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A recipe for multi-metric gravity / マルチメトリック重力理論の構成法Nomura, Kouichi 23 March 2015 (has links)
京都大学 / 0048 / 新制・課程博士 / 博士(理学) / 甲第18793号 / 理博第4051号 / 新制||理||1583(附属図書館) / 31744 / 京都大学大学院理学研究科物理学・宇宙物理学専攻 / (主査)教授 田中 貴浩, 教授 中村 卓史, 教授 高柳 匡 / 学位規則第4条第1項該当 / Doctor of Science / Kyoto University / DFAM
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On the gravity anomaly above the earth and its attenuation /Madkour, Mohamed Fathi January 1966 (has links)
No description available.
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Non-global recovery of gravity anomalies from a combination of terrestrial and satellite altimetry data /Gopalapillai, S. January 1974 (has links)
No description available.
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Mean gravity anomaly prediction from terrestrial gravity data and satellite altimetry data /Smith, Glenn Nils January 1974 (has links)
No description available.
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A gravity anomaly simulator with reflected light /Liard, Jacques O. January 1976 (has links)
No description available.
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A regional Bouguer gravity anomaly map of ArizonaWest, Robert Elmer, 1938- January 1972 (has links)
No description available.
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Toward a theory of observationCarney, Daniel Joseph, Jr. 06 November 2014 (has links)
Quantum mechanics is usually formulated in terms of a single Hilbert space and observables are defined as operators on this space. Attempts to describe entire spacetimes and their resident matter in this way often encounter paradoxes. For example, it has been argued that an observer falling into a black hole may be able to witness deviations from unitary, violations of semi-classical quantum field theory, and the like. This thesis argues that the essential problem is the insistence on the use of a single, global Hilbert space, because in general it may be that a physical observer cannot causally probe all of the information described by this space due to the presence of horizons. Instead, one could try to define unitary quantum physics directly in terms of the information causally accessible to particular observers. This thesis makes steps toward a systematization of this idea. Given an observer on a timelike worldline, I construct coordinates which (in good cases) cover precisely the set of events to which she can send and then receive a signal. These coordinates have spatial sections parametrized by her proper time, and the metric manifestly encodes the equivalence principle in the sense that it is flat along her worldline. To describe the quantum theory of fields according to these observers, I define Hilbert spaces in terms of field configurations on these spatial sections and show how to implement unitary time-evolution along proper time. I explain how to compare the observations of a pair of observers, and how to obtain the description according to some particular observer given some a priori global description. In this sense, the program outlined here constructs a manifestly unitary description of the events which the observer can causally probe. I give a number of explicit examples of the coordinates, and show how the quantum theory works for a uniformly accelerated observer in flat spacetime and for an inertial (co-moving) observer in an inflating universe. / text
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Isostatic and Bouguer gravity anomalies along the inside passage of Alaska and British ColumbiaBanks, Ernest Robey 23 August 1968 (has links)
Graduation date: 1969
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Splines and local approximation of the earth's gravity fieldVan Gysen, Hermanus Gerhardus January 1988 (has links)
Bibliography: pages 214-220. / The Hilbert space spline theory of Delvos and Schempp, and the reproducing kernel theory of L. Schwartz, provide the conceptual foundation and the construction procedure for rotation-invariant splines on Euclidean spaces, splines on the circle, and splines on the sphere and harmonic outside the sphere. Spherical splines and surface splines such as multi-conic functions, Hardy's multiquadric functions, pseudo-cubic splines, and thin-plate splines, are shown to be largely as effective as least squares collocation in representing geoid heights or gravity anomalies. A pseudo-cubic spline geoid for southern Africa is given, interpolating Doppler-derived geoid heights and astro-geodetic deflections of the vertical. Quadrature rules are derived for the thin-plate spline approximation (over a circular disk, and to a planar approximation) of Stokes's formula, the formulae of Vening Meinesz, and the L₁ vertical gradient operator in the analytical continuation series solution of Molodensky's problem.
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The IGSN 71 residual Bouguer gravity anomaly map of ArizonaLysonski, Joseph C. (Joseph Charles) January 1980 (has links)
No description available.
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