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A seafloor experiment to monitor vertical deformation at the Lucky Strike volcano, Mid-Atlantic Ridge / Marie-Noëlle Bouin in Journal of geodesy, vol 83 n° 2 (February 2009)
[article]
Titre : A seafloor experiment to monitor vertical deformation at the Lucky Strike volcano, Mid-Atlantic Ridge Type de document : Article/Communication Auteurs : Marie-Noëlle Bouin , Auteur ; V. Ballut, Auteur ; Jérôme Ammann, Auteur ; O. Pot, Auteur ; Olivier de Viron, Auteur ; et al., Auteur Année de publication : 2009 Article en page(s) : pp 147 - 159 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Applications de géodésie spatiale
[Termes IGN] Atlantique (océan)
[Termes IGN] déformation verticale de la croute terrestre
[Termes IGN] dorsale
[Termes IGN] fond marin
[Termes IGN] surveillance géologique
[Termes IGN] volcanRésumé : (Auteur) Decades of cruise-based exploration have provided excellent snapshots of the structure of mid-ocean ridges and have revealed that accretion is a mixture of steady-state and quantum events. Observatory-type studies are now needed to quantify the temporal evolution of these systems. A multi-disciplinary seafloor observatory site is currently being set up at the Lucky Strike volcano, in the axial valley of the slow spreading Mid-Atlantic ridge as a part of the MoMAR (monitoring of the Mid-Atlantic Ridge) initiative. The aim of this observatory is to better understand the dynamics of the volcano and the hydrothermal vents hosted at its summit as well as their plumbing systems. In August 2006, the GRAVILUCK cruise initiated an experiment to monitor the deformation of Lucky Strike volcano. A geodetic network was installed, and seafloor pressure, gravity and magnetic data were collected. In this paper, we present the method used to monitor volcanic deformation, which involves measuring relative depth difference between points within a seafloor geodesy network. We show that, taking into account oceanographic variability and measurement noise, the network should be able to detect vertical deformations of the order of 1 cm. Copyright Springer Numéro de notice : A2009-189 Affiliation des auteurs : non IGN Thématique : POSITIONNEMENT Nature : Article nature-HAL : ArtAvecCL-RevueIntern DOI : 10.1007/s00190-008-0248-3 En ligne : https://doi.org/10.1007/s00190-008-0248-3 Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=29819
in Journal of geodesy > vol 83 n° 2 (February 2009) . - pp 147 - 159[article]Exemplaires(1)
Code-barres Cote Support Localisation Section Disponibilité 266-09021 SL Revue Centre de documentation Revues en salle Disponible Estimating sea floor dynamics in the southern North Sea to improve bathymetric survey planning / L. Dorst (2009)
Titre : Estimating sea floor dynamics in the southern North Sea to improve bathymetric survey planning Type de document : Thèse/HDR Auteurs : L. Dorst, Auteur Editeur : Delft : Netherlands Geodetic Commission NGC Année de publication : 2009 Collection : Netherlands Geodetic Commission Publications on Geodesy, ISSN 0165-1706 num. 69 Importance : 220 p. Format : 17 x 24 cm ISBN/ISSN/EAN : 978-90-6132-311-2 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Bathymétrie
[Termes IGN] bathymétrie
[Termes IGN] covariance
[Termes IGN] déformation de la croute terrestre
[Termes IGN] fond marin
[Termes IGN] géodynamique
[Termes IGN] géostatistique
[Termes IGN] interpolation
[Termes IGN] krigeage
[Termes IGN] marée océanique
[Termes IGN] morphogenèse
[Termes IGN] nivellement indirect
[Termes IGN] Nord, mer du
[Termes IGN] océanographie dynamique
[Termes IGN] port
[Termes IGN] relèvement
[Termes IGN] Rotterdam (Pays-Bas)
[Termes IGN] sable
[Termes IGN] vagueIndex. décimale : 32.10 Bathymétrie Résumé : (Auteur) Safe nautical charts require a carefully designed bathymetric survey policy, especially in shallow sandy seas that potentially have dynamic sea floor patterns. Bathymetric resurveying at sea is a costly process with limited resources, though. A pattern on the sea floor known as tidal sand waves is clearly present in bathymetric surveys, endangering navigation in the Southern North Sea because of the potential dynamics of this pattern. An important factor in an efficient resurvey policy is the type and size of sea floor dynamics. The uncertainties of measurement and interpolation associated with the depth values enable the statistical processing of a time series of surveys, using deformation analysis. Currently, there is no procedure available that satisfies the Royal Netherlands Navy requirements. Therefore, a deformation analysis procedure is designed, implemented and tested in such a way that the procedure works on bathymetric data and satisfies the Royal Netherlands Navy requirements. Also, it is necessary to develop a procedure that translates the results into changes of the resurvey policy, taking into account their confidence intervals.
To describe the sea floor statistically, we assume the sea floor to consist of a spatial trend function (or characterization) and a residual function (or dispersion). Such a description is called a representation. The covariances between positions are expressed in a covariance function, based on the residual function. The covariance function is used by Kriging, an interpolation procedure that propagates the variances and covariances of the data points to variances of the interpolated values. This approach is used widely for spatial analyses, like the interpolation of a bathymetric data set.
The method that we propose uses Kriging to produce a time series of grids of depth values and their variances. Subsequently, it uses deformation analysis, a statistical procedure based on testing theory. Our application of deformation analysis is particularly aimed at the detection of dynamics in areas with tidal sand waves, resulting in parameter estimates for the sea floor dynamics, and their uncertainty. We apply the method to sea floor representations both with and without a sand wave pattern. A test scenario is set up, consisting of a survey of an existing area in the Southern North Sea, for which dynamics are simulated. The results show that the proposed method detects different types of sea floor dynamics well, leading to satisfactory estimates of the corresponding parameters.
We show results for the anchorage area Maas West near the Port of Rotterdam, the Netherlands first. The area is divided into 18 sub-areas. The results show that a sand wave pattern is detected for most of the sub-areas, and a shore-ward migration is detected for a majority of them. The estimated migration rates of the sand waves are up to 7.5 m/yr, with a 95% confidence interval that depends on the regularity of the pattern. The results are in confirmation with previously observed migration rates for the Southern North Sea, and with an idealized process-based model.
Thereafter, we analyze several other areas for which a time series of surveys is available in the bathymetric, archives of the Netherlands Hydrographic Service, to study the spatial variations in sea floor dynamics. We present results for several sand wave areas and a single flat area. In some of those areas, dredging takes place, to guarantee minimum depths. The results indicate sand wave migration in areas close to the coast, and bed level changes of the order of decimeters. The dominant wavelength of the sand waves varies. We compare our results to literature of the same sand wave areas, in which we find similar migration rates, and different wavelengths.
By formulating four indicators, recommendations are made for the resurvey policy on the Belgian and Netherlands Continental Shelf. These indicators follow from the estimates for sea floor dynamics. We present a concept for the shallowest likely depth surface, on which we base two of the indicators. The other two indicators act as a warning: they quantify the potentially missed dynamics, which makes the procedure more robust in case of complicated morphology. We show clear differences in recommended resurvey frequency between the five analyzed regions.
We conclude that the designed method is able to use a time series of bathy-metric surveys for the estimation of sea floor dynamics in a satisfactory way. Those dynamics may be present on the scale of the sea floor, it may be a local effect, or it may be due to a tidal sand wave pattern. Also, the results are successfully reduced to a set of four indicators, used to improve a resurvey policy. Based on these conclusions, we formulate recommendations on the extrapolation of the results in space and time, on potential adaptations to the designed procedure, and on implementation of the procedure.Note de contenu : Preface
1 Introduction
1.1 Nautical charting
1.2 Survey plan design
1.3 Detection of sea floor dynamics
1.4 Tidal sand waves
1.5 The uncertainty of depth measurements
1.6 Problem formulation
1.7 Research question and subquestions
1.8 Research strategy and outline
2 Bathymetric applications of Geostatistics
2.1 Introduction
2.2 Depth as a trend and its residuals
2.3 Covariance functions
2.4 Kriging
2.5 Conclusion
3 Estimating sea floor dynamics
3.1 Introduction
3.2 The method for the estimation of sea floor dynamics
3.3 Specification of a test scenario
3.4 Analysis results of a dynamic sea floor
3.5 Discussion
3.6 Conclusion
3.A Error characteristics
3.B Transformation of the sand wave parameters
3.C The application of statistical estimation and testing
4 The analysis of migrating tidal sand waves
4.1 Introduction
4.2 The application of deformation analysis
4.3 Results of the deformation analysis
4.4 Discussion of results
4.5 Conclusion
4.A Overview of used surveys
4.B Quantification of measurement errors
4.B.1 Covariance function of the error
4.B.2 Variances of the SEES surveys
4.B.3 Variances of the MBES survey
5 Spatial variations in sea floor dynamics
5.1 Introduction
5.2 Deformation analysis
5.3 The Selected Track region: little dynamics
5.4 The Noordhinder region: comparison with other methods
5.5 The region West of IJmuiden: sand wave migration
5.6 The region North of Terschelling: a flat sea floor
5.7 Discussion
5.8 Conclusion
5.A Overview of used surveys
6 Application to the resurvey policy
6.1 Introduction
6.2 Background: Hydrographic practice
6.3 Method: indicators of sea floor dynamicsNuméro de notice : 15495 Affiliation des auteurs : non IGN Thématique : POSITIONNEMENT Nature : Thèse étrangère DOI : sans Accessibilité hors numérique : Non accessible via le SUDOC En ligne : https://www.ncgeo.nl/downloads/69Dorst.pdf Format de la ressource électronique : URL Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=62737 Exemplaires(1)
Code-barres Cote Support Localisation Section Disponibilité 15495-01 32.10 Livre Centre de documentation Topographie Disponible Mouvements verticaux des marégraphes par GPS / Emmanuel Bardiere (2009)
Titre : Mouvements verticaux des marégraphes par GPS : installations, rattachements, traitements et analyses en soutien des actions de l'équipe ULR Type de document : Mémoire Auteurs : Emmanuel Bardiere, Auteur Editeur : Champs-sur-Marne : Ecole nationale des sciences géographiques ENSG Année de publication : 2009 Importance : 96 p. Format : 21 x 30 cm Note générale : Bibliographie
Rapport de projet pluridisciplinaire, cycle des ingénieurs diplômés de l'ENSG 2ème année (IT2)Langues : Français (fre) Descripteur : [Vedettes matières IGN] Applications de géodésie spatiale
[Termes IGN] Bernese
[Termes IGN] déformation verticale de la croute terrestre
[Termes IGN] GAMIT
[Termes IGN] marégraphe
[Termes IGN] Matlab
[Termes IGN] positionnement ponctuel précis
[Termes IGN] rattachement de station
[Termes IGN] série temporelle
[Termes IGN] station GPS
[Termes IGN] temps réelIndex. décimale : PROJET Mémoires : Rapports de projet - stage des ingénieurs de 2e année Résumé : (Auteur) Ce rapport reprend différents aspects d'un stage réalisé au cours de l'été 2009 à l'Université de La Rochelle. Le laboratoire a en charge le suivi, l'entretien et l'installation de stations GPS conjointement à des marégraphes. Le but de l'installation de station GPS en relation avec des marégraphes est de permettre le suivi des mouvements verticaux. Ces mouvements sont aussi bien ceux de la croûte terrestre et des plaques continentales que des mouvements locaux. Par exemple, le quai qui sert du support au marégraphe peut s'affaisser ou se tasser. Aussi, ce rapport comprend des aspects allant des installations techniques de stations GPS aux méthodes mises en œuvre pour l'exploitation des mesures en passant par l'étude des divers modes de collectes des données en temps réel. Un ensemble de documents a été réalisé au cours de ce stage, ils figurent en annexes. Note de contenu : Introduction
1) Installation de nouvelles stations
1.1) Réalisations d'installations simples : aspect purement technique
Bâtiment ILE
Fort Enet/ Fort Boyard
Roscoff
1.2) Prise en charge des aspects administratifs / relationnels
Ile d'Aix
Fort Boyard
Port de La Palliée
2) Automatisation de la collecte des données GPS
2.1) Présentation des matériels et des intervenants
2.2) Solutions retenues
Solution court terme (fiche de vidage)
Solutions pérennes (réseau)
3) Traitements et analyses
Rattachement des zéros
Historique
GPS + Nivellement.
Les différentes méthodes de calcul
Comparaison des méthodes et résultats sur SETE
ConclusionNuméro de notice : 13859 Affiliation des auteurs : non IGN Thématique : POSITIONNEMENT Nature : Mémoire de projet pluridisciplinaire Organisme de stage : Université de La Rochelle ULR Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=50169 Exemplaires(2)
Code-barres Cote Support Localisation Section Disponibilité 13859-01 PROJET Livre Centre de documentation Travaux d'élèves Disponible 13859-02 PROJET Livre Centre de documentation Travaux d'élèves Disponible Physically consistent system model for the study of the Earth's rotation, surface deformation and gravity field parameters / A. Hense (2009)
Titre : Physically consistent system model for the study of the Earth's rotation, surface deformation and gravity field parameters : scientific results of the DFG project Type de document : Monographie Auteurs : A. Hense, Auteur ; J. Sündermann, Auteur ; Hermann Drewes, Auteur ; et al., Auteur Editeur : Munich : Bayerische Akademie der Wissenschaften Année de publication : 2009 Collection : DGK - B Sous-collection : Angewandte Geodäsie num. 317 Importance : 53 p. Format : 21 x 30 cm ISBN/ISSN/EAN : 978-3-7696-8596-1 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Géodésie physique
[Termes IGN] champ de pesanteur terrestre
[Termes IGN] circulation atmosphérique
[Termes IGN] circulation océanique
[Termes IGN] déformation de la croute terrestre
[Termes IGN] modèle hydrographique
[Termes IGN] modèle physique
[Termes IGN] pesanteur terrestre
[Termes IGN] rotation de la Terre
[Termes IGN] surcharge océanique
[Termes IGN] terme de ChandlerIndex. décimale : 30.40 Géodésie physique Résumé : (Auteur) [introduction] This report is the final report of a serie of projects which studied the Earth's rotational parameters angular momentum, tensor of inertia as well as related variables of the Earth's gravitational field. A system view has been taken by trying to incorporate the contributions from the various subsystems of the Earth system in a physically consistent way. This introduction will highlight the project history and performance since 1996 and the state of the art in 2000. Note de contenu : 1. Introduction
1.1 The projects
1.2 Historical overview and motivations
2. Models of subsystems
2.1 Atmosphere models ECHAM
2.1.1 ECHAM5
2.1.2 Stand-alone atmosphere 20th century simulation
2.1.3 Results
2.2 Ocean model OMCT
2.3 Hydrological Discharge Model HDM
2.3.1 Continental hydrology modelling
2.3.1.1 SLS model component
2.3.1.2 HDM model component
2.3.1.3 Atmospheric forcing data
2.3.2 Results
2.3.2.1 Implementation of a 3-D relief model
2.3.2.2 Calculation of gravity field coefficients
2.3.2.3 Test simulations and validation of continental discharge with ECHAM4 and NCEP
2.3.2.4 Verification of simulated continental runoff (control runs)
2.3.2.5 Interface adaptation and verification of mass conservation at the boundaries in the coupled model system
2.3.2.6 Validation and analysis of continental water mass transports of ECOCTH
2.3.2.7 Statistical analysis and validation of simulated gravity field variations
2.3.2.8 Global water balance
2.3.3 Summary
3. Models of the coupled system
3.1 Coupled atmosphere-hydrosphere model ECOCTH
3.1.1 Model description
3.1.2 Validation
3.1.2.1 The lunisolar ocean tides
3.1.2.2 Global ocean circulation
3.1.2.3 Tropical variability and global warming
3.1.3 Results
3.1.3.1 Inter-annual variations and secular trends in length of day
3.2 Dynamic model of Earth rotation, gravity and surface deformation DyMEG
3.2.1 Numerical solution of the Liouville differential equation
3.2.2 Inverse model for surface deformations of the solid Earth due to mass loads
4. Results for Earth rotation, surface deformation and gravity
4.1 Validation of DyMEG with NCEP and ECCO
4.2 Results of DyMEG with ECOCTH forcing
5. Scientific highlights
5.1 Tidal mixing
5.1.1 Tidal mixing in OMCT2
5.1.2 Effect of tidal mixing on ocean water mass properties
5.2 Secular and decadal variations
5.2.1 Coupled simulation of Earth Rotation Parameters
5.2.2 Axial AAM long-term trends in 21st century scenario runs
5.3 Forcing mechanisms of the Chandler oscillation
5.3.1 Atmospheric and hydrospheric excitation of the Chandler oscillation
5.3.2 Noise as excitation mechanism of the Chandler oscillation
6. Conclusions and outlook
7. ReferencesNuméro de notice : 15454 Affiliation des auteurs : non IGN Thématique : POSITIONNEMENT Nature : Monographie Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=62723 Exemplaires(1)
Code-barres Cote Support Localisation Section Disponibilité 15454-01 30.40 Livre Centre de documentation Géodésie Disponible vol 28 - Proceedings of the workshop seismicity patterns in the Euro-Med region, 17-19 november 2008, Luxembourg [Actes] (Bulletin de Cahiers bleus du Centre Europeen de Geodynamique et de Séismologie, vol 28 [01/01/2009]) / A. Oth
[n° ou bulletin]
Titre : vol 28 - Proceedings of the workshop seismicity patterns in the Euro-Med region, 17-19 november 2008, Luxembourg [Actes] Type de document : Périodique Auteurs : A. Oth, Éditeur scientifique Année de publication : 2009 Conférence : ECGS 2008, workshop seismicity patterns in the Euro-Med region 17/11/2008 19/11/2008 Luxembourg Grand Duché du Luxembourg Importance : 163 p. Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Géophysique interne
[Termes IGN] Europe (géographie physique)
[Termes IGN] géodynamique
[Termes IGN] séisme
[Termes IGN] sismologie
[Termes IGN] surveillance géologique
[Termes IGN] tectonique des plaquesNote de contenu : 1- Godey, S., G. Mazet-Roux, R. Bossu, S. Merrer and J. Guilbert - Ten years of seismicity in the Euro-Mediterranean region: Panorama of the EMSC bulletin 1998-2007
2- Griinthal, G. and R. Wahlstrom - A harmonized seismicity data base for the Euro-Mediterranean region
3- Harbi, A. - Compiling an earthquake catalogue for Algeria (ECA): Sources and methods
4- Camelbeeck, Th., E. Knuts, F. Davos and P. Alexandre - The historical earthquake database of the Royal Observatory of Belgium
5- Lecocq, Th., G. Rapagnani, H. Martin, F. Davos, M. Hendrickx, M. Van Camp, K. Vanneste and Th. Camelbeeck - B-FEARS: The Belgian Felt Earthquake Alert and Report System
6- Barth, A., D. Delvaux and F. Wenzel - Tectonic stress field in rift systems - a comparison of Rhinegraben, Baikal Rift and East African Rift
7- Sokolov, V. and F. Wenzel - First steps toward realistic ground-motion prediction for SW-Germany
8- Garcia Moreno, D., A. Hubert-Ferrari, J. Moernaut, J.G. Fraser, X. Boes, U. Avsar, M. Van Daele, E. Damci, N. Cagatay and M. De Batist - Structure of the East Anatolian Fault zone at the Hazar Basin, eastern Turkey
9- Hakimhashemi, A., H. Schelle and G. Griinthal - Time-dependent analysis of the earthquake rates in the Dead Sea Fault zone
10- Kohler, N., F. Wenzel, M. Erdik, H. Alcik, A. Mert and M. Bose - Expansion of the Istanbul Earthquake Early Warning System -Performance tests
11- Bouhadad, Y. - Probabilistic seismic hazard assessment in eastern Algeria
12- Miksat, J., V. Sokolov, K.-L. Wen, F. Wenzel and Ch.-T. Chen - Ground motion simulations for the Taipei basin (Taiwan) for shallow and deep seismicity
13- Mihailov, V. and D. Dojcinovski - Seismic monitoring of structures ? An important element of seismic hazard reduction
14- Daskalaki, E. and G.A. Papadopoulos - Rupture zones of large earthquakes and seismic potential in the Hellenic Arc and Trench
15- Boughacha, M.S. and M. Ouyed - Co-seismic stress transfer in northern Africa through 1980-2008
16- Ouyed, M. and M.S. Boughacha - Seismicity analysis of Algeria and adjacent regions through 1972-2007
17- Dojcinovski, D. and V. Mihailov - Comparison between seismic hazard assessments using Poisson 's and Markov's process - Skopje (Republic of Macedonia) and lower Rhine (Belgium) Case Studies
18- Gospodinov, D., E. Papadimitriou, V. Karakostas and B. Ranguelov - Energy release patterns in aftershock sequences of north Aegean Sea (Greece) through stochastic modeling
19- Popa, M., M. Radulian, N. Mandrescu and D. Paulescu - Seismicity patterns in Vrancea region as revealed by revised historical and instrumental catalogues
20- Raileanu, V., C. Dinu, L. Ardeleanu, V. Diaconescu, E. Popescu and A. Bala - Crustal seismicity and associated fault systems in RomaniaNuméro de notice : 10526 Affiliation des auteurs : non IGN Thématique : POSITIONNEMENT Nature : Numéro de périodique En ligne : https://www.ecgs.lu/wp-content/ecgs_pdf/cahiers/ECGS_CB_Vol28.pdf Format de la ressource électronique : URL bulletin Permalink : https://documentation.ensg.eu/index.php?lvl=bulletin_display&id=31480 [n° ou bulletin]Exemplaires(1)
Code-barres Cote Support Localisation Section Disponibilité 10526-01 CG2008 Livre Centre de documentation Congrès Disponible Tectonique des plaques, séismes et GPS / Christophe Vigny in Géomatique expert, n° 65 (01/11/2008)PermalinkAlgerian permanent GPS network: first results / M. Haddad in Bulletin des sciences géographiques, n° 22 (octobre 2008)PermalinkThe gravitational effect of ocean tide loading at high latitude coastal stations in Norway / D.I. Lysaker in Journal of geodesy, vol 82 n° 9 (September 2008)PermalinkMonitoring post-mining subsidence in the North-Pas-de-Calais coal basin (France): interferometric SAR results and levelling / Daniel Raucoules in Geocarto international, vol 23 n° 4 (August - September 2008)PermalinkRetrieving earthquake signature in GRACE gravity solutions / Olivier de Viron in Geophysical journal international, vol 174 n° 1 (July 2008)PermalinkUplift and subsidence due to the 26 December 2004 Indonesian earthquake detected by SAR data / Marco Chini in International Journal of Remote Sensing IJRS, vol 29 n°13-14 (July 2008)PermalinkSubsidence induced by urbanisation in the city of Rome detected by advanced InSAR technique and geotechnical investigations / S. Stramondo in Remote sensing of environment, vol 112 n° 6 (16/06/2008)PermalinkIntérêt des images radar ERS pour la géologie en Afrique tropicale : application à la cartographie lithostructurale dans la région de Ferkessédougou / B.G. Koffi in Photo interprétation, vol 44 n° 1 (Mars 2008)PermalinkLocal ties, VLBI-GPS eccentricities and combination of geodetic reference frames / Claudio Abbondanza (2008)PermalinkCoseismic and post-seismic signatures of the Sumatra 2004 December and 2005 March earthquakes in GRACE satellite gravity / Isabelle Panet in Geophysical journal international, vol 171 n° 1 (Octobre 2007)Permalink