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  • 04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamics  (1)
  • granular  (1)
  • 1
    Publication Date: 2017-04-04
    Description: Changes in the Earth’s gravity fi eld are caused by the redistribution of mass within the Earth and on or above its surface.While previous studies [Tapley, 2004; Wahr, 2004] showed that the Gravity Recovery and Climate Experiment (GRACE) satellite mission, executed by NASA,had successfully determined oceanic mass redistribution, the relative motions between two GRACE satellites caused by the 2004 Sumatra tsunami is still uncertain. This present study combines a numerical model of the tsunami and GRACE orbit data to estimate the realistic effect of oceanic mass redistribution on the inter-satellite range-rate change between two GRACE satellites.The GRACE mission is designed to map out the Earth’s gravity field to high accuracy. Instead of measuring the Earth gravity field or mass variations directly, GRACE estimates a set of spherical harmonic coefficients denoting the Earth gravity fi eld each month by measuring range changes between two spacecrafts [Chambers et al., 2004]. The aftermath of this study has shown that the sea surface height anomaly due to the 2004 Sumatra tsunami can cause GRACE inter-satellite range-rate change (i.e., the small relative motions between twin GRACE satellites).When the GRACE trajectories are near the tsunami regions, the range-rate variations are large enough to be observed by GRACE. On 26 December 2004, the fourth strongest earthquake over the past century occurred in the Indian Ocean off the western coast of northern Sumatra, Indonesia. Measuring 9.0 in magnitude, the earthquake generated a massive tsunami that struck the Indian Ocean countries and Somalia.The sudden and violent vertical displacement of the seafl oor caused a disturbance to the overlying water column that propagated rapidly across the whole Indian Ocean.As the tsunami reached shallow water, the height of the wave drastically increased and produced huge inundations and runup heights of up to a few tens of meters.
    Description: Published
    Description: 353-356
    Description: 3.1. Fisica dei terremoti
    Description: 3.3. Geodinamica e struttura dell'interno della Terra
    Description: reserved
    Keywords: Sumatra ; tsunami ; propagation ; gravity ; satellite ; 04. Solid Earth::04.03. Geodesy::04.03.04. Gravity anomalies ; 04. Solid Earth::04.03. Geodesy::04.03.05. Gravity variations ; 04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesy ; 04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    ISSN: 1572-9605
    Keywords: Field-cooled ; granular ; paramagnetic Meissner effect ; isotropic ; anisotropic
    Source: Springer Online Journal Archives 1860-2000
    Topics: Electrical Engineering, Measurement and Control Technology , Physics
    Notes: Abstract The field-cooled magnetization of high-T c superconducting ceramics measured in low magnetic fields exhibits the paramagnetic Meissner effect (PME), i.e., the diamagnetic signal initially increases with decrease in temperature but reaches a maximum at temperatureT d and later decreases with decrease in temperature. Even in some samples the signal is ultimately able to transform inversely into a paramagnetic regime once the sample is cooled below a temperatureT p as long as the applied field is sufficiently small. This PME has been observed in various high-T c cuprates and is explained by disparate aspects. An anisotropic model, in which the granular superconductors are assumed to be ideally anisotropic, was first alternatively proposed in the present work so as to theoretically account for this effect. On the other hand, an isotropic model, suitable for granular superconductors with randomly oriented grains, was proposed to deal with the samples prepared by a conventional solid-state reaction method. The anomalous magnetization behavior in the present model was demonstrated to be the superposition of the diamagnetic signal, which occurs as a result of the intragranular shielding currents, over the paramagnetic one due to the induction of the intergranular component induced by these currents where the intergranular one behaved as the efective pinning centers. The PME was demonstrated by this model to exist parasitically in granular superconductors. This intergranular effect is therefore worthy of remark when evaluating the volume fraction of superconductivity for the samples from the Meissner signal, in particular, at a low magnetic field.
    Type of Medium: Electronic Resource
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