標(biāo)題: Titlebook: Geoid Determination; Theory and Methods Fernando Sansò,Michael G. Sideris Book 2013 Springer-Verlag Berlin Heidelberg 2013 [打印本頁(yè)] 作者: 根深蒂固 時(shí)間: 2025-3-21 16:06
書目名稱Geoid Determination影響因子(影響力)
作者: 巡回 時(shí)間: 2025-3-21 22:39
Combination of Heightse provided and more importantly an approach for the assessment of selected models is described in detail. These techniques are supported by numerical examples with real data sets (in Canada and Switzerland). Finally, it should be noted that this chapter is an abridged version of Fotopoulos (2003) an作者: 無(wú)能力之人 時(shí)間: 2025-3-22 03:37 作者: 仇恨 時(shí)間: 2025-3-22 07:21 作者: laparoscopy 時(shí)間: 2025-3-22 08:45
Versuchseierichtungen und Messverfahren,e start with the gravitation law in Sect. 1.2, we clarify what is a gravitation field, in particular for an extended body, and we prove that this is a conservative or potential field (Sect. 1.3), i.e., the vector field of gravitational accelerations can be expressed as the gradient of a potential. S作者: harbinger 時(shí)間: 2025-3-22 15:23 作者: harbinger 時(shí)間: 2025-3-22 17:19 作者: Albumin 時(shí)間: 2025-3-22 23:45
https://doi.org/10.1007/978-3-476-04281-1quasi-geoid modeling. Terrain and bathymetry models of high-resolution and accuracy are used in order to provide the high-frequency content of the gravity field spectrum through the available mass reduction methods (e.g., terrain corrections, simple and refined Bouguer effects, residual terrain mode作者: 得罪 時(shí)間: 2025-3-23 02:45 作者: Conducive 時(shí)間: 2025-3-23 07:39
https://doi.org/10.1007/978-3-663-09689-4lution integrals involved in geoid determination. An attempt was made to make this document as self-contained as possible for the benefit of readers inexperienced in spectral methods. Therefore, the Fourier transform and its properties are presented in the appendix following the chapter (Appendix A)作者: 未開(kāi)化 時(shí)間: 2025-3-23 10:50 作者: meditation 時(shí)間: 2025-3-23 15:01
Agrarwissenschaft und Agrarpolitikf geodesy in spaces of harmonic functions is quite justified. More precisely, from the mathematical point of view we are interested in a situation in which . is an open, simply connected bounded set, with a relatively smooth boundary . and . (the complement of the closure of .) is simply connected t作者: SPURN 時(shí)間: 2025-3-23 18:20
https://doi.org/10.1007/978-3-322-88935-5a modern mathematical form. Yet the same item has been treated in the past by different authors leading to numerical solutions, transforming the problem into integral equations, which are still applied in some cases. This matter is summarized in Sect. 14.2 from the historical point of view.作者: floodgate 時(shí)間: 2025-3-23 23:16
Pathologische Physiologie der Nierenfunktion harmonic coefficients. With the mathematical details having been presented in . of Part I of this book, the focus here is on the main concepts and considerations involved in the design and in the choice of alternative techniques and strategies that can be used to develop GGMs.作者: 受辱 時(shí)間: 2025-3-24 06:22
https://doi.org/10.1007/978-3-322-95962-1uthern Pacific Ocean the distance between surveys lines are several hundred kilometres thus only resolving signals of twice that distance. Satellite altimetry can provide information of the height of the oceans over nearly 60% of the Earth surface.作者: 粗魯?shù)娜?nbsp; 時(shí)間: 2025-3-24 07:46
https://doi.org/10.1007/978-3-322-88935-5a modern mathematical form. Yet the same item has been treated in the past by different authors leading to numerical solutions, transforming the problem into integral equations, which are still applied in some cases. This matter is summarized in Sect. 14.2 from the historical point of view.作者: aneurysm 時(shí)間: 2025-3-24 14:03 作者: Alopecia-Areata 時(shí)間: 2025-3-24 15:18 作者: Suggestions 時(shí)間: 2025-3-24 20:43 作者: 路標(biāo) 時(shí)間: 2025-3-25 01:25 作者: 固執(zhí)點(diǎn)好 時(shí)間: 2025-3-25 04:16 作者: Resistance 時(shí)間: 2025-3-25 07:53 作者: 軟弱 時(shí)間: 2025-3-25 15:31 作者: Minikin 時(shí)間: 2025-3-25 17:22
Verfassungsrechtliche Betrachtungsweise,The chapter is devoted to the construction and manipulation of so-called ..作者: 使苦惱 時(shí)間: 2025-3-25 22:27 作者: 有說(shuō)服力 時(shí)間: 2025-3-26 03:06 作者: 內(nèi)疚 時(shí)間: 2025-3-26 05:15 作者: entice 時(shí)間: 2025-3-26 11:58
Observables of Physical Geodesy and Their Analytical RepresentationAs we have shown in Chap. 1, the gravity potential . can be split into a known normal potential . plus the anomalous potential .; thus knowing . means knowing ..作者: 助記 時(shí)間: 2025-3-26 15:17 作者: Stricture 時(shí)間: 2025-3-26 18:23 作者: Offensive 時(shí)間: 2025-3-26 22:10 作者: 胰臟 時(shí)間: 2025-3-27 03:11
The Analysis of Geodetic Boundary Value Problems in Linear formAssume that . is a smooth surface, in the sense explained in Sect. 13.2, and that there is a function .(.) harmonic in . (the exterior of .), regular at infinity, and we have performed a very large number of measurements that can be expressed as functionals of .(.) at every point . ∈ .. then one can attempt to determine .(.) by solving the BVP .作者: 故意 時(shí)間: 2025-3-27 09:01
The Forward Modelling of the Gravity Fielde start with the gravitation law in Sect. 1.2, we clarify what is a gravitation field, in particular for an extended body, and we prove that this is a conservative or potential field (Sect. 1.3), i.e., the vector field of gravitational accelerations can be expressed as the gradient of a potential. S作者: 反對(duì) 時(shí)間: 2025-3-27 12:29 作者: Phonophobia 時(shí)間: 2025-3-27 17:22
Geoid Determination by 3D Least-Squares Collocationmented by the GRAVSOFT Fortran programs is described. The software also implements the remove-restore method so that gravity variations outside the region of computation are accounted for by subtracting the contribution of an Earth Gravity Model (EGM) and so that statistical homogenisation is achiev作者: Archipelago 時(shí)間: 2025-3-27 20:10
Topographic Reductions in Gravity and Geoid Modelingquasi-geoid modeling. Terrain and bathymetry models of high-resolution and accuracy are used in order to provide the high-frequency content of the gravity field spectrum through the available mass reduction methods (e.g., terrain corrections, simple and refined Bouguer effects, residual terrain mode作者: 啞巴 時(shí)間: 2025-3-28 00:21 作者: 豐滿有漂亮 時(shí)間: 2025-3-28 04:03 作者: deadlock 時(shí)間: 2025-3-28 06:42
Combination of Heightsrevious chapters, only a brief introduction to the theoretical issues is included along with some insight into why combining geoid, orthometric and ellipsoidal height data is relevant and important on both regional and global scales. The next section is devoted to a detailed outline of a computation作者: 酷熱 時(shí)間: 2025-3-28 14:11
On Potential Theory and HS of Harmonic Functionsf geodesy in spaces of harmonic functions is quite justified. More precisely, from the mathematical point of view we are interested in a situation in which . is an open, simply connected bounded set, with a relatively smooth boundary . and . (the complement of the closure of .) is simply connected t作者: inundate 時(shí)間: 2025-3-28 16:00 作者: adduction 時(shí)間: 2025-3-28 19:05 作者: 小母馬 時(shí)間: 2025-3-29 02:50
Geoid Determination by 3D Least-Squares Collocationed by removing the contribution of topographic short wavelength features. It is also described how LSC may be used to determine parameters like a height datum off-set or to detect possible gross errors. Examples using data from New Mexico, USA, illustrates the use of the method.作者: amygdala 時(shí)間: 2025-3-29 04:43
Geoid Determination by FFT Techniquesnexperienced in spectral methods. Therefore, the Fourier transform and its properties are presented in the appendix following the chapter (Appendix A), and reference is made to the particular formulas and properties employed in geoid determination.作者: AMEND 時(shí)間: 2025-3-29 11:11 作者: 無(wú)瑕疵 時(shí)間: 2025-3-29 14:19
https://doi.org/10.1007/978-3-476-04281-1s. The high-frequency contribution of the topographic and bathymetric effects to gravity-field related quantities (e.g., gravity anomalies, gravity disturbances, geoid undulations, deflections of the vertical, gravity gradients) is primarily due to the strong correlation of the short-wavelength gravity features with topography and bathymetry.作者: 生銹 時(shí)間: 2025-3-29 18:29 作者: chisel 時(shí)間: 2025-3-29 22:34 作者: Barrister 時(shí)間: 2025-3-30 00:25 作者: 相反放置 時(shí)間: 2025-3-30 04:11 作者: antiandrogen 時(shí)間: 2025-3-30 12:08 作者: 山羊 時(shí)間: 2025-3-30 14:28
Agrarwissenschaft und Agrarpolitikwhich . is an open, simply connected bounded set, with a relatively smooth boundary . and . (the complement of the closure of .) is simply connected too. Let us note explicitly that this prevents . from having holes in it or even single points removed.作者: 叢林 時(shí)間: 2025-3-30 16:43
Book 2013y the International Geoid Serivice of the International Association of Geodesy. It consolidates, unifies, and streamlines this material in a unique way not covereed by the few other books that exist on this subjext. More specifically, the book presents (for the first time in a single volume) the the作者: 現(xiàn)代 時(shí)間: 2025-3-30 22:32 作者: Glaci冰 時(shí)間: 2025-3-31 04:31
