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引用本文:周江存,孙和平.?人??????????????峱??????????????[J].大地测量与地球动力学,2007,27(6):28-32.
作者姓名:周江存  孙和平
作者单位:1. 中国科学院测量与地球物理研究所动力大地测量学重点实验室,武汉,430077;中国科学院研究生院,北京,100049
2. 中国科学院测量与地球物理研究所动力大地测量学重点实验室,武汉,430077
基金项目:中国科学院知识创新工程项目 , 国家自然科学基金 , 国家自然科学基金
摘    要:?????人????????????????????????????????????????????????????????峱??????????? ????У???????У???????У??????Σ?????????????????????????????????峱????????????????????????????? ??泱??????в??????????????????????????????????????????????????????????????????????? ??????????????????????????????????????????????С????????????????????????????????????????????????????????Щ???????????????????????????

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文章编号:1671-5942(2007)06-0028-05
收稿时间:2007-05-03
修稿时间:2007年5月3日

OCEAN TIDE LOADING CORRECTION ON LONG PERIOD EARTH TIDAL GRAVITY OBSERVATION AT WUHAN STATION
Zhou Jiangcun,Sun Heping.OCEAN TIDE LOADING CORRECTION ON LONG PERIOD EARTH TIDAL GRAVITY OBSERVATION AT WUHAN STATION[J].Journal of Geodesy and Geodynamics,2007,27(6):28-32.
Authors:Zhou Jiangcun  Sun Heping
Institution:1)KeyLaboratoryofDynamicalGeodesy,InstituteofGeodesyandGeophysics,CAS,Wuhan 430077 2)GraduateUniversityofChineseAcademyofSciences,Beijing  100049
Abstract:Applying the long term tidal parameters gravity obtained with the VAV and Etema softwares,the gravity observations with superconducting gravimeter at Wuhan station and on the ocean tide models:TPXO5,TPXO6,TPXO7,NAO99 and FES04.We have made the ocean tide loading correction to these observations.The numerical results show that the residuals of constituents of Mm and Mf are mainly caused by ocean tide loading.The corrected amplitude factors are closer to the theoretical ones of which the differences decrease from 3.4% and 2.5% to 0.16% and 0.12% respectively.Due to the low signal noise ratio of the long-period constituents with relatively small amplitudes,the tidal parameters of these constituents are difficult to be measured accurately at present.This is also proved by the results of ocean tide loading correction.
Keywords:long period earth tidal gravity  tidal parameter  ocean tide loading correction  superconducting gravimeter  ocean tide model
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