首页 | 本学科首页   官方微博 | 高级检索  
     检索      

黄石台ORBES-81型伸缩仪观测结果的调和分析及海潮改正
引用本文:周坤根 Ducar.,B.黄石台ORBES-81型伸缩仪观测结果的调和分析及海潮改正[J].地球物理学报,1991,34(4):474-481.
作者姓名:周坤根 Ducar.  B
作者单位:1. 国家地震局地震研究所, 湖北武昌 430071; 2. 比利时皇家天文台
摘    要:本文对黄石台ORBES-81型石英伸缩仪的应变固体潮观测资料作了分析计算,其调和分析结果为:对O1波,振幅因子0.4219,相位滞后6°36';对M2波,振幅因子0.4256,相位滞后-4°42'.同时,讨论了海潮引起的负荷潮汐应变的改正问题.模拟计算发现负荷潮汐应变与体潮应变大致为同一量级,文中列出了海潮改正后的结果,并作了讨论.最后,对黄石台伸缩仪的架设方位作了评价.

关 键 词:应变固体潮  调和分析  海潮改正  
收稿时间:1987-08-22

HARMONIC ANALYSIS AND OCEAN LOADING CORRECTION OF OBSERVATION BY ORBES-81 EXTENSOMETER AT HUANGSHI STATION
ZHOU KUN-GEN,B. DUCARME,HU YAN-CHANG.HARMONIC ANALYSIS AND OCEAN LOADING CORRECTION OF OBSERVATION BY ORBES-81 EXTENSOMETER AT HUANGSHI STATION[J].Chinese Journal of Geophysics,1991,34(4):474-481.
Authors:ZHOU KUN-GEN  B DUCARME  HU YAN-CHANG
Institution:1. Institute of Seismology, Wuhan 430071; 2. Observatoire Royal de Belgique, 1180 Bruxelles
Abstract:In this paper, a harmonic analysis of strain tidal observation of the ORBES-81 quartz extensometer at Huangshi is made by using the program of the International Center for Earth Tides (the amplitude factor and the phase lag are 0.4219 and 6°36 for O1, 0.4256 and - 4°42' for M2). Furthermore, a discussion of the loading tidal strain correction is given with the result after the loading correction. We found that the loading tidal strain has approximately the same amplitude as the body one. An evaluation of the actual azimuth of the extensometer at Huangshi is discussed.
Keywords:Strain tides  Harmonic analysis  Ocean loading correction  
本文献已被 维普 等数据库收录!
点击此处可从《地球物理学报》浏览原始摘要信息
点击此处可从《地球物理学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号