Literatura académica sobre el tema "Gravità globale"
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Artículos de revistas sobre el tema "Gravità globale"
V. Kage, V. Kage, A. Welling A. Welling, P. Gurudut P. Gurudut, S. Patil S. Patil, R. Phadke R. Phadke, M. Joshi M. Joshi y S. Govindaswamy S. Govindaswamy. "Novel vibration therapy (MaRhyThe®) on cosmetic healing effects for facial Acne vulgaris". Journal of Applied Cosmetology 40, n.º 2 (24 de diciembre de 2022): 147/160. http://dx.doi.org/10.56609/jac.v40i2.26.
Texto completoCavazzuti, F., R. Nardi y C. D'Anastasio. "Implicazioni etiche nel trattamento farmacologico dell'anziano". Medicina e Morale 43, n.º 4 (31 de agosto de 1994): 637–65. http://dx.doi.org/10.4081/mem.1994.1006.
Texto completoYılmaz, Mustafa y Bürhan Kozlu. "The Comparison of Gravity Anomalies based on Recent High-Degree Global Models". Afyon Kocatepe University Journal of Sciences and Engineering 18, n.º 3 (1 de diciembre de 2018): 981–90. http://dx.doi.org/10.5578/fmbd.67502.
Texto completoKallosh, Renata, Andrei Linde, Dmitri Linde y Leonard Susskind. "Gravity and global symmetries". Physical Review D 52, n.º 2 (15 de julio de 1995): 912–35. http://dx.doi.org/10.1103/physrevd.52.912.
Texto completoKatanaev, M. O. "Global solutions in gravity". Nuclear Physics B - Proceedings Supplements 88, n.º 1-3 (junio de 2000): 233–36. http://dx.doi.org/10.1016/s0920-5632(00)00774-x.
Texto completoMannheim, Philip D. "Local and global gravity". Foundations of Physics 26, n.º 12 (diciembre de 1996): 1683–709. http://dx.doi.org/10.1007/bf02282129.
Texto completoBouman, Johannes y Martin J. Fuchs. "GOCE gravity gradients versus global gravity field models". Geophysical Journal International 189, n.º 2 (14 de marzo de 2012): 846–50. http://dx.doi.org/10.1111/j.1365-246x.2012.05428.x.
Texto completoDransfield, Mark. "Conforming Falcon gravity and the global gravity anomaly". Geophysical Prospecting 58, n.º 3 (mayo de 2010): 469–83. http://dx.doi.org/10.1111/j.1365-2478.2009.00830.x.
Texto completoPaik, Ho Jung, Jurn-Sun Leung, Samuel H. Morgan y Joseph Parker. "Global gravity survey by an orbiting gravity gradiometer". Eos, Transactions American Geophysical Union 69, n.º 48 (1988): 1601. http://dx.doi.org/10.1029/88eo01211.
Texto completoYale, Mara M. y D. T. Sandwell. "Stacked global satellite gravity profiles". GEOPHYSICS 64, n.º 6 (noviembre de 1999): 1748–55. http://dx.doi.org/10.1190/1.1444680.
Texto completoTesis sobre el tema "Gravità globale"
Mariani, Patrizia. "Caratterizzazione della struttura litosferica del bacino intracratonico del Parana' (Sud America) mediante modellazione di dati gradiometrici e gravimetrici da satelliti di nuova generazione (GRACE e GOCE)". Doctoral thesis, Università degli studi di Trieste, 2012. http://hdl.handle.net/10077/7393.
Texto completoRiassunto: La finalità di questo studio è la caratterizzazione della litosfera sottostante il bacino intracratonico del Paraná. I modelli gravimetrici adottati sono vincolati ai dati geofisici tra i quali quelli sismologici più recenti (Lloyd et al., 2010) e sono corroborati dai modelli petrografici (Bryan & Ernst, 2008). Si offre un approccio che include la comparazione isostatica a quella sismologica al fine di interpretare al meglio la struttura litosferica nell’area del bacino in analisi e di comprendere le variazioni geodinamiche legate alle province geologiche ivi presenti. Il bacino del Paraná (Sud America) è ubicato nella piattaforma stabile del Sud America, ed è circondato da cratoni tra i quali: il cratone amazzonico, il cratone di San Francisco e il Rio de La Plata. La sua genesi in epoca paleozoica è quella di vasto bacino sedimentario, sul quale però durante il Mesozoico (Cretaceo inferiore) si è sviluppata un’intensa attività vulcanica (Capitolo 3). Quest’attività effusiva lo classifica tra le maggiori LIP (Large Igneous Province) mondiali, provincie magmatiche con volume di materiale espulso superiore a 0.1 Mkm3 (Bryan & Ernst, 2008). L’analisi effettuata in questo lavoro è eseguita tramite lo studio del campo gravimetrico da modelli di nuova generazione derivanti dal satellite GOCE (Gravity field and steady state Ocean Circulation Explorer) e GRACE (Gravity Recovery and Climate Experiment). I prodotti gravimetrici satellitari di GOCE possiedono una risoluzione senza precedenti (mezza lunghezza d’onda 80 km): ciò consente di validare i modelli gravimetrici precedenti (280 km, EGM08, Pavlis et al., 2008) che per offrire una maggior dettaglio nelle anomalie integravano ai dati satellitari di GRACE le campagne gravimetriche terrestri, non sempre complete e quindi globalmente precise e di adempire agli indispensabile fini di interpretazione geodinamica. La descrizione dei modelli e la validazione degli stessi sono offerte nel Capitolo 2. I campi potenziali studiati per le principali province geologiche sono illustrati nel Capitolo 5; mentre nel Capitolo 6 si applica la metodologia spettrale sulla seconda derivata verticale del potenziale per discernere le diverse litologie individuate nell’area di studio. L’anomalia di Bouguer calcolata tramite sviluppo in armoniche sferiche viene corretta sia in superficie e in profondità stimando l’effetto di gravità dei sedimenti conosciuti (Capitolo 4) e le conoscenze geofisiche note. Il bacino è composto da: i sedimenti pre-vulcanici paleozoici di spessore pari a circa 3500 m, la Formazione Serra Geral composta principalmente da basalti tholeiitici del cretaceo inferiore (~1500 m di spessore), ed infine i sedimenti post-vulcanici del cretaceo superiore appartenenti al Gruppo Bauru, solo 300 m di spessore (Capitolo 3). Sfruttando i modelli sismologici regionali è stato infine possibile valutare anche il contributo gravimetrico dello spessore crostale stimato con la sismologia. Con questi elementi viene calcolata la Bouguer residua, che è interpretata come anomalia isostatica e quindi correlata alle strutture geologiche locali e regionali. Questo comporta il riconoscimento di una struttura anomala sotto la parte settentrionale del bacino del Paraná comprendente anche parte del settore adiacente Blocco del Guaporé. L’inquadramento a scala maggiore però permette di evidenziare un’area molto più ampia di quanto riconosciuto in prima istanza. Tale anomalia è centrata infatti nel nucleo archeano del cratone amazzonico, di cui quindi il bacino del Paraná risulta solamente il suo braccio più meridionale. In assenza di attività tettonica-magmatica recente (ultima risale 50 Ma) ed in mancanza di grandi anomalie superficiali, tale anomalia positiva potrebbe essere inserita in un contesto regionale e più profondo, rappresentando delle dinamiche di mantello. Infine tramite inversione gravimetrica è stata quantificata numericamente l’anomalia nel bacino di studio utilizzando la geometria semplice di un tronco di cono. La quantità di materiale in presunto underplating che dovrebbe spiegare l’anomalia positiva è compatibile ai modelli petrografici conosciuti. Tali modelli sottolineano come la presenza di un magmatismo noto in superficie rappresenti solo una piccola parte di quello che dovrebbe trovarsi in intrusione: è stato calcolato infatti che il magmatismo superficiale potrebbe rappresentare solo la decima parte di quello associato in profondità.
Abstract: Goal of this study is the characterization of the lithosphere beneath the intracratonic area of Paraná basin. We formulate gravimetric models constrained by geophysical data and new seismological models (Lloyd et al., 2010) and also underpinned by petrographic models (Bryan & Ernst, 2008). Our approach includes isostatic Moho to seismological Moho comparison to better understand lithospheric structures in the area of basin, and geodynamic context of the local geological province. Paraná basin (South America) is located on the stable South American platform, and it is surrounded by some craton areas, as: the Amazon craton, the San Francisco craton and the Rio de La Plata Craton. During Paleozoic epoch the Paraná region was a wide sedimentary basin, while in the Mesozoic (Early Cretaceous) a significant volcanic activity developed on it. This effusive phase classifies the basin between the greatest LIP (Large Igneous Province) worldwide known, where the magmatism volume is greater than 0.1 Mkm3(Bryan & Ernst, 2008). We analyzed gravimetric field using new generation satellite models as GOCE (Gravity field and steady-state Ocean Circulation Explorer) and GRACE (Gravity Recovery and Climate Experiment). GOCE’s products gives unprecedented resolution (half wavelength: 80 km) helping to validate previous global gravity models as EGM08 (Pavlis et al., 2008). The 280 km satellite- only resolution was increased by integration of terrestrial gravity fields data, but this methodology added some problems during processing, where the terrestrial information is not complete or precise. On Chapter 2 some descriptions and validation among models are shown. We calculated potential field for the main geological provinces of Chapter 5; while in Chapter 6, using spectral methodology on the second vertical derivatives of potential field, we identify main lithologic units. The Bouguer anomaly calculated with the spherical harmonics expansion of the potential field is corrected by known stratigraphic units. The basin is made by pre-volcanic sediments of Paleozoic age, with over 3500 m of thickness, Serra Geral Formation, mainly tholeiitic basalts of Early Cretaceous (~1500 m), and post-volcanic sediment of Bauru Group, only 300 m of thickness. We evaluate the effect of crustal thickness variations on the gravity field by using the seismological crustal model. Removing these elements from the Bouguer anomaly, we obtain the residual Bouguer anomaly. Further we calculate the isostatic anomaly and we correlate it to the local and regional geological framework. This helps to recognize a positive residual anomaly on the northern part of the Paraná basin, including the nearby Guaporé Block. Setting a major scale we see the same phenomenon: it is in agreement with the archean nucleus of the Amazon craton, so we can claim that the anomaly on the Paraná is only the southern part of a greater positive area. The relative gravity positive anomaly in the Paraná basin is not very extended and lack of tectonic activity since50 Ma makes us consider that this anomaly is part of a deeper and greater anomaly, maybe due to mantle dynamic effects. We quantified the intracrustal density anomaly using gravity inversion and adopting a truncated cone geometry and volume in accord to petrographic models. It is known that an underplated magmatic body can be up to 10 time larger than the associated extrusive volume and this corroborates our models.
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Lerisson, Gaétan. "Stabilité d'une onde de gravité interne, analyse locale, globale et croissance transitoire". Thesis, Université Paris-Saclay (ComUE), 2017. http://www.theses.fr/2017SACLX017/document.
Texto completoInternal gravity waves that exist in a continuously stratified fluid are particularly important in the ocean. They transport energy and are thought to generate turbulent mixing, which contribute to the deep ocean circulation.We generate an internal wave beam that propagates in a continuously stratified fluid with direct numerical simulations. This situation is equivalent to a tidal wave, where the tidal flow oscillates over a topography and generates a wave. Experimental results obtained by cite{Bourget13} are recovered, ie. the beam destabilizes into a small scale mode. We consider the effect of an horizontal mean flow on the instability and lower the forcing frequency in order to compensate for the doppler effect and to keep locally the same wave. A limit case appears when the forcing becomes stationary. This case is equivalent to a lee wave appearing when a stratified fluid flows over a topography.For small mean flow, small scale instabilities develop as in the tidal case. The beam then stabilizes at intermediate mean flows and destabilizes again for increasing flow speed. At this second threshold, down to the lee wave case, the instability is of much larger scale than for the tidal case. Varying the Reynolds number, the Froude number, the wave angle or the beam size doesn't affect the instability scale selection : a small scale instability in the tidal regime, and large scale instability in the lee regime.We show that the instability mechanism may be interpreted using the triadic instability. Scale selection corresponds to different branches of triadic resonance. We confirm the presence of a stability region for intermediate value of the mean advection velocity by computing the linear eigenmode as Floquet mode with an Arnoldi-Krylov technique and show that the leading eigenmode has a negative growth rate.In the lee wave, case the flow is unstable and a selective frequency damping method cite{Akervik06} is used to compute a steady base flow. We then implement a linear direct-adjoint method to compute the optimal perturbations that maximizes the total energy at different time horizons. At short time horizon, the optimal perturbation is small scale while at large time the perturbation switches to a large scale solution and converges to the large scale mode observed through the nonlinear simulations. Short time transients correspond to the small scale triadic instability advected by the flow whereas the long time large scale instability corresponds to large scale branch of the triadic instability that is able to sustain the flow.We propose an interpretation of the selection of these different instabilities in term of absolute and convective instability. In the case of the lee wave, the large scale instability is absolute whereas the small scale instability is convective (and dominates the short time transient growth because it has a larger local growth rate). When the mean flow is varied, the properties of small scale and large scale instabilities exchange: in the tidal case the short scale instability is absolute and the large scale convective. This conjecture is confirmed by computing the impulse response around a plane monochromatic internal gravity wave in an extended two dimensional periodic domain. The spatio temporal evolution of a perturbation localized in space and time points out the formation of three different wave packets corresponding to different branches of triadic instability. Using the triadic theory with finite detuning cite{McEwan77},we derive the group velocity at the maximum growth rate of the three different branches of triadic instability and find a good agreement with the velocity of the three wave paquet maxima in the impulse response. Analyzing the impulse response along rays, i.e. at x/t and z/tconstant, we compute the absolute growth rate along all possible rays and validate our conjecture
Ceriotti, Matteo. "Global optimisation of multiple gravity assist trajectories". Thesis, University of Glasgow, 2010. http://theses.gla.ac.uk/2003/.
Texto completoWerth, Susanna. "Calibration of the global hydrological model WGHM with water mass variations from GRACE gravity data". Phd thesis, Universität Potsdam, 2010. http://opus.kobv.de/ubp/volltexte/2010/4173/.
Texto completoDas Schwerefeld der Erde spiegelt die Verteilung von Massen auf und unter der Erdoberfläche wieder. Umverteilungen von Erd-, Luft- oder Wassermassen auf unserem Planeten sind damit über eine kontinuierliche Vermessung des Erdschwerefeldes beobachtbar. Besonders Satellitenmissionen sind hierfür geeignet, da deren Umlaufbahn durch zeitliche und räumliche Veränderung der Schwerkraft beeinflusst wird. Seit dem Start der Satellitenmission GRACE (Gravity Recovery And Climate Experiment) im Jahr 2002 stellt die Geodäsie daher globale Daten von zeitlichen Veränderungen des Erdschwerefeldes mit hoher Genauigkeit zur Verfügung. Mit diesen Daten lassen sich geophysikalische und klimatologische Massenumverteilungen auf der Erdoberfläche studieren. GRACE liefert damit erstmals Beobachtungen von Variationen des gesamten kontinentalen Wasserspeichers, welche außerordentlich wertvoll für die Analyse des Wasserkreislaufes über große Regionen sind. Die Daten ermöglichen die Überprüfung von großräumigen mathematischen Modellen der Hydrologie, welche den natürlichen Kreislauf des Wassers auf den Kontinenten, vom Zeitpunkt des Niederschlags bis zum Abfluss in die Ozeane, nachvollziehbar machen. Das verbesserte Verständnis über Transport- und Speicherprozesse von Süßwasser ist für genauere Vorhersagen über zukünftige Wasserverfügbarkeit oder potentielle Naturkatastrophen, wie z.B. Überschwemmungen, von enormer Bedeutung. Ein globales Modell, welches die wichtigsten Komponenten des Wasserkreislaufes (Boden, Schnee, Interzeption, Oberflächen- und Grundwasser) berechnet, ist das "WaterGAP Global Hydrology Model" (WGHM). Vergleiche von berechneten und beobachteten Wassermassenvariationen weisen bisher insbesondere in der jährlichen Amplitude deutliche Differenzen auf. Sehr große Unterschiede zwischen verschiedenen hydrologischen Modellen betonen die Notwendigkeit, deren Berechnungen zu verbessern. Zu diesem Zweck verbindet GRACE die Wissenschaftsbereiche der Geodäsie und der Hydrologie. Diese Verknüpfung verlangt von beiden Seiten die Entwicklung geeigneter Methoden zur Datenintegration, welche die Hauptaufgaben dieser Arbeit darstellten. Dabei handelt es sich insbesondere um die Auswertung der GRACE-Daten mit möglichst hoher Genauigkeit sowie um die Entwicklung einer Strategie zur Integration von GRACE Daten in das hydrologische Modell. Mit Hilfe von GRACE wurde das Modell neu kalbriert, d.h. Parameter im Modell so verändert, dass die hydrologischen Berechnungen besser mit den GRACE Beobachtungen übereinstimmen. Dabei kam ein multikriterieller Kalibrieralgorithmus zur Anwendung mit dem neben GRACE-Daten auch Abflussmessungen einbezogen werden konnten. Die Modellkalibierung wurde weltweit für die 28 größten Flusseinzugsgebiete durchgeführt. In den meisten Fällen konnte eine verbesserte Berechnung von Wassermassenvariationen und Abflüssen erreicht werden. Hieraus ergeben sich, z.B. für tropische Regionen, größere saisonale Variationen. Die Ergebnisse führen zu einem verbesserten Verständnis hydrologischer Prozesse. Zum Schluss konnte die Robustheit der Ergebnisse gegenüber Fehlern in GRACE- und Abflussmessungen erfolgreich getestet werden. Nach den wichtigsten Schlussfolgerungen, die aus den Ergebnissen abgeleitet werden konnten, sind nicht nur Bodenfeuchte- und Schneespeicher, sondern auch Grundwasser- und Oberflächenwasserspeicher in Vergleiche von berechneten und GRACE-beobachteten Wassermassenvariationen einzubeziehen. Weiterhin sind neben Abflussmessungen zusätzlich Beobachtungen von weiteren hydrologischen Prozessen notwendig, um die Ergebnisse mit größerer Genauigkeit überprüfen zu können. Die Ergebnisse dieser Arbeit heben hervor, wie wertvoll GRACE-Daten für die großräumige Hydrologie sind und eröffnen eine Methode zur Verbesserung unseres Verständnisses des globalen Wasserkreislaufes.
Dando, Owen Robert. "Topological defects in low-energy string gravity". Thesis, Durham University, 1999. http://etheses.dur.ac.uk/4496/.
Texto completoHan, Shin-Chan. "Efficient global gravity field determination from satellite-to-satellite tracking". Columbus, Ohio : Ohio State University, 2003. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1061995200.
Texto completoTitle from first page of PDF file. Document formatted into pages; contains xvii, 198 p.; also includes graphics (some col.). Includes abstract and vita. Advisor: Christopher Jekeli, Dept. of Geodetic Science and Surveying. Includes bibliographical references (p. 192-198).
Bai, Lu. "Effects of global financial crisis on Chinese export: a gravity model study". Thesis, Internationella Handelshögskolan, Högskolan i Jönköping, IHH, Economics, Finance and Statistics, 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:hj:diva-18297.
Texto completoWöhr, Andreas J. [Verfasser] y Stefan [Akademischer Betreuer] Teufel. "Global Formalism of Loop Quantum Gravity / Andreas J. Wöhr ; Betreuer: Stefan Teufel". Tübingen : Universitätsbibliothek Tübingen, 2014. http://d-nb.info/1163236373/34.
Texto completoWan, Mohd Akib Wan Abdul Aziz. "A preliminary determination of a gravimetric geoid in Peninsular Malaysia". Thesis, University College London (University of London), 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.283665.
Texto completoBeres, Jadwiga H. "Gravity waves generated by tropical convection : generation mechanisms and implications for global circulation models /". Thesis, Connect to this title online; UW restricted, 2002. http://hdl.handle.net/1773/10048.
Texto completoLibros sobre el tema "Gravità globale"
Global gravity field modelling using satellite gravity gradiometry. Delft, The Netherlands: Nederlandse Commissie voor Geodesie, 1993.
Buscar texto completoRapp, Richard H., Anny A. Cazenave y R. Steven Nerem, eds. Global Gravity Field and Its Temporal Variations. Berlin, Heidelberg: Springer Berlin Heidelberg, 1996. http://dx.doi.org/10.1007/978-3-642-61140-7.
Texto completoAldrovandi, Ruben. Teleparallel Gravity: An Introduction. Dordrecht: Springer Netherlands, 2013.
Buscar texto completoFrancesco, Bonsante, ed. Canonical Wick rotations in 3-dimensional gravity. Providence, R.I: American Mathematical Society, 2009.
Buscar texto completoBernauer, Irene. Lokale Schwerefeldbestimmung und gravimetrische Modellrechnungen im Satelliten (GPS)-Testnetz "Turtmann" (Wallis). Editado por Geiger Alain. Zürich: Schweizerische Geodätische Kommission, 1986.
Buscar texto completoMiropol'sky, Yu Z. Dynamics of Internal Gravity Waves in the Ocean. Dordrecht: Springer Netherlands, 2001.
Buscar texto completoDekle, Robert. Global rebalancing with gravity: Measuring the burden of adjustment. Cambridge, MA: National Bureau of Economic Research, 2008.
Buscar texto completoPoliakovsky, Arkady. Lorentzian Geometrical Structures with Global Time, Gravity and Electrodynamics. Cham: Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-23762-1.
Texto completo1956-, Hamilton Kevin, North Atlantic Treaty Organization. Scientific Affairs Division. y NATO Advanced Research Workshop "Gravity Wave Processes and Their Parameterization in Global Climate Models" (1996 : Santa Fe, [New Mexico]), eds. Gravity wave processes: Their parameterization in global climate models. Berlin: Springer-Verlag, 1997.
Buscar texto completoJ, Bouman. Quality assessment of satellite-based global gravity field models. Delft: NCG, 2000.
Buscar texto completoCapítulos de libros sobre el tema "Gravità globale"
Aldrovandi, Ruben y José Geraldo Pereira. "Global Formulation for Gravity". En Teleparallel Gravity, 73–81. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-5143-9_7.
Texto completoPavlis, Nikolaos K. "Gravity, Global Models". En Encyclopedia of Solid Earth Geophysics, 1–15. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-10475-7_76-1.
Texto completoPavlis, Nikolaos K. "Gravity, Global Models". En Encyclopedia of Solid Earth Geophysics, 533–47. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-8702-7_76.
Texto completoPavlis, Nikolaos K. "Gravity, Global Models". En Encyclopedia of Solid Earth Geophysics, 677–91. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-58631-7_76.
Texto completoMarcantonio, Carla. "Conclusion: Of Gravity and Tears". En Global Melodrama, 143–48. New York: Palgrave Macmillan US, 2015. http://dx.doi.org/10.1057/9781137528193_6.
Texto completoKaula, W. M. "Global Harmonic and Statistical Analysis of Gravimetry". En Gravity Anomalies: Unsurveyed Areas, 58–67. Washington, D.C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm009p0058.
Texto completoZachara-Szymańska, Małgorzata. "Changing the Centre of Gravity". En Global Political Leadership, 76–139. London: Routledge, 2022. http://dx.doi.org/10.4324/9781003166757-3.
Texto completoBerry, P. A. M., R. G. Smith y J. Benveniste. "ACE2: The New Global Digital Elevation Model". En Gravity, Geoid and Earth Observation, 231–37. Berlin, Heidelberg: Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-642-10634-7_30.
Texto completoRummel, Reiner. "Global Unification of Height Systems and GOCE". En Gravity, Geoid and Geodynamics 2000, 13–20. Berlin, Heidelberg: Springer Berlin Heidelberg, 2001. http://dx.doi.org/10.1007/978-3-662-04827-6_3.
Texto completoMcfarlane, N. "Gravity-Wave Drag". En Numerical Modeling of the Global Atmosphere in the Climate System, 297–320. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-011-4046-1_12.
Texto completoActas de conferencias sobre el tema "Gravità globale"
Green, C. M., J. D. Fairhead, S. M. Masterton y P. J. Webb. "Residual Gravity for Plate Tectonic Modelling Based on Global Gravity Model Analysis". En 76th EAGE Conference and Exhibition 2014. Netherlands: EAGE Publications BV, 2014. http://dx.doi.org/10.3997/2214-4609.20141068.
Texto completoSandwell, D. T. "Improved global marine gravity by retracking altimeter waveforms". En Oceans 2003. Celebrating the Past ... Teaming Toward the Future (IEEE Cat. No.03CH37492). IEEE, 2003. http://dx.doi.org/10.1109/oceans.2003.178408.
Texto completoAndersen, Ole B., P. Knudsen, P. A. M. Berry, S. Kenyon y N. Pavlis. "The DNSC07 high resolution global marine gravity field". En SEG Technical Program Expanded Abstracts 2008. Society of Exploration Geophysicists, 2008. http://dx.doi.org/10.1190/1.3063756.
Texto completoHorowitz, Franklin G., Gabriel Strykowski, Fabio Boschetti, Peter Hornby, Nick Archibald, Darren Holden, Peter Ketelaar y Robert Woodcock. "Earthworms; “multiscale” edges in the EGM96 global gravity field". En SEG Technical Program Expanded Abstracts 2000. Society of Exploration Geophysicists, 2000. http://dx.doi.org/10.1190/1.1816081.
Texto completoDing, Yaqing, Daniel Barath, Jian Yang, Hui Kong y Zuzana Kukelova. "Globally Optimal Relative Pose Estimation with Gravity Prior". En 2021 IEEE/CVF Conference on Computer Vision and Pattern Recognition (CVPR). IEEE, 2021. http://dx.doi.org/10.1109/cvpr46437.2021.00046.
Texto completoVarga, Matej. "ANALYSIS OF SATELLITE BASED GLOBAL GRAVITY FIELD MODELS ON GNSS/LEVELLING AND REFERENCE GRAVITY STATIONS WORLDWIDE". En 17th International Multidisciplinary Scientific GeoConference SGEM2017. Stef92 Technology, 2017. http://dx.doi.org/10.5593/sgem2017/22/s09.013.
Texto completoDaniels, R. y C. Green. "Production and Use of Global Topography Models in Gravity Compilations". En 57th EAEG Meeting. Netherlands: EAGE Publications BV, 1995. http://dx.doi.org/10.3997/2214-4609.201409303.
Texto completod, Luigi y Michela Costa. "Global instability analysis of 2D liquid sheets flow under gravity". En 2nd AIAA, Theoretical Fluid Mechanics Meeting. Reston, Virigina: American Institute of Aeronautics and Astronautics, 1998. http://dx.doi.org/10.2514/6.1998-2596.
Texto completoWang*, Meng, Junlu Wang y Changli Yao. "Discussion on the resolution of the global satellite gravity database". En International Geophysical Conference, Qingdao, China, 17-20 April 2017. Society of Exploration Geophysicists and Chinese Petroleum Society, 2017. http://dx.doi.org/10.1190/igc2017-072.
Texto completoCheyney, Samuel, Kirsten Fletcher, Chris Green y Simon Campbell. "New global lake gravity from advances in satellite altimetry processing". En SEG Technical Program Expanded Abstracts 2017. Society of Exploration Geophysicists, 2017. http://dx.doi.org/10.1190/segam2017-17732561.1.
Texto completoInformes sobre el tema "Gravità globale"
Newell, Steven W. Global Takfiri Radicalization: A Center of Gravity Deconstruction. Fort Belvoir, VA: Defense Technical Information Center, octubre de 2010. http://dx.doi.org/10.21236/ada535571.
Texto completoDekle, Robert, Jonathan Eaton y Samuel Kortum. Global Rebalancing with Gravity: Measuring the Burden of Adjustment. Cambridge, MA: National Bureau of Economic Research, marzo de 2008. http://dx.doi.org/10.3386/w13846.
Texto completoEthridge, Joe E. y Jr. Center of Gravity Determination in the Global War on Terrorism. Fort Belvoir, VA: Defense Technical Information Center, mayo de 2004. http://dx.doi.org/10.21236/ada423285.
Texto completoSmart, Cheryl L. The Global War on Terror: Mistaking Ideology as the Center of Gravity. Fort Belvoir, VA: Defense Technical Information Center, julio de 2005. http://dx.doi.org/10.21236/ada435894.
Texto completoHaberkem, John L. The Global War on Terrorism: Idealogy as its Strategic Center of Gravity. Fort Belvoir, VA: Defense Technical Information Center, marzo de 2004. http://dx.doi.org/10.21236/ada423887.
Texto completoReilly, James. A Strategic Level Center for Gravity Analysis on the Global War on Terrorism. Fort Belvoir, VA: Defense Technical Information Center, abril de 2002. http://dx.doi.org/10.21236/ada401641.
Texto completoMassotti, Luca, Günther March y Ilias Daras. Next Generation Gravity Mission as a Mass-change And Geosciences International Constellation (MAGIC) Mission Requirements Document. Editado por Roger Haagmans y Lucia Tsaoussi. European Space Agency, octubre de 2020. http://dx.doi.org/10.5270/esa.nasa.magic-mrd.2020.
Texto completoMetzger, E. J., Robert C. Rhodes, Dong S. Ko y Harley E. Hurlburt. Validation Test Report for OCEANS 1.0: The 1/40 Global, Reduced Gravity NRL Layered Ocean Model. Fort Belvoir, VA: Defense Technical Information Center, junio de 1998. http://dx.doi.org/10.21236/ada352049.
Texto completoRoland-Holst, David, Kamalbek Karymshakov, Burulcha Sulaimanova y Kadyrbek Sultakeev. ICT, Online Search Behavior, and Remittances: Evidence from the Kyrgyz Republic. Asian Development Bank Institute, diciembre de 2022. http://dx.doi.org/10.56506/fepw3647.
Texto completoKeen, C. E., K. Dickie, L. T. Dafoe, T. Funck, J. K. Welford, S A Dehler, U. Gregersen y K J DesRoches. Rifting and evolution of the Labrador-Baffin Seaway. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321854.
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