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作者: Nonchalant    時(shí)間: 2025-3-21 17:52
書目名稱Gravity, Gradiometry, and Gravimetry影響因子(影響力)




書目名稱Gravity, Gradiometry, and Gravimetry影響因子(影響力)學(xué)科排名




書目名稱Gravity, Gradiometry, and Gravimetry網(wǎng)絡(luò)公開度




書目名稱Gravity, Gradiometry, and Gravimetry網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Gravity, Gradiometry, and Gravimetry被引頻次




書目名稱Gravity, Gradiometry, and Gravimetry被引頻次學(xué)科排名




書目名稱Gravity, Gradiometry, and Gravimetry年度引用




書目名稱Gravity, Gradiometry, and Gravimetry年度引用學(xué)科排名




書目名稱Gravity, Gradiometry, and Gravimetry讀者反饋




書目名稱Gravity, Gradiometry, and Gravimetry讀者反饋學(xué)科排名





作者: PANT    時(shí)間: 2025-3-22 00:15
Kishan Gopal Ramawat,Jean-Michel Mérillonns with additional local eccenters. The gravity stations shall partly serve as stations of the . proposed by the ., and will also provide gravimeter calibration lines in the countries involved. By connection to the national gravity networks, I.G.S.N.71 in South America will be improved and densified
作者: Hiatus    時(shí)間: 2025-3-22 03:01
Natural Products as Enzyme Inhibitorsds its importance in monitoring the microgravity environment, examining the gravity field continuation theory, improving the analyses subjected orbital vehicle to gravitational force and exactly testing the law of gravity.
作者: 隱士    時(shí)間: 2025-3-22 06:13
Gordon M. Cragg,David J. Newmany on it a GPS (Global Positioning System) receiver for precise orbit tracking. In doing this in a satellite of relatively low altitude (650 km) in polar orbit around the Earth, we create a system that will also, as an unexpected “coexperiment”, improve knowledge of the Earth’s gravity field by a fac
作者: 閑聊    時(shí)間: 2025-3-22 10:20
Nanjoo Suh,Hubert Maehr,David Augeri) derived from the Ohio State University 1°×1° gravity anomaly data. PTGF-4 was computed using satellite tracking data and altimeter crossover data, whereas PTGF-4A was determined using these data sets as well as direct altimeter data and surface gravity data. The estimated parameters for PTGF-4A in
作者: 可忽略    時(shí)間: 2025-3-22 15:52

作者: 可忽略    時(shí)間: 2025-3-22 17:28
Martha A. Mutschler,William M. Wintermantel, 1987. The distribution of the hypocentres suggests the existence of thrust faulting across the Toyama Trough off Noto Peninsula according to the seismic data catalogue of Japan Meteorological Agency. Therefore, this area of the expected plate boundary was selected as a target of precise survey, an
作者: Volatile-Oils    時(shí)間: 2025-3-23 01:16
The Investigation of Gravity Variations Near a Pumped-Storage Reservoir in North Walese.g. uncertainty in lake geometry, gravimeter calibration and elastic properties of the local rock). The uncertainty in both the permeability and porosity of the rock in the vicinity of the gravimeter is found to be the dominant limiting factor in the overall accuracy of the experiment.
作者: anchor    時(shí)間: 2025-3-23 05:10
Large-Scale Absolute Gravity Control in Brazilns with additional local eccenters. The gravity stations shall partly serve as stations of the . proposed by the ., and will also provide gravimeter calibration lines in the countries involved. By connection to the national gravity networks, I.G.S.N.71 in South America will be improved and densified
作者: 傳授知識(shí)    時(shí)間: 2025-3-23 09:22

作者: 揮舞    時(shí)間: 2025-3-23 10:15
Contribution of the Gravity Probe B Mission to Geodesy and to Satellite Navigationy on it a GPS (Global Positioning System) receiver for precise orbit tracking. In doing this in a satellite of relatively low altitude (650 km) in polar orbit around the Earth, we create a system that will also, as an unexpected “coexperiment”, improve knowledge of the Earth’s gravity field by a fac
作者: 煞費(fèi)苦心    時(shí)間: 2025-3-23 15:23
An Improved Model for the Earth’s Gravity Field) derived from the Ohio State University 1°×1° gravity anomaly data. PTGF-4 was computed using satellite tracking data and altimeter crossover data, whereas PTGF-4A was determined using these data sets as well as direct altimeter data and surface gravity data. The estimated parameters for PTGF-4A in
作者: 飲料    時(shí)間: 2025-3-23 18:27
A New Geopotential Model Tailored to Gravity Data in Europemgal to 6.0 mgal for OSU86F resp. IFE88E2. The magnitude of residual point free-air anomalies relative to OSU86F and IFE88E2 were evaluated in 1495 points in Scandinavia. The RMS values of the differences were 23.4 mgal and 18.5 mgal respectively. Especially comparisons of the two models with GPS/le
作者: 無能力之人    時(shí)間: 2025-3-24 01:19

作者: CESS    時(shí)間: 2025-3-24 03:11

作者: FEMUR    時(shí)間: 2025-3-24 07:27
Least-Squares Collocation Error Estimates in a Test of Newton’s Gravitational Lawhnique that was used to upward-continue ground data was least-squares collocation (LSC). The predicted standard deviation at 600 m above ground in the LSC estimate was significantly smaller than the observed discrepancy between the upward continuation estimate and the measured value. This indicates
作者: 歡樂東方    時(shí)間: 2025-3-24 11:22
Validation of the Inverse Square Law of Gravitation Using the Tower at Erie, Colorado, U.S.A.n, whose validity in the distance range of 10– 1000m has been repeatedly questioned during the last decade. Eckhardt et al (loc. cit.) and Romaides et al (1989) have interpreted their measurements on the 600m WTVD tower in North Carolina as evidence for non-Newtonian gravitation. This paper describe
作者: 經(jīng)典    時(shí)間: 2025-3-24 17:34

作者: 只有    時(shí)間: 2025-3-24 19:40

作者: GRACE    時(shí)間: 2025-3-25 02:34

作者: Enteropathic    時(shí)間: 2025-3-25 07:20
Large-Scale Absolute Gravity Control in Brazil comparative measurements at absolute and relative stations, the instrument has been employed for absolute gravity control in fundamental and geodynamic networks in central and northern Europe. At approximately 100 gravity determinations at about 60 different stations an average station precision of
作者: Host142    時(shí)間: 2025-3-25 08:08

作者: 字形刻痕    時(shí)間: 2025-3-25 14:15
Contribution of the Gravity Probe B Mission to Geodesy and to Satellite Navigationextremely important effects of Einstein’s general theory of relativity as observed with gyroscopes in Earth orbit. These are respectively the . exerted by a spinning body (the Earth) on an angular momentum vector (the set of gyroscopes), and the . resulting from the motion of the gyroscope in its or
作者: 良心    時(shí)間: 2025-3-25 17:17

作者: 離開真充足    時(shí)間: 2025-3-25 20:43

作者: paleolithic    時(shí)間: 2025-3-26 03:39
Gravity Field of Phobos and its Long Term Variationsobos boundary topography was established by Turner (197B), based on the Mariner 9 television pictures. Provided that Phobos is a homogeneous body, Sagitov et al. (1981), evaluated the Stokes parameters of the external gravitational field by numerical integration. An independent analytical approach b
作者: 半球    時(shí)間: 2025-3-26 05:49
“Feldgrav” A Data Bank System for High Precision Gravity ObservationsPASCAL. A data logging system allows automatic data collecting within the data bank system. The software runs on IBM compatible portable Personal computers (PC). The ad hoc status of the system is described, whereby special emphasis is given to the adjustment procedure. Advantages of the system are
作者: 枯萎將要    時(shí)間: 2025-3-26 10:37
Digital Compilation of Gravity Data Over the Japanese Islandshave many summits of 3,000 meters in elevation, comparable with the Alps. The length of the islands is about 2,000 km. The topographic relief is so great that roads are largely restricted to river courses, and large areas around high mountains remain difficult to access for gravity measurements.
作者: Restenosis    時(shí)間: 2025-3-26 15:31
Gravity Measurement on the Bottom of Toyama Trougha, 1983). The assumed boundary is located from Fossa Magna along the Toyama Trough, Sado Ridge, Okushiri Ridge towards the western egde of Okhotsk Sea (Fig.1). Some features of subducting slab, that is, thrust faulting, are observed by seismic profiling survey in several places along the line, (Naka
作者: 改正    時(shí)間: 2025-3-26 19:05

作者: Fierce    時(shí)間: 2025-3-26 23:34

作者: encyclopedia    時(shí)間: 2025-3-27 02:12
Natural Processes and Human Impactsfall. Although geodesy does use the only one unit for gravity, that of the acceleration. Technical physics, esp. mechanics need to distinguish the different meanings of gravity also by using the adequate unit in the SI system. In fact the intensity of the gravity field (the force acting on the unit
作者: 小教堂    時(shí)間: 2025-3-27 07:43
Charu Upadhyay,Sumit Kumar,Poonamhnique that was used to upward-continue ground data was least-squares collocation (LSC). The predicted standard deviation at 600 m above ground in the LSC estimate was significantly smaller than the observed discrepancy between the upward continuation estimate and the measured value. This indicates
作者: SEMI    時(shí)間: 2025-3-27 12:39
Philip W. Le Quesne,Robert H. Purdyn, whose validity in the distance range of 10– 1000m has been repeatedly questioned during the last decade. Eckhardt et al (loc. cit.) and Romaides et al (1989) have interpreted their measurements on the 600m WTVD tower in North Carolina as evidence for non-Newtonian gravitation. This paper describe
作者: 重畫只能放棄    時(shí)間: 2025-3-27 15:50

作者: 繁忙    時(shí)間: 2025-3-27 18:32

作者: prodrome    時(shí)間: 2025-3-27 21:58
Chris M. Farnet,Emmanuel Zazopoulosen tested in the laboratories of the Geophysical Division of the Geological Survey of Canada (GSC). This method involves a computer controlled apparatus which performs the measurements automatically as well as the preliminary analysis of the observations. The ground work to establish methodologies a
作者: Cabinet    時(shí)間: 2025-3-28 05:21
Kishan Gopal Ramawat,Jean-Michel Mérillon comparative measurements at absolute and relative stations, the instrument has been employed for absolute gravity control in fundamental and geodynamic networks in central and northern Europe. At approximately 100 gravity determinations at about 60 different stations an average station precision of
作者: HAVOC    時(shí)間: 2025-3-28 06:18
Natural Products as Enzyme Inhibitorslly now. Gravity gradiometry will be of great use for detecting the short wave component of the earth’s gravity gradient field. In this paper the necessity and possibility of carrying out the satellite gravity gradiometry and developing the ultra-sensitive gradiometer are discussed with regard to th
作者: 王得到    時(shí)間: 2025-3-28 10:35

作者: 斷言    時(shí)間: 2025-3-28 15:35
Nanjoo Suh,Hubert Maehr,David Augerih’s gravity field and other geophysical parameters from the combination of satellite ground based tracking data, satellite altimetry data, and the surface gravimetry data. The University of Texas Earth’s gravity field models, PTGF-4 and PTGF-4A, were determined from data sets collected for fifteen s
作者: chiropractor    時(shí)間: 2025-3-28 22:46
Nattakorn Kuncharoen,Somboon Tanasupawatgeoid computations show a strong slope (1.5 m/700 km) between Denmark and Norway. This slope was suspected to be caused by bad quality of the up to now available 6′ × 10′ gravity values for Scandinavia. Therefore an updated set of 0.5° × 0.5° mean free-air gravity anomalies was calculated for Scandi
作者: 小溪    時(shí)間: 2025-3-29 00:42

作者: thalamus    時(shí)間: 2025-3-29 04:02
https://doi.org/10.1007/978-3-642-54461-3PASCAL. A data logging system allows automatic data collecting within the data bank system. The software runs on IBM compatible portable Personal computers (PC). The ad hoc status of the system is described, whereby special emphasis is given to the adjustment procedure. Advantages of the system are
作者: 悶熱    時(shí)間: 2025-3-29 08:43
F. C. Pinto,J. R. Ascenso,M. J. U. Ferreirahave many summits of 3,000 meters in elevation, comparable with the Alps. The length of the islands is about 2,000 km. The topographic relief is so great that roads are largely restricted to river courses, and large areas around high mountains remain difficult to access for gravity measurements.
作者: opportune    時(shí)間: 2025-3-29 12:56
Martha A. Mutschler,William M. Wintermantela, 1983). The assumed boundary is located from Fossa Magna along the Toyama Trough, Sado Ridge, Okushiri Ridge towards the western egde of Okhotsk Sea (Fig.1). Some features of subducting slab, that is, thrust faulting, are observed by seismic profiling survey in several places along the line, (Naka
作者: VICT    時(shí)間: 2025-3-29 17:56
Climate Change: Equity and Sustainability,res solution is compared to robust-M-estimation. The data of a large scale geodynamic network in South America, of a local deformation net in Norway and of a very high precision indoor net are evaluated. The capabilities of robust estimation in these three cases with rather different accuracies is i
作者: Carbon-Monoxide    時(shí)間: 2025-3-29 22:30

作者: 痛苦一生    時(shí)間: 2025-3-30 00:08
Chris M. Farnet,Emmanuel Zazopoulosus which performs the measurements automatically as well as the preliminary analysis of the observations. The ground work to establish methodologies and analysis techniques was done on the gravity meter D-28 of the GSC.
作者: Ptosis    時(shí)間: 2025-3-30 07:53

作者: Small-Intestine    時(shí)間: 2025-3-30 09:59
Alka Swami,Rajni,Pragati Hemrajaniation campaigns (1988 and 1989) are given. Significant gravity changes up to 450 [nm sec.] between northwestern and southeastern stations are obtained. Vertical crustal movements or other physical processes however must be excluded as reasons. On the contrary we assume that the gravity changes reflect not well understood instrumental problems.
作者: gait-cycle    時(shí)間: 2025-3-30 13:01

作者: 議程    時(shí)間: 2025-3-30 18:45
https://doi.org/10.1007/978-981-99-6038-5ses, the density of water can be reliably predicted. This paper describes techniques aiming to determine all necessary corrections with a differential accuracy of 5 nm.s. over a 50 m vertical interval in order to exploit the 10 nm.s. accuracy available from LaCoste & Romberg gravity meters.
作者: Indebted    時(shí)間: 2025-3-30 22:01
Biswanath Dinda,Manikarna Dinda981) results. Unfortunately, due to many possible shortcomings of the Turner’s globe, results by Sagitov et al. (1981), as well as, by Bur?a et al. (1988; cannot be used for the correct representation of the Phobos external gravitational field.
作者: 向外才掩飾    時(shí)間: 2025-3-31 01:31
Climate Change: Equity and Sustainability,d gravity values are changed by one to two times their mean square error at maximum compared to the ordinary least squares solution. Outliers are routinely detected and their effect is reduced significantly. The complete procedure for the adjustment of high precision gravimetry with observations in different epochs is presented.
作者: Engulf    時(shí)間: 2025-3-31 06:26

作者: gusher    時(shí)間: 2025-3-31 10:25
Testing Newton’s Law in the Megget Water Reservoirses, the density of water can be reliably predicted. This paper describes techniques aiming to determine all necessary corrections with a differential accuracy of 5 nm.s. over a 50 m vertical interval in order to exploit the 10 nm.s. accuracy available from LaCoste & Romberg gravity meters.
作者: 繁榮地區(qū)    時(shí)間: 2025-3-31 17:05

作者: 謙虛的人    時(shí)間: 2025-3-31 19:09

作者: 預(yù)防注射    時(shí)間: 2025-3-31 23:01
Natural Processes and Human Impactsmass) with the unit N/kg is the generally needed quantity instead of the acceleration. Its use will be suggested also in geodesy and proper units in the SI system will be recommended for gravity potential, geopotential number etc.
作者: 簡(jiǎn)潔    時(shí)間: 2025-4-1 05:06
Charu Upadhyay,Sumit Kumar,Poonameither a possible violation of Newton’s law or a model error (bias). Although the LSC error estimates of gravity interpolation on the ground are shown to be quite reasonable, it is suggested that a terrain misrepresentation can invalidate the error estimates of upward continuation.
作者: 修正案    時(shí)間: 2025-4-1 07:48

作者: aesthetician    時(shí)間: 2025-4-1 12:13
Least-Squares Collocation Error Estimates in a Test of Newton’s Gravitational Laweither a possible violation of Newton’s law or a model error (bias). Although the LSC error estimates of gravity interpolation on the ground are shown to be quite reasonable, it is suggested that a terrain misrepresentation can invalidate the error estimates of upward continuation.
作者: 增強(qiáng)    時(shí)間: 2025-4-1 14:24





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