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[1]朱传东,刘金钊,占 伟,等.青藏高原南缘绝对重力测站的非构造重力效应特征*[J].地震研究,2020,43(04):651-657.
 ZHU Chuandong,LIU Jinzhao,ZHAN Wei,et al.Non-tectonic Gravity Effect of Absolute Gravity Observation Stations in Southern Margin of Qinghai-Tibetan Plateau[J].Journal of Seismological Research,2020,43(04):651-657.
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青藏高原南缘绝对重力测站的非构造重力效应特征*(PDF/HTML)

《地震研究》[ISSN:1000-0666/CN:53-1062/P]

卷:
43
期数:
2020年04期
页码:
651-657
栏目:
出版日期:
2020-09-17

文章信息/Info

Title:
Non-tectonic Gravity Effect of Absolute Gravity Observation Stations in Southern Margin of Qinghai-Tibetan Plateau
作者:
朱传东刘金钊占 伟陈兆辉李经纬
(中国地震局第一监测中心,天津 300180)
Author(s):
ZHU ChuandongLIU JinzhaoZHAN WeiCHEN ZhaohuiLI Jingwei
(The First Monitoring and Application Center,China Earthquake Administration,Tianjin 300180,China)
关键词:
青藏高原南缘 绝对重力 非构造重力效应
Keywords:
southern margin of Qinghai-Tibet Plateau absolute gravity non-tectonic gravity effect
分类号:
P315.726
DOI:
-
摘要:
基于2002—2017年的ECMWF Interim三维大气再分析资料、GRACE时变重力场模型和GPS数据,分析了青藏高原南缘的拉萨、日喀则、仲巴、噶尔4个绝对重力测站的非构造重力效应。结果表明:ECMWF Interim大气负荷重力效应主要表现为季节性变化特征,最大周年振幅可达到1.4 μGal; GRACE陆地水负荷重力效应和GPS地壳垂直位移引起的重力效应均存在较为明显的季节性及长期趋势变化特征,二者的最大周年振幅和长期趋势分别达到2.6 μGal,-0.6 μGal/a和1.8 μGal,-0.3 μGal/a; GRACE与GPS的比较分析结果表明青藏高原南缘的非构造重力效应会受到局部流体质量负荷的显著影响。
Abstract:
Based on three-dimensional ECMWF interim reanalysis data,GRACE time variable gravity model and GPS data from 2002 to 2017,we analyzed the nontectonic gravity effects of absolute gravity observation stations in southern margin of Qinghai-Tibetan Plateau.The results show that the ECMWF Interim atmospheric gravity effect mainly presents seasonal characteristics.Its maximum annual amplitude is 1.4 μGal.The GRACE hydrological gravity effect and gravity effect caused by the vertical crustal deformation from GPS show obvious seasonal and long-term trend characteristics.The maximum annual amplitude and long-term trend can reach 2.6 μGal and -0.6 μGal/a,1.8 μGal and 0.3 μGal/a,respectively.The comparative analysis of GRACE and GPS show that the nontectonic gravity effects in southern margin of Qinghai-Tibetan Plateau can be significantly affected by the local fluid mass load.

参考文献/References:

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备注/Memo

备注/Memo:
收稿日期:2020-01-19
基金项目:中国地震局地震科技星火计划项目(XH194204Y)、国家自然科学基金(41804010,41704084)、国家重点研发计划项目(2018YFC1503606)和天津市自然科学基金(17JCYBJC21600)联合资助.

更新日期/Last Update: 2020-09-17