共查询到20条相似文献，搜索用时 31 毫秒
1.
Pavel Peška Reviewers J. Švancara Reviewers K. Pěč 《Studia Geophysica et Geodaetica》1989,33(4):405-408
Summary This short note contributes to the methods of computing the bounds on some properties of the source of measured data. 相似文献
2.
Earthquake sources exhibiting anelastic volume changes are studied in a gravitating earth. The excitation of seismic displacement fields by such sources cannot be fully described by a moment tensor.The effect of gravity manifests itself through the action of a buoyancy force at the source, which is compensated by a continuous distribution of volume forces through the earth.An inversion scheme which does not take into account these gravitational forces may lead to a pseudo-precursive action in the source and to an erroneous source characterisation. 相似文献
3.
A processing strategy and the corresponding software architecture for the processing of GOCE (Gravity field and steady-state Ocean Circulation Explorer) observables is presented and described, with the major objective to compute a high-accuracy, high-resolution spherical harmonic model of the Earth's gravity field. The combination of two numerical solution strategies, i.e. the rigorous solution of the corresponding large normal equation systems applying parallel processing (on a PC cluster) as the core solver, and the fast semianalytic approach as a quick-look gravity field analysis (QL-GFA) tool, is proposed. Such a method fusion benefits from the advantages of the individual components: the rigorous inversion of the system providing also the full variance-covariance information, and the quickness enabling the consecutive production of intermediate gravity field solutions, for the purpose to analyse partial and incomplete data sets and to derive a diagnosis of the performance of the GOCE measurement system. The functionality and operability of the individual components are demonstrated in the framework of a closed loop simulation, which is based on a realistic mission scenario both in terms of the orbit configuration and the coloured measuring noise. Special concern is given to the accuracy of the recovered coefficients, the numerical behaviour, the required computing time, and the particular role of the individual modules within the processing chain. In the case of the core solver, it is demonstrated that the assembling and rigorous solution of large normal equation systems can be handled by using Beowulf clusters within a reasonable computing time. The application of the quick-look tool to partial data sets with short-term data gaps is demonstrated on the basis of several case studies. Additionally, the spectral analysis of the residuals of the adjustment is presented as a valuable tool for the verification of the noise characteristics of the GOCE gradiometer. 相似文献
4.
台风引起的重力扰动现象 总被引：3，自引：1，他引：2
山东省泰安台LaCoste-PET型重力仪安装以来,出现了几次固体潮“脉动加粗”的情况．用高通滤波进行信息分离后发现,“脉动加粗”与2008年登陆我国最强的３次台风发生时间有很好的对应．烟台SSQ-2型倾斜仪表现出与重力仪同步“脉动加粗”的特征,泰安台JCZ-1型地震仪在台风发生期间也观测到了“纺锤形”振幅加大的情况,台风信号卓越周期为3—7s．分析结果表明,重力仪及倾斜仪的这些异常变化均是台风引起的扰动,“扰动”信号的频率、幅度在重力仪的监测能力内．“扰动”的出现与台风发展强度、移动速度及地理位置有关． 相似文献
5.
A gravity network was established by a crew of gravity measurement in July, 1981, with three LCR gravimeters. The measurement
errors are less than 100 nm/s2. The detectable changes in gravity with time in the Beijing-Tianjin-Tangshan area are described.
The results show that the gravity has increased 1000 nm/s2 in Tianjin area where the ground has been subsiding at a rate of 7–8 cm/a and at the center of subsidence gravity has increased.
At other stations, such as Baodi, Tangerli, etc., gravity has also increased gradually, but with an amplitude smaller than
that of Tianjin. In the area surveyed gravity tendentiously decreases from south-east to north-east. 相似文献
6.
Three-Dimensional Gravity Modeling In All Space 总被引：11，自引：2，他引：9
We review available analytical algorithms for the gravity effect and gravity gradients especially the vertical gravity gradient due to a right rectangular prism, a right polygonal prism, and a polyhedron. The emphasis is placed on an investigation of validity, consistency, and especially singularities of different algorithms, which have been traditionally proposed for calculation of the gravity effect on ground (or outside anomalous bodies), when they are applied to all points in space. The rounding error due to the computer floating point precision is estimated. The gravity effect and vertical gradient of gravity in three dimensions caused by a cubic model are calculated by different types of algorithms. The reliability of algorithms for the calculation of gravity of a right polygonal prism and a polyhedron is further verified by using a regular polygonal prism approximating a vertical cylinder and a regular polyhedron approximating a sphere, respectively. By highlighting Haáz-Jung-Plouff and Okabe-Steiner-Zilahi-Sebess' formulae for a right rectangular prism, Plouff's algorithm for a right polygonal prism, and Gouml;tze and Lahmeyer's algorithm for a polyhedron and removing their singularities, we demonstrate that these formulae and algorithms can be used to model the gravity anomaly and its vertical gradient at all possible computation positions. 相似文献
7.
Mapping Buried Bedrock Topography with Gravity 总被引：3，自引：0，他引：3
8.
The ALOMAR SOUSY Radar operated at 53.5 MHz has been used in a five-beam configuration to study dynamical processes at gravity wave periods in the summer polar mesosphere. A case study of a gravity wave with a period of about 9 min is presented and analysed in some detail. The three-dimensional wave number vector is determined from the phase information of the 9-min velocity oscillations obtained in all beam directions and all range gates. The horizontal wavelengths in the north and east direction are estimated to be about 60 and 50 km, respectively. The echo power variations, simultaneously observed at different beam pointing positions, are investigated using cross-correlation analysis. The results show that these wave-associated variations lead to horizontal and vertical deformation of the echoing layers. The horizontal wavelength in the north-south direction, derived from the echo power modification, is in good agreement with the one obtained from the velocity analysis. 相似文献
9.
10.
11.
利用经过去相关滤波处理的GRACE时变重力场模型获得了青藏高原东缘2003—2012年的卫星年重力变化图像,并针对该区域近年发生的三次特大地震,结合震前及震后月重力场变化图像,分析与强震有关的卫星重力场变化特征。从区域年重力变化图像可以看出,三次大震均发生在年重力变化较低的时段内,震前小幅值变化可能是地震发生的中短期前兆;从汶川地震和玉树地震发生前后的月重力场变化图像可以发现,发震前后断层附近的重力变化模式发生变化,这可能印证了震后位场变化恢复理论;从汶川地震前后的龙门山断层附近点上的周重力变化趋势可以明显发现,汶川地震发生（第20周）后近9周的时间,断层东西侧呈现了相反的重力变化特征,这可能是对震后壳幔物质调整过程的反映。 相似文献
12.
Discussion of Mean Gravity Along the Plumbline 总被引：2，自引：1，他引：1
According to the definition of the orthometric height, the mean value of gravity along the plumbline between the Earth's surface and the geoid is defined in an integral sense. In Helmert's (1890) definition of the orthometric height, a linear change of the gravity with depth is assumed. The mean gravity is determined so that the observed gravity at the Earth's surface is reduced to the approximate mid-point of the plumbline using Poincaré-Prey's gravity gradient. Niethammer (1932) and later Mader (1954) took into account the mean value of the gravimetric terrain correction within the topography considering the constant topographical density distribution along the plumbline (for more details see Heiskanen and Moritz, 1967). Vaníek et al. (1995) included the effect of the lateral variation of the topographical density into the definition of Helmert's orthometric height. Recently, Hwang and Hsiao (2003) discussed the influence of the vertical gradient of disturbing gravity on the orthometric heights. In this paper, the mean integral value of gravity along the plumbline within the topography is defined so that the actual topographical density distribution and the change of the disturbing gravity with depth are taken into account. Based on the definition of the mean gravity, the relation between the orthometric and normal heights is discussed. 相似文献
13.
The National Survey and Cadastre - Denmark (KMS) has for several years produced gravity anomaly maps over the oceans derived from satellite altimetry. During the last four years, KMS has also conducted airborne gravity surveys along the coast of Greenland dedicated to complement the existing onshore gravity coverage and fill in new data in the very-near coastal area, where altimetry data may contain gross errors. The airborne surveys extend from the coastline to approximately 100 km offshore, along 6000 km of coastline. An adequate merging of these different data sources is important for the use of gravity data especially, when computing geoid models in coastal regions.The presence of reliable marine gravity data for independent control offers an opportunity to study procedures for the merging of airborne and satellite data around Greenland. Two different merging techniques, both based on collocation, are investigated in this paper. Collocation offers a way of combining the individual airborne gravity observation with either the residual geoid observations derived from satellite altimetry or with gravity derived from these data using the inverse Stokes method implemented by Fast Fourier Transform (FFT). 相似文献
14.
Roland Klees 《Surveys in Geophysics》1993,14(4-5):419-432
The Boundary Element Method (BEM), a numerical technique for solving boundary integral equations, is introduced to determine the earth's gravity field. After a short survey on its main principles, we apply this method to the fixed gravimetric boundary value problem (BVP), i.e. the determination of the earth's gravitational potential from measurements of the intensity of the gravity field in points on the earth's surface. We show how to linearize this nonlinear BVP using an implicit function theorem and how to transform the linearized BVP into a boundary integral equation using the single layer representation. A Galerkin method is used to transform the boundary integral equation using the single layer representation. A Galerkin method is used to transform the boundary integral equation into a linear system of equations. We discuss the major problems of this approach for setting up and solving the linear system. The BVP is numerically solved for a bounded part of the earth's surface using a high resolution reference gravity model, measured gravity values of high density, and a 50 50 m2 digital terrain model to describe the earth's surface. We obtain a gravity field resolution of 1 1 km2 with an accuracy of the order 10–3 to 10–4 in about 1 CPU-hour on a Siemens/Fujitsu SIMD vector pipeline machine using highly sophisticated numerical integration techniques and fast equation solvers. We conclude that BEM is a powerful numerical tool for solving boundary value problems and may be an alternative to classical geodetic techniques. 相似文献
15.
16.
17.
利用2018年庐山重力短基线场绝对重力和相对重力观测资料,基于绝对重力控制下的相对重力联测方式对庐山基线场的稳定性进行了分析。结果表明：庐山基线场2015～2018年测段重力变化为-11.6～13.4μGal、均值-0.962μGal,较小的重力变化表明庐山短基线重力场较稳定;2000～2018年测段重力变化为-39～33.5μGal、均值-0.275μGal,总体以G16测点为界呈分化特征,上山侧（G16～JZ04）重力变化较平缓（约-3 μGal）,下山侧（G03～G16）因G04、G14测点重力值变化显著（分别为-24.95、-18.5μGal）,导致相邻测段重力变化剧烈;测段重力变化与段差比值（B）为1.19×10-4～3.58×10-3;庐山及其周边地区由地表垂直运动引起的重力变化速率为0.7543±0.16μGal/a;近期研究区地震活动性呈震级小、沿断裂带集中分布特征;重力变化对相对重力仪一次项系数标定结果影响较大（正比于B值）,对校正精度影响小,利用以往重力观测成果进行一次项系数标定时,绝对重力测段JZ02～JZ04误差影响小于最大重力段差测段,定期维护和复测是保障高精度重力短基线场的有效途径。 相似文献
18.
19.
卫星重力探测技术的发展 总被引：2，自引：0，他引：2
在地球物理勘探领域中,人造地球卫星的发射为重力测量提供了新的途径。与以往探测重力的手段相比,重力卫星的发射大大改善了人们对地球重力场的认识,随着CHAMP、GRACE和GOCE卫星的发射,将把现有静态中长波部分重力场的精度提高1—2个数量级,并提供长波部分重力场随时间变化的信息。卫星重力学对我国的基础测绘服务和国防建设有着重要的实用价值。 相似文献
20.
Subsalt exploration for oil and gas is attractive in regions where 3D seismic depth-migration to recover the geometry of a salt base is difficult. Additional information to reduce the ambiguity in seismic images would be beneficial. Gravity data often serve these purposes in the petroleum industry. In this paper, the authors present an algorithm for a gravity inversion based on Tikhonov regularization and an automatically regularized solution process. They examined the 3D Euler deconvolution to extract the best anomaly source depth as a priori information to invert the gravity data and provided a synthetic example. Finally, they applied the gravity inversion to recently obtained gravity data from the Bandar Charak (Hormozgan, Iran) to identify its subsurface density structure. Their model showed the 3D shape of salt dome in this region. 相似文献