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  • 1
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Nuclear Physics, Section A 189 (1972), S. 368-384 
    ISSN: 0375-9474
    Keywords: Radioactivity
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Physics
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Nuclear Physics, Section A 161 (1971), S. 177-190 
    ISSN: 0375-9474
    Keywords: Radioactivity
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Physics
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2013-06-04
    Description: We have determined for the Bolivian Andes that the new global gravity models derived from the Gravity field and steady-state Ocean Circulation Explorer (GOCE) satellite mission may be used directly to study lithospheric structure. Toward this end, we have formulated Bouguer and isostatic gravity anomalies in spherical approximation, rather than in the usual planar approach, using spherical harmonic series consistent with the satellite-derived gravitational models. From the approximate equivalency of topographic masses and surface density layers using the Helmert condensation method we further derived and used isotropic transfer relations between the spherical spectra of topographic loads and elastic spherical shell deflections, where the Airy isostatic compensation is the special case of no flexural rigidity. A numerical comparison of these spherical harmonic models to conventional three-dimensional modeling based on topographic data and newly acquired surface gravity data in Bolivia confirmed their suitability for lithospheric interpretation. Specifically, the relatively high and uniform resolution of the satellite gravitational model (better than 83 km) produces detailed maps of the isostatic anomaly that clearly delineate the flexure of the Brazilian shield that is thrust under the Sub-Andes. Inferred values of the thickness of Airy-type roots and the flexural rigidity of the elastic lithosphere agree reasonably with published results based on seismic and surface gravity data. In addition, a local minimum in the flexural rigidity is evident at the sharp bend of the eastern margins of the Sub-Andes in Bolivia. This feature is consistent with earlier theories for counter rotations about a vertical axis at this minimum, associated with the confluence of the subducted Nazca plate and the Brazilian craton. The GOCE model thus generates high-resolution isostatic anomaly maps that offer additional structural detail not seen as clearly from previous seismic and gravity investigations in this region.
    Print ISSN: 0016-8033
    Electronic ISSN: 1942-2156
    Topics: Geosciences , Physics
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  • 4
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-07-13
    Description: The National Geodetic Survey (NGS) has been collecting airborne gravity data as part of its Gravity for the Redefinition of the American Vertical Datum (GRAV-D) project since 2008. The end of the first phase of the data collection is approaching (10km line spacing over the US and all of its territories - currently over 97% complete), and all of the data collected to date have been reprocessed. This allows NGS to incorporate a variety of improvements over the initial data set: analysis of multiple East/West line repeats (providing instrument calibration information), a reanalysis of airport absolute gravity ties, consistent use of ITRF2020 positioning throughout the data set, improved off-level corrections, filtering of the gravity disturbance, as well as a generally more consistent and automated (where possible) reduction of raw gravity. The latest version of these efforts also includes all lines flown in partially completed survey areas (or "blocks").We will provide statistics quantifying the improved results - comparisons with gravitational models, crossover line analysis, repeat line analysis, and adjacent line correlations - along with conclusions on their implications. We will also describe the formats and availability of the revised data products.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 5
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-08-09
    Description: The widespread use of relative gravimeters has enabled scientists, surveyors, and engineers to collect large amounts of surface gravity data in a rapid and relatively inexpensive way. Nevertheless, to obtain absolute values of acceleration due to gravity, the relative measurements need to be tied to absolute gravity stations through a network adjustment, and the sources of error present in the data must be accounted for. Gravity observations are affected by (1) systematic errors, such as the gravimeter drift, atmospheric pressure variations, groundwater changes, and Earth tides, (2) random errors (ground vibrations, environmental and transportation conditions, accumulation of random-walk-type errors, etc.) that can allow long wavelength biases to develop in the adjusted solution, especially towards the edges of the network, and (3) blunders (e.g., operator reading and transcribing errors). Therefore, obtaining high accuracy gravity values for thousands of stations that spread over vast distances, largely depends on rigorous data-collection protocols and appropriate adjustment techniques. In this work we present a field protocol that is based on massively redundant observation patterns and a robust two-step least squares adjustment. This methodology, implemented as a Matlab package, guarantees reliable adjusted gravity values with well-constrained standard error estimates. We demonstrate the capabilities of our technique for the case of the Bolivian gravity network (~2400 stations), where the acceleration of gravity was determined with a typical level of uncertainty of 0.1 to 0.15 mGals.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 6
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-08-09
    Description: NOAA’s National Geodetic Survey is on a mission to establish a gravimetric-geoid-based geopotential datum in 2025. This work presents the latest prototype geoid model developed jointly by three agencies of the U.S.A., Canada and Mexico. Each agency is working independently using the same terrestrial gravity data, altimetric gravity and digital elevation models. In addition, the Gravity for the Redefinition of the American Vertical Datum (GRAV-D) project provides airborne gravity data covering all the U.S. territories. GRAV-D data provides critical gravity information in coastal and lake regions and areas where there is no gravity data or data with insufficient quality or distribution. The GRAV-D data was reprocessed to increase its quality and the improved gravity signal is modeled in a spherical harmonic series up to degree and order 2160. Using this spherical harmonic series as the reference field, the residual geoid is computed in the standard remove-compute-restore fashion. The geoid models are compared and validated using the GPS/leveling data collected in the Geoid Slope Validation Survey, which were conducted in 2011, 2014 and 2017. The final geoid model is then computed by weighting the individual countries' contribution. Additionally, the geoid accuracy and relative accuracy of the model are also developed. This paper reports the preliminary results of the prototype geoid model.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 7
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-08-29
    Description: Two preliminary gravity disturbance grids are derived from airborne gravity data collected by the National Geodetic Survey, USA as part of the Gravity for the Redefinition of the American Vertical Datum (GRAV-D) project. The data set does not include releases after 2020. Nominal altitude and spatial resolution of GRAV-D surveys are ~6.3 km and ~20 km, respectively. Actual flight altitude varies from ~ 5 km to ~11 km resulting in heterogeneous spatial resolution of the gravity signal from block to block, and within each block. The airborne data used in this study includes all collected flight lines as of December 2022 covering the US territory and the US-Canada Great Lakes region with extension of about 100 km into Canada and Mexico along land borders. The least-squares collocation is chosen for the 3-D interpolation to derive the two grids at a constant height of 6000 m and on the reference ellipsoid, respectively. The two grids are assessed by the Poisson downward continuation for consistence between the two grids; comparisons are made with ultra-high degree Global Gravitational Models (EGM2008, EIGEN6C-4, XGeoidRefA, and XGM2019e), and a regional geoid model is computed by including the terrestrial gravity data. An airborne-only geoid model is determined and evaluated using GPS-Levelling data over the US and satellite altimetry data over the Great Lakes region. The two new gravity grids are expected to contribute to geodetic, geophysical and geological applications, especially development of the North-American and Pacific Geopotential Datum of 2022 (NAPGD2022).
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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