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Auteur J. Flury |
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Affiner la recherche Interroger des sources externesEarth System Mass Transport Mission (e.motion): A Concept for Future Earth Gravity Field Measurements from Space / Isabelle Panet in Surveys in Geophysics, vol 34 n° 2 (March 2013)
Titre : Earth System Mass Transport Mission (e.motion): A Concept for Future Earth Gravity Field Measurements from Space Type de document : Article/Communication Auteurs : Isabelle Panet Année de publication : 2013 Article en page(s) : pp 141 - 163 Note générale : bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Géodésie physique
[Termes IGN] déformation de la croute terrestre
[Termes IGN] données GRACE
[Termes IGN] gravimétrie spatiale
[Termes IGN] interférométrie à très grande base
[Termes IGN] masse d'eau
[Termes IGN] mission spatiale
[Termes IGN] satellite de télémétrie
[Termes IGN] Terre (planète)Résumé : (auteur) In the last decade, satellite gravimetry has been revealed as a pioneering technique for mapping mass redistributions within the Earth system. This fact has allowed us to have an improved understanding of the dynamic processes that take place within and between the Earth’s various constituents. Results from the Gravity Recovery And Climate Experiment (GRACE) mission have revolutionized Earth system research and have established the necessity for future satellite gravity missions. In 2010, a comprehensive team of European and Canadian scientists and industrial partners proposed the e.motion (Earth system mass transport mission) concept to the European Space Agency. The proposal is based on two tandem satellites in a pendulum orbit configuration at an altitude of about 370 km, carrying a laser interferometer inter-satellite ranging instrument and improved accelerometers. In this paper, we review and discuss a wide range of mass signals related to the global water cycle and to solid Earth deformations that were outlined in the e.motion proposal. The technological and mission challenges that need to be addressed in order to detect these signals are emphasized within the context of the scientific return. This analysis presents a broad perspective on the value and need for future satellite gravimetry missions. Numéro de notice : A2013-814 Affiliation des auteurs : LASTIG LAREG+Ext (2012-mi2018) Thématique : POSITIONNEMENT Nature : Article nature-HAL : ArtAvecCL-RevueIntern DOI : 10.1007/s10712-012-9209-8 Date de publication en ligne : 31/10/2012 En ligne : http://dx.doi.org/10.1007/s10712-012-9209-8 Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=80127
in Surveys in Geophysics > vol 34 n° 2 (March 2013) . - pp 141 - 163[article]
Titre : Astronomical-topographic levelling using high-precision astrogeodetic vertical deflections and Digital Terrain Model data Type de document : Article/Communication Auteurs : C. Hirt, Auteur ; J. Flury, Auteur Année de publication : 2008 Article en page(s) : pp 231 - 248 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Nivellement
[Termes IGN] Alpes
[Termes IGN] champ de pesanteur local
[Termes IGN] collocation par moindres carrés
[Termes IGN] déviation de la verticale
[Termes IGN] modèle numérique de terrain
[Termes IGN] nivellement indirectRésumé : (Auteur) At the beginning of the twenty-first century, a technological change took place in geodetic astronomy by the development of Digital Zenith Camera Systems (DZCS). Such instruments provide vertical deflection data at an angular accuracy level of 0.?1 and better. Recently, DZCS have been employed for the collection of dense sets of astrogeodetic vertical deflection data in several test areas in Germany with high-resolution digital terrain model (DTM) data (10–50 m resolution) available. These considerable advancements motivate a new analysis of the method of astronomical-topographic levelling, which uses DTM data for the interpolation between the astrogeodetic stations. We present and analyse a least-squares collocation technique that uses DTM data for the accurate interpolation of vertical deflection data. The combination of both data sets allows a precise determination of the gravity field along profiles, even in regions with a rugged topography. The accuracy of the method is studied with particular attention on the density of astrogeodetic stations. The error propagation rule of astronomical levelling is empirically derived. It accounts for the signal omission that increases with the station spacing. In a test area located in the German Alps, the method was successfully applied to the determination of a quasigeoid profile of 23 km length. For a station spacing from a few 100 m to about 2 km, the accuracy of the quasigeoid was found to be about 1–2 mm, which corresponds to a relative accuracy of about 0.05-0.1 ppm. Application examples are given, such as the local and regional validation of gravity field models computed from gravimetric data and the economic gravity field determination in geodetically less covered regions. Copyright Springer Numéro de notice : A2008-168 Affiliation des auteurs : non IGN Thématique : POSITIONNEMENT Nature : Article nature-HAL : ArtAvecCL-RevueIntern DOI : 10.1007/s00190-007-0173-x En ligne : https://doi.org/10.1007/s00190-007-0173-x Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=29163
in Journal of geodesy > vol 82 n° 4-5 (April - May 2008) . - pp 231 - 248[article]Exemplaires(2)
Code-barres Cote Support Localisation Section Disponibilité 266-08042 RAB Revue Centre de documentation En réserve L003 Disponible 266-08041 RAB Revue Centre de documentation En réserve L003 Disponible
Titre : Schwerefeldfunktionale im Gebirge : Modellierungsgenauigkeit, Messpunktdichte und Darstellungsfehler am Beispiel des Testnetzes Estergebirge Titre original : [Fonction du champ de pesanteur en montagne : exactitude de la modélisation et erreur de représentation, exemple du réseau test des montagnes Estergebirge] Type de document : Thèse/HDR Auteurs : J. Flury, Auteur Editeur : Munich : Bayerische Akademie der Wissenschaften Année de publication : 2002 Collection : DGK - C Sous-collection : Dissertationen num. 557 Importance : 114 p. Format : 21 x 30 cm ISBN/ISSN/EAN : 978-3-7696-9596-0 Note générale : Bibliographie Langues : Allemand (ger) Descripteur : [Vedettes matières IGN] Géodésie physique
[Termes IGN] alpes orientales
[Termes IGN] anomalie de pesanteur
[Termes IGN] Bavière (Allemagne)
[Termes IGN] champ de pesanteur terrestre
[Termes IGN] géoïde gravimétrique
[Termes IGN] géoïde local
[Termes IGN] hauteur ellipsoïdale
[Termes IGN] levé gravimétrique
[Termes IGN] montagne
[Termes IGN] nivellement
[Termes IGN] nivellement par GPSIndex. décimale : 30.40 Géodésie physique Résumé : (Auteur) In this work the question is examinated, which geoid accuracies can be achieved from gravity field functions which are measured at discrete, but very dense points. The difficult conditions for the required modelling of the topography in mountainous terrain have been considered.
In the Estergebirge mountains in the Bavarian Alps since the year 1994 a very dense network of gravity measurements, precision levelling, precise GPS height measurements and deflections of the vertical has been created, covering all height zones of the terrain. These measurements and their accuracies are described in this work. From levelling, gravity measurements and GPS measurements height anomalies and geoid heights have been determined, analyzed and compared to the german ECG97 geoid model. A precise modelling of the topographic attraction is described for gravity and the deflections of the vertical, based on a high resolution terrain model and a terrain survey of the very near zone of each data point. After the topographic reduction different disturbing bodies with anomalous densities have been detected, with typical characteristics for mountainous areas. Some of these bodies have been modelled taking into account various geophysical data. The models have been used in an adjustment to determine the densities of the topography and the disturbing bodies.
In the second part a statistical analysis of gravity disturbances from the Estergebirge and from other data sets from the Alps is carried out. Empirical signal covariance functions and spectral representations of signal power are shown. The comparison of the different data sets shows good agreement of signal properties. Using measurements in independent control points realistic errors for the continuous representation of the gravity disturbances have been obtained, depending on the density of data points. It is shown, that for high point densities the high frequent parts of the signal are still dominating the representation error, whereas errors of measurement and modelling play a minor role. The representation error computed for selected data point densities have been propagated to geoid errors and errors of spherical harmonic coefficients. The error volume is used as an intermediate step, assuming homogeneous signal properties all over the earth. By this approach it can be shown, that for a geoid error standard deviation of 1 cm the spacing of gravity measurements may not exceed about 5 km.Numéro de notice : 13161 Affiliation des auteurs : non IGN Thématique : POSITIONNEMENT Nature : Thèse étrangère Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=54898 Exemplaires(1)
Code-barres Cote Support Localisation Section Disponibilité 13161-01 30.40 Livre Centre de documentation Géodésie Disponible
