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  • 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous  (29)
  • Lunar and Planetary Science and Exploration
  • E52
  • J24
  • 2010-2014  (30)
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Years
Year
  • 1
    Publication Date: 2019-07-13
    Description: In this paper, we analyze the strong unidentified emission near 3.28 micron in Titan's upper daytime atmosphere recently discovered by Dinelli et al.We have studied it by using the NASA Ames PAH IR Spectroscopic Database. The polycyclic aromatic hydrocarbons (PAHs), after absorbing UV solar radiation, are able to emit strongly near 3.3 micron. By using current models for the redistribution of the absorbed UV energy, we have explained the observed spectral feature and have derived the vertical distribution of PAH abundances in Titan's upper atmosphere. PAHs have been found to be present in large concentrations, about (2-3) 10(exp 4) particles / cubic cm. The identified PAHs have 9-96 carbons, with a concentration-weighted average of 34 carbons. The mean mass is approx 430 u; the mean area is about 0.53 sq. nm; they are formed by 10-11 rings on average, and about one-third of them contain nitrogen atoms. Recently, benzene together with light aromatic species as well as small concentrations of heavy positive and negative ions have been detected in Titan's upper atmosphere. We suggest that the large concentrations of PAHs found here are the neutral counterpart of those positive and negative ions, which hence supports the theory that the origin of Titan main haze layer is located in the upper atmosphere.
    Keywords: Lunar and Planetary Science and Exploration
    Type: ARC-E-DAA-TN13901 , The Astrophysical Journal (ISSN 0004-637X); 770; 2; 132
    Format: application/pdf
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  • 2
    Publication Date: 2020-02-24
    Description: The plate boundary between Africa and Eurasia represents an interesting geodynamical region characterized by a complex pattern of deformation. First-order scientific problems regarding the existence of rigid blocks within the plate boundary, the present-day activity of the Calabrian slab and the regional crust and upper mantle structures are still awaiting for a better understanding. For answering these open questions, INGV deployed a permanent, integrated and real-time monitoring GPS network (RING) all over Italy. The RING is now constituted by about 120 stations. The CGPS sites, acquiring at 1Hz and 30s sampling rate, are integrated either with broad band and very broad band seismometers or accelerometers to improve the monitoring of the background seismicity in the Apennines seismic belts and to better constrain the geometry of the seismogenic structures. Most of the network is connected to the acquisition centre (located in Rome and duplicated in Grottaminarda) by a satellite system (VSAT), while the remaining sites transmit data by Internet and classical phone connections. The satellite data transmission and the integration with seismic instruments makes this network one of the most innovative CGPS networks in Europe. Either the heterogeneity of the installed instrumentation and of the transmission types or the continuous increasing number of stations needed a central monitoring and acquisition system. Thus, in Grottaminarda, for the seismic monitoring we chose to use the open source system Earthworm, developed by USGS, with which we store waveforms and implement automatic localization of the seismic events occurred in the area. As most of the GPS sites are acquired by means of Nanometrics satellite technology, we decided to develop a new software (GpsView), written in Java, to monitor the state of health of those CGPS. This software receives GPS data from NaqsServer (Nanometrics acquisition system) and outputs information about the sites (i.e. position, number of satellites) in real-time. Furthermore, we developed also a web-based application for the management of the data and the metadata relative to the GPS sites of the RING. We present (a) the existing and planned CGPS site distribution, (b) the technological description of the seismic and GPS data acquisitions in Grottaminarda INGV centre, and (c) the first results of CGPS data analysis.
    Description: Unpublished
    Description: San Francisco, USA
    Description: 1.1. TTC - Monitoraggio sismico del territorio nazionale
    Description: 1.9. Rete GPS nazionale
    Description: open
    Keywords: RING and Seismic network ; Italy ; 04. Solid Earth::04.03. Geodesy::04.03.99. General or miscellaneous ; 04. Solid Earth::04.03. Geodesy::04.03.09. Instruments and techniques ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous ; 04. Solid Earth::04.06. Seismology::04.06.06. Surveys, measurements, and monitoring
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Poster session
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  • 3
    Publication Date: 2017-04-04
    Description: In this paper we introduce a simple procedure to identify clusters of multivariate waveforms based on a simultaneous assignation and alignment procedure. This approach is aimed at the identification of clusters of earthquakes,assuming that similarities between seismic events with respect to hypocentral parameters and focal mechanism correspond to similarities between waveforms of events. Therefore we define a distance measure between seismic curve, in order to interpret and better understand the main features of the generating seismic process.
    Description: Published
    Description: 60-69
    Description: 2.5. Laboratorio per lo sviluppo di sistemi di rilevamento sottomarini
    Description: JCR Journal
    Description: reserved
    Keywords: Waveforms clustering, multiplets, Ocean Bottom Seismometer ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 4
    Publication Date: 2020-02-24
    Description: Il 6 settembre 2002 un forte evento sismico (Mw 5.9) colpì la Sicilia settentrionale. L’evento fu localizzato dalla rete sismica nazionale INGV nell’offshore settentrionale siciliano a circa 50 km NNE dalla città di Palermo. Nei tre seguenti mesi oltre un migliaio di aftershocks furono localizzati nella medesima area descrivendo un volume sismo-genetico poco profondo lungo una ventina di chilometri e orientato in direzione NE-SO.Poco dopo l’evento principale le comunicazioni attraverso un cavo sottomarino in fibre ottiche steso tra Palermo e Roma vennero interrotte. Il cavo recuperato apparse quasi completamente fuso (Favali et al., 2006). I test di laboratorio mostrarono una temperatura di fusione del cavo superiore ai 700 °C (Favali et al., 2006). Le informazioni raccolte portarono ad ipotizzare una possibile fuoriuscita di lava sottomarina, innescata dal main-shock, che avrebbe fuso il cavo in fibre ottiche. A distanza di circa 8 anni INGV-CNT ha programmato una campagna di monitoraggio sismo-acustico sottomarino, della durata complessiva di 8 mesi, nell’area epicentrale del suddetto volume sismogenetico. Per tale campagna si è utilizzato un’OBS/H (Ocean Bottom Seismometer with Hydrophone) progettato e realizzato presso l’OBSLab di Gibilmanna (D’Anna et al., 2009). Durante il periodo di deposizione la stazione sismica sottomarina l’OBS/H ha registrato numerosi eventi sismici sia regionali che telesismici. L’analisi preliminare dei segnali di pressione e velocità registrati ha permesso di rilevare inoltre una intensa attività microsismica. Durante gli otto mesi della campagna di monitoraggio sono stati registrati circa 250 eventi sismici di origine locale. Gli eventi micro-sismici, per lo più di ML〈1.5, sono stati registrati anche da alcune stazione della rete sismica onshore. Nel presente lavoro saranno presentati i risultati dell'applicazione di una tecnica di clusterizzazione delle forme d'onda e di un tecnica di localizzazione ipocentrale con stazione singola, alla microsismicità registrata durante la campagna di monitoraggio
    Description: Published
    Description: Prato (Italy)
    Description: 2.5. Laboratorio per lo sviluppo di sistemi di rilevamento sottomarini
    Description: open
    Keywords: Palermo 2002 ; clusterizzazione forme d'onda ; localizzazione con singola stazione ; OBS/H ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 5
    Publication Date: 2020-02-24
    Description: Una rete sismica opportunamente strutturata è un valido strumento per il monitoraggio delle aree sismiche e la valutazione del rischio.Nel presente lavoro viene proposto unmetodo per la valutazione della performance di una rete sismica permezzo di simulazione numerica (SNES, SeismicNetworks Evaluation through Simulation). Per una sua applicazione il metodo necessita come dati di input: il modello di velocità utilizzato nelle routine di localizzazione, l’esatta ubicazione e rumorosità delle stazioni sismiche che compongono la rete e una legge che permette di stimare la varianza dei tempi residui alle varie stazioni. Il metodo permette di determinare, in funzione dellamagnitudo, della profondità ipocentrale e del livello di confidenza, la distribuzione spaziale del numero di stazioni attive nel processo di localizzazione, del gap azimutale e dell’intervallo di confidenza dei parametri ipocentrali, legati sia alla geometria della rete sismica che all’utilizzo di un modello di velocità inadeguato. Negli ultimi anni la RSNC-INGV (Rete Sismica Nazionale Centralizzata dell’Istituto Nazionale di Geofisica e Vulcanologia) è stata ampiamente potenziata; al 2009 riceve segnali da 305 stazioni sismiche di cui ben 258 con sensori 3D a larga banda. Dopo la descrizione del metodo e degli algoritmi utilizzati, vengono mostrati i risultati della sua applicazione alla RSNC-INGV. Tale applicazione ha permesso di individuare le aree più rumorose della RSNC-INGV e di valutare la bontà del modello di velocità utilizzato nelle routine di localizzazione. Il metodo SNES ha permesso inoltre di quantificare la performance di localizzazione della RSNC-INGV e di individuare zone simogenetiche del territorio nazionale attualmente non sufficientemente coperte. L’adeguamento della rete in queste aree può essere progettato per mezzo della tecnica qui descritta.
    Description: Published
    Description: 1-33
    Description: 2.5. Laboratorio per lo sviluppo di sistemi di rilevamento sottomarini
    Description: N/A or not JCR
    Description: open
    Keywords: RSNC-INGV ; Completezza di Magnitudo ; performance di localizzazione ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 6
    Publication Date: 2020-02-24
    Description: earthquakes simulation (SNES - Seismic Networks Evaluation through Simulation). To be applied, the SNES method require: P and S velocity models, seismic attenuation law, seismic stations positions and their experimental noise spectra and, finally, an empirical law that link the variance of the residual times of a station to the hypocenter position. This method allow to map the confidence interval estimates of the hypocentral parameters as function of magnitude, focus depth and confidence level. The simulation was carried out assuming that the epicentres of synthetic earthquakes are located in the knots of a square grid which was covering the investigated area. For each synthetic earthquake, the seismic spectrum was calculated in every station to determine the local Signal to Noise Ratio (SNR): the set of active stations in the location procedure and the relative azimuthal gap was determined by a threshold value of this parameter. Finally, the covariance matrix of synthetic data and the partial derivatives of the model were determined and used to estimate the covariance matrix of the hypocentral parameters. This method was applied to the Italian RSNC-INGV to evaluate its location performance, with a 95% confidence level. This simulation was carried out for small magnitude earthquakes (1.5〈ML〈3, H=10km), both using only P arrival times and P and S arrival times. This simulation allowed to highlight some zones of the Italian peninsula and its surrounding seas that need an improvement of the seismic network. We show how the Ocean Bottom Seismometers can play an important role in this network improvement.
    Description: Published
    Description: Vienna (Austria)
    Description: 2.5. Laboratorio per lo sviluppo di sistemi di rilevamento sottomarini
    Description: open
    Keywords: SNES ; Seismic Network Location Performance ; RSNC-INGV ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 7
    Publication Date: 2020-02-24
    Description: In May 2007, to monitor the seismic processes taking place in the Ionian region, the Centro Nazionale Terremoti, department of INGV, in the frame of the NERIES project (NA6), extended offshore through the deposition of 3 Ocean Bottom Seismometers (OBS) its seismic network. During this experiment the magnitudes of completeness (the magnitude of the smallest events that can be reliably and completely detected by the network) appreciably decreased and the precision of hypocenter estimation of medium-large magnitude earthquakes with epicentres in the Ionian Sea increased. However traveltime-based location methods are inapplicable to many earthquakes recorded only by the OBS’s. The most effective and economical methods to locate small-magnitude seismic events recorded by single three-component stations are based on the polarization analysis of broadband seismic data. The classical polarization analysis assumes that the signal is noise free, nevertheless the 3C recording includes both signal and noise and the polarization analysis is reliable only if the signal to noise ratio is very high. To statistically improve the polarization estimated attributes, we applied a noise correction to the covariance matrix. This correction is based on the assumption that in the selected time-window the noise can be regarded as a stochastic process stationary both in the time and in the space domain. To locate the earthquake hypocenters we used the back-azimuth and emergence angle of P-phase and Ts-Tp delay time. This parameters were estimated by polarization analysis. Using the 1D velocity model proposed by de Voogd (1992) for this region of Ionian Sea, we mapped the emersion angle of the seismic ray and the Ts-Tp delay time as functions of epicentral distance and focal depth. We used the punctual estimates of these parameters and the confidence intervals to determine their intersection region. This method defines in the vertical azimuthal plane the area containing the focus position with some probability. The application of this procedure to about 100 seismic events recorded only by a single OBS, allow to detect low energy seismicity near to the Hyblean-Maltese escarpement.
    Description: Published
    Description: Vienna (Austria)
    Description: 2.5. Laboratorio per lo sviluppo di sistemi di rilevamento sottomarini
    Description: open
    Keywords: OBS ; Ionian Sea ; Single station location ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Poster session
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  • 8
    Publication Date: 2020-02-24
    Description: A procedure for the construction of 3D velocity-density models and earthquake relocation by integrated inversion of P and S wave traveltimes and Bouguer anomaly distribution was applied to a large data set concerning the Sicilian area and portions of the surrounding basins.
    Description: Published
    Description: Trieste (Italy)
    Description: open
    Keywords: joint inversion ; seismic and gravimetric data ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 9
    Publication Date: 2021-03-01
    Description: In this work we aim at two objects: quantifying, by a binomial-beta probabilistic model, the uncertainty involved in the assessment of the intensity decay, an ordinal quantity often incorrectly treated as real variable, and, given the finite dimension of the fault, modelling non-symmetric decays but exploiting information collected from previous studies on symmetric cases. To this end we transform the plane so that the ellipse having the fault length as maximum axis is changed into a circle with fixed diameter. We start from an explorative analysis of a set of macroseismic fields representative of the Italian seismicity among which we identify three different decay trends by applying a hierarchical clustering method. Then we focus on the exam of the seismogenic area of Etna volcano where some fault structures are well recognizable as well as the anisotropic trend of the attenuation. As in volcanic zones the seismic attenuation is much quicker than in other zones, we first shrink and then transform the plane so that the decay becomes again symmetric. Following the Bayesian paradigm we update the model parameters and associate the estimated values of the intensity at site with the corresponding locations in the original plane. Backward validation and comparison with the deterministic law are also presented.
    Description: This work was funded by the Italian Dipartimento della Protezione Civile in the frame of the 2007-2009 Agreement with Istituto Nazionale di Geofisica e Vulcanologia (INGV) - Project V4 FLANK Volcanology.
    Description: Published
    Description: Universidad Carlos III de Madrid, Colmenarejo Campus, on July 5th-8th, 2010
    Description: 4.1. Metodologie sismologiche per l'ingegneria sismica
    Description: open
    Keywords: anisotropy ; Bayesian inference ; seismic attenuation ; Etna volcano ; Italy ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Extended abstract
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  • 10
    Publication Date: 2017-04-04
    Description: La Sicilia Orientale è una delle aree che presenta i valori di pericolosità sismica tra i più elevati in Italia nella mappa di riferimento MPS04 (Gruppo di Lavoro MPS 2004). Considerando che questa è una zona con una elevata esposizione, sia in termini di Beni Culturali che di attività industriali, è stato compiuto uno studio particolareggiato che prendesse in considerazione i molti elementi conoscitivi resisi disponibili negli ultimi anni. E’ stato anche possibile utilizzare i notevoli progressi metodologici, resi possibili grazie allo sviluppo di codici di calcolo sempre più raffinati, che, insieme alle moltiplicate capacità di calcolo dei processori oggi disponibili, rendono queste valutazioni realizzabili in tempi molto brevi e quindi consentono anche di sviluppare modelli con un grado di complessità elevato. I calcoli sono stati realizzati utilizzando la versione 2007 del software CRISIS, un codice Open Source e liberamente distribuito, messo a punto presso l’Università Autonoma del Messico (Ordaz et al., 1999), in particolare usando l’applicazione web sviluppata nell’ambito del progetto INGV-DPC S2 (http://nuovoprogettoesse2.stru.polimi.it) che aggiunge alla versione desktop alcune importanti funzionalità, quali la possibilità di condividere dati tra diversi utenti, l’indipendenza dal sistema operativo utilizzato per lo sviluppo dell’applicazione, l’esecuzione dei calcoli da parte del server liberando le risorse locali dell’utente. CRISIS si basa essenzialmente sull’approccio standard di Cornell (1968) alla stima probabilistica della pericolosità sismica e consente di utilizzare due diversi modelli di sismicità: quello “poissoniano” (vale a dire di eventi indipendenti tra loro e con modalità di rilascio “costanti” nel tempo) e il modello “caratteristico” (che si applica a faglie sismogenetiche per le quali si ipotizza il rilascio di energia attraverso terremoti di magnitudo prefissata e con periodo di ritorno noto). Secondo la prassi standard e consolidata a livello internazionale per la stima della pericolosità sismica (SSHAC, 1997), è stato seguito un approccio cosiddetto ad albero logico per considerare tutte le possibili alternative nella scelta dei modelli utilizzati nel calcolo e valutare l’incertezza epistemica delle stime prodotte derivante dall’uso di queste opzioni.
    Description: Published
    Description: Trieste
    Description: 4.2. TTC - Modelli per la stima della pericolosità sismica a scala nazionale
    Description: open
    Keywords: Pericolosità sismica ; Sicilia Orientale ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Abstract
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