers (OBS) and hydrophones over an area of 2000  ×  2000 km2 surrounding the hotspot. The array contained 48 wideband OBS from the German DEPAS pool and 9 broadband OBS from the French INSU pool. It is the largest deployment of DEPAS and INSU OBS so far, and the first joint experiment. This article reviews network performance and data quality: of the 57 stations, 46 and 53 yielded good seismometer and hydrophone recordings, respectively. The 19 751 total deployment days yielded 18 735 days of hydrophone recordings and 15 941 days of seismometer recordings, which are 94 and 80 % of the theoretically possible yields. The INSU seismic sensors stand away from their OBS frames, whereas the DEPAS sensors are integrated into their frames. At long periods (〉  10 s), the DEPAS seismometers are affected by significantly stronger noise than the INSU seismometers. On the horizontal components, this can be explained by tilting of the frame and buoy assemblage, e.g. through the action of ocean-bottom currents, but in addition the DEPAS intruments are affected by significant self-noise at long periods, including on the vertical channels. By comparison, the INSU instruments are much quieter at periods 〉  30 s and hence better suited for long-period signals studies. The trade-off of the instrument design is that the integrated DEPAS setup is easier to deploy and recover, especially when large numbers of stations are involved. Additionally, the wideband sensor has only half the power consumption of the broadband INSU seismometers. For the first time, this article publishes response information of the DEPAS instruments, which is necessary for any project where true ground displacement is of interest. The data will become publicly available at the end of 2017.
    Materialart: Online-Ressource
    ISSN: 1680-7359
    Sprache: Englisch
    Verlag: Copernicus GmbH
    Publikationsdatum: 2016
    ZDB Id: 2625759-2
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 3
    Online-Ressource
    Online-Ressource
    Oxford University Press (OUP) ; 2021
    In:  Geophysical Journal International Vol. 228, No. 3 ( 2021-12-02), p. 1808-1849
    In: Geophysical Journal International, Oxford University Press (OUP), Vol. 228, No. 3 ( 2021-12-02), p. 1808-1849
    Kurzfassung: Global variations in the propagation of fundamental-mode and overtone surface waves provide unique constraints on the low-frequency source properties and structure of the Earth’s upper mantle, transition zone and mid mantle. We construct a reference data set of multimode dispersion measurements by reconciling large and diverse catalogues of Love-wave (49.65 million) and Rayleigh-wave dispersion (177.66 million) from eight groups worldwide. The reference data set summarizes measurements of dispersion of fundamental-mode surface waves and up to six overtone branches from 44 871 earthquakes recorded on 12 222 globally distributed seismographic stations. Dispersion curves are specified at a set of reference periods between 25 and 250 s to determine propagation-phase anomalies with respect to a reference Earth model. Our procedures for reconciling data sets include: (1) controlling quality and salvaging missing metadata; (2) identifying discrepant measurements and reasons for discrepancies; (3) equalizing geographic coverage by constructing summary rays for travel-time observations and (4) constructing phase velocity maps at various wavelengths with combination of data types to evaluate inter-dataset consistency. We retrieved missing station and earthquake metadata in several legacy compilations and codified scalable formats to facilitate reproducibility, easy storage and fast input/output on high-performance-computing systems. Outliers can be attributed to cycle skipping, station polarity issues or overtone interference at specific epicentral distances. By assessing inter-dataset consistency across similar paths, we empirically quantified uncertainties in traveltime measurements. More than 95 per cent measurements of fundamental-mode dispersion are internally consistent, but agreement deteriorates for overtones especially branches 5 and 6. Systematic discrepancies between raw phase anomalies from various techniques can be attributed to discrepant theoretical approximations, reference Earth models and processing schemes. Phase-velocity variations yielded by the inversion of the summary data set are highly correlated (R ≥ 0.8) with those from the quality-controlled contributing data sets. Long-wavelength variations in fundamental-mode dispersion (50–100 s) are largely independent of the measurement technique with high correlations extending up to degree ∼25. Agreement degrades with increasing branch number and period; highly correlated structure is found only up to degree ∼10 at longer periods (T  & gt; 150 s) and up to degree ∼8 for overtones. Only 2ζ azimuthal variations in phase velocity of fundamental-mode Rayleigh waves were required by the reference data set; maps of 2ζ azimuthal variations are highly consistent between catalogues ( R = 0.6–0.8). Reference data with uncertainties are useful for improving existing measurement techniques, validating models of interior structure, calculating teleseismic data corrections in local or multiscale investigations and developing a 3-D reference Earth model.
    Materialart: Online-Ressource
    ISSN: 0956-540X , 1365-246X
    Sprache: Englisch
    Verlag: Oxford University Press (OUP)
    Publikationsdatum: 2021
    ZDB Id: 3042-9
    ZDB Id: 2006420-2
    ZDB Id: 1002799-3
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 4
    Online-Ressource
    Online-Ressource
    Institute of Electrical and Electronics Engineers (IEEE) ; 2005
    In:  IEEE Transactions on Signal Processing Vol. 53, No. 6 ( 2005-06), p. 2216-2227
    In: IEEE Transactions on Signal Processing, Institute of Electrical and Electronics Engineers (IEEE), Vol. 53, No. 6 ( 2005-06), p. 2216-2227
    Materialart: Online-Ressource
    ISSN: 1053-587X
    RVK:
    Sprache: Unbekannt
    Verlag: Institute of Electrical and Electronics Engineers (IEEE)
    Publikationsdatum: 2005
    ZDB Id: 2034304-8
    ZDB Id: 187297-7
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 5
    Online-Ressource
    Online-Ressource
    MyJove Corporation ; 2020
    In:  Journal of Visualized Experiments , No. 164 ( 2020-10-09)
    In: Journal of Visualized Experiments, MyJove Corporation, , No. 164 ( 2020-10-09)
    Materialart: Online-Ressource
    ISSN: 1940-087X
    Sprache: Englisch
    Verlag: MyJove Corporation
    Publikationsdatum: 2020
    ZDB Id: 2259946-0
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 6
    Online-Ressource
    Online-Ressource
    American Geophysical Union (AGU) ; 2017
    In:  Geophysical Research Letters Vol. 44, No. 21 ( 2017-11-16)
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 44, No. 21 ( 2017-11-16)
    Kurzfassung: Earth's eigenmodes observed at ocean bottom in the absence of earthquakes Linear regression and frequency transfer functions are effective methods to remove tilt and compliance Autocorrelation of continuous data and windowing to show eigenmodes at PREM frequencies
    Materialart: Online-Ressource
    ISSN: 0094-8276 , 1944-8007
    URL: Issue
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 2017
    ZDB Id: 2021599-X
    ZDB Id: 7403-2
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 7
    Online-Ressource
    Online-Ressource
    Springer Science and Business Media LLC ; 2015
    In:  Biomedical Microdevices Vol. 17, No. 4 ( 2015-8)
    In: Biomedical Microdevices, Springer Science and Business Media LLC, Vol. 17, No. 4 ( 2015-8)
    Materialart: Online-Ressource
    ISSN: 1387-2176 , 1572-8781
    Sprache: Englisch
    Verlag: Springer Science and Business Media LLC
    Publikationsdatum: 2015
    ZDB Id: 2004019-2
    SSG: 12
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 8
    Online-Ressource
    Online-Ressource
    Elsevier BV ; 2016
    In:  Acta Oecologica Vol. 72 ( 2016-04), p. 120-128
    In: Acta Oecologica, Elsevier BV, Vol. 72 ( 2016-04), p. 120-128
    Materialart: Online-Ressource
    ISSN: 1146-609X
    Sprache: Englisch
    Verlag: Elsevier BV
    Publikationsdatum: 2016
    ZDB Id: 2003658-9
    SSG: 12
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 9
    Online-Ressource
    Online-Ressource
    Copernicus GmbH ; 2014
    In:  Solid Earth Vol. 5, No. 2 ( 2014-11-17), p. 1055-1069
    In: Solid Earth, Copernicus GmbH, Vol. 5, No. 2 ( 2014-11-17), p. 1055-1069
    Kurzfassung: Abstract. Seismic source inversion is a non-linear problem in seismology where not just the earthquake parameters themselves but also estimates of their uncertainties are of great practical importance. Probabilistic source inversion (Bayesian inference) is very adapted to this challenge, provided that the parameter space can be chosen small enough to make Bayesian sampling computationally feasible. We propose a framework for PRobabilistic Inference of Seismic source Mechanisms (PRISM) that parameterises and samples earthquake depth, moment tensor, and source time function efficiently by using information from previous non-Bayesian inversions. The source time function is expressed as a weighted sum of a small number of empirical orthogonal functions, which were derived from a catalogue of 〉1000 source time functions (STFs) by a principal component analysis. We use a likelihood model based on the cross-correlation misfit between observed and predicted waveforms. The resulting ensemble of solutions provides full uncertainty and covariance information for the source parameters, and permits propagating these source uncertainties into travel time estimates used for seismic tomography. The computational effort is such that routine, global estimation of earthquake mechanisms and source time functions from teleseismic broadband waveforms is feasible.
    Materialart: Online-Ressource
    ISSN: 1869-9529
    Sprache: Englisch
    Verlag: Copernicus GmbH
    Publikationsdatum: 2014
    ZDB Id: 2545676-3
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 10
    Online-Ressource
    Online-Ressource
    Copernicus GmbH ; 2012
    In:  Solid Earth Vol. 3, No. 2 ( 2012-11-07), p. 339-354
    In: Solid Earth, Copernicus GmbH, Vol. 3, No. 2 ( 2012-11-07), p. 339-354
    Kurzfassung: Abstract. Triplicated body waves sample the mantle transition zone more extensively than any other wave type, and interact strongly with the discontinuities at 410 km and 660 km. Since the seismograms bear a strong imprint of these geodynamically interesting features, it is highly desirable to invert them for structure of the transition zone. This has rarely been attempted, due to a mismatch between the complex and band-limited data and the (ray-theoretical) modelling methods. Here we present a data processing and modelling strategy to harness such broadband seismograms for finite-frequency tomography. We include triplicated P-waves (epicentral distance range between 14 and 30°) across their entire broadband frequency range, for both deep and shallow sources. We show that is it possible to predict the complex sequence of arrivals in these seismograms, but only after a careful effort to estimate source time functions and other source parameters from data, variables that strongly influence the waveforms. Modelled and observed waveforms then yield decent cross-correlation fits, from which we measure finite-frequency traveltime anomalies. We discuss two such data sets, for North America and Europe, and conclude that their signal quality and azimuthal coverage should be adequate for tomographic inversion. In order to compute sensitivity kernels at the pertinent high body wave frequencies, we use fully numerical forward modelling of the seismic wavefield through a spherically symmetric Earth.
    Materialart: Online-Ressource
    ISSN: 1869-9529
    Sprache: Englisch
    Verlag: Copernicus GmbH
    Publikationsdatum: 2012
    ZDB Id: 2545676-3
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
Schließen ⊗
Diese Webseite nutzt Cookies und das Analyse-Tool Matomo. Weitere Informationen finden Sie hier...