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《Chinese Journal of Geophysics》 1991-01
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Du PIN-REN(Institute of Geology, State Seismological Bureau, Beijing 100029)  
The detailed structure of spectrum of atmospheric tides is obtained by the spectral analysis-and harmonic analysis from the microbarograph records in 1984 and 1985 years in Ta-Yuan region in Beijing. Substituting load Love numbers for tidal Love numbers and following relative formula of earth tides, the expressions of crustal strain and tilt resulted from atmospheric tides are derived. Using the tidal water level data in Ta-Yuan well in conjunction with barometric data in situ, the influence of barometric pressure variations on water level in the well is analysed. The results of theoretic calculation are basically consistent with that analysed observations, especially, both results give that cubic dilatation of the crust produced by the atmospheric S2 tide is about 20 per cent of S2 tidal cubic dilatation.
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Chinese Journal Full-text Database 2 Hits
1 SUN He-ping LUO Shao-cong(Key Laboratory of Dynamics Geodesy, Institute of Geodesy and Geophysics, Chinese Academy of Sciences, Wuhan 430077, China);Study of the Atmospheric Pressure Influence on Geophysical Observations[J];Progress In Geophysics;2002-03
2 ZHOU Long-shou,QIU Ze-hua,TANG Lei(Institute of Crustal Dynamics,China Earthquake Administration,Beijing 100085,China);The response of crustal strain field to short-period Atmospheric pressure variation[J];Progress in Geophysics;2008-06
Chinese Journal Full-text Database 10 Hits
2 Xu Houze(Institute of Geodesy and Geophysics The Chinese Academy of Sciences);TIDE CORRECTIONS OF PRECISEGRAVITY MEASURMENTS[J];Acta Geodaetica Et Cartographic Sinica;1984-02
3 Cheng Xuerong(Institute of Geodesy and Ceophysios Sinica Academia)A method is proposed to calculate 3 components of purterbed gravity by combiningthe terrestrial gravimetric data and sattlite altimetric ones,with the fictitious gravityanomalies and fictitious mass points as Intermediate mediums.Model computation of the above methods shows pretty good digital results.We findthat to get the same accuracy,the extent needed is much smaller when using our methodthan that when using Stokes' Fomula.For example,if we perform Stokes' integra-tion within concentric circles with radii of 4.4 km and 44 km respectively,we shallfind that the former is about1/25 of the latter; but the accuracy changes little whenusing our method in the above different areas.This shows its advantage.We concludethat it will be suitable for the calculation of 3 components of purterbed gravity.;A DISCRETE METHOD OF GEODETIC BOUNDARYVALUE PROBLEM[J];Acta Geodaetica Et Cartographic Sinica;1984-02
4 Wu Xiaoping(Zhengzhou Institute of Surveying and Mapping);POINT-MASS MODEL OF LOCAL GRAVITY FIELD[J];Acta Geodaetica Et Cartographic Sinica;1984-04
5 Cao Huasheng Zhu Zhuowen Wang Xiaolan(Institute of Ceodesy and Geophysics, Academia Sinica);DIGITAL REALIZATION OF THE THEORY OF REPRE-SENTING THE EARTH'S GRAVITY FIELD BYFICTITIOUS SINGLE-LAYER DENSITY[J];Acta Geodaetica Et Cartographic Sinica;1985-04
6 Zhou Jiangwen(Institute of Geodesy and Geophysics. Chinese Academy of Sciences);INTEGRATED GEODESY AND ROTATION MATRICES[J];Acta Geodaetica Et Cartographic Sinica;1986-01
7 Xu Houze(Institute of Geodesy and Geophysics, Chinese Academy of Science);ERROR ESTIMAION ONGRAVITY LOADING CORRECTION[J];Acta Geodaetica Et Cartographic Sinica;1987-02
8 Qiu Weigen(Wuhan Technical Uniuersity of Surveying and Mapping);NUMERICAL SOLUTION OF MIXED BOUNDARYVALUE PROBLEM[J];Acta Geodaetica Et Cartographic Sinica;1990-01
9 Ning Jinsheng. Chao Dingbo. Bian Shaofeng(Wuhan Technical University of Surveying and Mapping);B-SPLIE APPROXIMATION OF GRAVCITY FIELD[J];Acta Geodaetica Et Cartographic Sinica;1990-04
10 Liu Dajie, Ning Jinsheng. Chao Dingbo(Wuhan Technical University of Surveging and Mapping);THE DETERMINISTIC PARAMETER MODELFOR INTEGRATED GEODESY[J];Acta Geodaetica Et Cartographic Sinica;1991-04
【Secondary References】
Chinese Journal Full-text Database 4 Hits
1 YANG Qiang①②, DANG Ya-ming①, BEI jin-zhong①(Institute of Geodesy and Geodynamic, Chinese Academy of Surveying and Mapping, Beijing 100039; ② Geoinformation Science & Engineering College, Shandong University of science and Technology, Qingdao 266510);Analysis of GPS time series of height component based on IGS continuous observation stations[J];Science of Surveying and Mapping;2007-03
2 Luo Shaocong and Xu JianqiaoKey Laboratory of the Dynamic Geodesy,Institute of Geodesy and Geophysics,CAS, Wuhan 430077;INFLUENCES OF WATER VAPOR ON ATMOSPHERIC GRAVITY AND TILT GREEN’S FUNCTION[J];Crustal Deformation and Earthquake;2004-04
3 JIE Wei-qiang~(1,2), WEI Chun-guang~1,HE Yu-hong~3 (1 School of Earth Science and Resources,China University of Geosciences,Beijing 100083,China;2 International expolration and development corporation of SINOPEC,Beijng,100083,China;3 China Meteorological Administration,Beijing 100081,China);Weather service for oil exploration[J];Progress in Geophysics;2006-01
4 ZHOU Long-shou,QIU Ze-hua,TANG Lei(Institute of Crustal Dynamics,China Earthquake Administration,Beijing 100085,China);The response of crustal strain field to short-period Atmospheric pressure variation[J];Progress in Geophysics;2008-06
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