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云南丽江台OSG-066重力潮汐观测结果及应用
引用本文:梁莹,陈晓东,孙和平,崔小明,张苗苗,牛晓伟.云南丽江台OSG-066重力潮汐观测结果及应用[J].大地测量与地球动力学,2020,40(7):713-719.
作者姓名:梁莹  陈晓东  孙和平  崔小明  张苗苗  牛晓伟
作者单位:中国科学院测量与地球物理研究所大地测量与地球动力学国家重点实验室;中国科学院大学
基金项目:国家自然科学基金(41321063,41774092,41374084,41574072);中国博士后科学基金(2017M622552)。
摘    要:基于云南丽江台超导重力仪OSG-066超过5 a的连续重力潮汐观测资料,获取高精度潮汐参数并构建地方重力潮汐模型,为丽江地区精确重力潮汐改正提供参考。研究9个全球海潮模型在丽江台的重力影响改正有效性,用时域内回归分析法和频域内小波分析法分别研究大气重力导纳值的变化特征,并利用观测潮汐数据估算自由核章动本征参数。结果表明,9个海潮模型在丽江台的重力影响改正效果基本一致,NAO.99b模型的改正精度较高;大气重力导纳值在时域和频域内均显示出较为明显的季节性变化特征,且与降雨量变化存在负相关关系。自由核章动本征周期为431.5(411.2,454.0)恒星日,品质因子为-2796。

关 键 词:OSG-066  地方重力潮汐模型  海潮重力影响  大气重力导纳值  自由核章动

Gravity Tide Observation with OSG-066 and Their Applications at Lijiang Station,Yunnan Province,China
LIANG Ying,CHEN Xiaodong,SUN Heping,CUI Xiaoming,ZHANG Miaomiao,NIU Xiaowei.Gravity Tide Observation with OSG-066 and Their Applications at Lijiang Station,Yunnan Province,China[J].Journal of Geodesy and Geodynamics,2020,40(7):713-719.
Authors:LIANG Ying  CHEN Xiaodong  SUN Heping  CUI Xiaoming  ZHANG Miaomiao  NIU Xiaowei
Institution:(State Key Laboratory of Geodesy and Earth’s Dynamics,Institute of Geodesy and Geophysics,CAS,340 Xudong Street,Wuhan 430077,China;University of Chinese Academy of Sciences,A19 Yuquan Road,Beijing 100049,China)
Abstract:Abstract: We use more than 5 years continuous data recorded with the observatory superconducting gravimeter(OSG-066) at Lijiang station, Yunnan province, China. High precision tidal parameters are obtained, and the local gravity tide model is established to provide a reference for accurate gravity tide deduction in Lijiang area. The correction effectiveness of gravity influence of ocean tide is computed with 9 new global tide models. In addition, the atmospheric gravity admittance is studied with regression analysis in time domain and wavelet analysis in frequency domain. The parameters of free core nutation are further estimated with the observed tidal parameters. The results show that gravity influence corrections of the 9 different ocean tide models are almost the same at Lijiang station, and correction accuracy of the tide model NAO.99b is slightly higher among them. Results of obtained atmospheric gravity admittance demonstrate that significant seasonal variation characteristics are found in both time domain and frequency domain; significant inverse correlation is found between precipitation data and atmospheric gravity admittance. The eigen period of free core nutation is 431.5(411.2, 454.0) sidereal days, while the quality factor is -2 796.
Keywords:OSG-066  local gravity tide model  gravity influence of ocean tide  atmospheric gravity admittance  free core nutation  
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