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Titlebook: Intrinsic Geodesy; Antonio Marussi Book 1985 Springer-Verlag Berlin · Heidelberg 1985 Geod?sie.Orbit.geodesy.satellite

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書目名稱Intrinsic Geodesy
編輯Antonio Marussi
視頻videohttp://file.papertrans.cn/474/473252/473252.mp4
圖書封面Titlebook: Intrinsic Geodesy;  Antonio Marussi Book 1985 Springer-Verlag Berlin · Heidelberg 1985 Geod?sie.Orbit.geodesy.satellite
描述The science of Geodesy has undergone far-reaching changes in the last half century. The impact of new technology, from electromag- netic distance measurements to the use of artificial satellites, has been great, and is still largely to be felt. These changes have forced the practitioners of the ancient art of Earth measurement to alter their way of thinking about the space that surrounds us, something fundamentally more difficult than absorbing a new technology. A key influence in this modem change in geodetic thinking has been the work of Antonio Marussi, in his scientific publications from 1947 onwards, through his students and collaborators at the Uni- versity of Trieste, and in the series of symposia on three-dimensional Geodesy which he organised with his great friend and collaborator, Martin Hotine. His influence on the latter, stemming from their first meeting at the General Assembly of the International Association of Geodesy in Oslo in 1948, was remarkable in itself, leading as it did to the ultimate publication of Hotine‘s Mathematical Geodesy in 1969.
出版日期Book 1985
關(guān)鍵詞Geod?sie; Orbit; geodesy; satellite
版次1
doihttps://doi.org/10.1007/978-3-642-70243-3
isbn_softcover978-3-642-70245-7
isbn_ebook978-3-642-70243-3
copyrightSpringer-Verlag Berlin · Heidelberg 1985
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Generalized Legendre Expansions for Any Curve Whatever, Traced Out Upon Any Surface Whateverhe ellipsoid of rotation, which permit us to determine the geographic coordinates .. and λ. (latitude and longitude) of the extremity .. of the geodesic of finite length ., and of azimuth α. at .., if we know the geographic coordinates .. and λ. of the other extremity .., and the azimuth of the geodesic also at ..
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The Tidal Field of a Planet and the Related Intrinsic Reference Systemsy, or (2) in inertial motion around the planet, are the so-called tidal accelerations; they arise from the lack of uniformity of the gravity field. In case (1), g includes the centrifugal acceleration due to the rotation of the planet, and in case (2) the Newtonian gravitational acceleration only.
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Principles of Intrinsic Geodesy Applied to the Field of Somiglianach are suggested by cosmological or mechanical theories, and are confirmed by experiment to be approximately the equilibrium figure of a particular level surface of the Earth’s gravity field, the geoid.
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The First Fundamental Problem of Geodesy Developed for the Field of Somiglianaf the end . of a geodesic of finite length . drawn out on a surface ., and its azimuth at ., where the geographic coordinates .. and λ. at its other end .. are known, as well as the azimuth .. at this latter point.
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Some Remarks on the Use of Conformal Representations in Three-Dimensional Geodesyto my colleague Grossmann on the occasion of his 70th birthday, I have thought that a theme from . (Intrinsic Geodesy) might fulfil this aim. I have devoted myself for so many years to this subject, but its latest developments have eluded me and have been followed up by other distinguished colleagues.
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