Study on the influence of tropical cyclone to the deformation observation data of Wuzhishan Station
-
摘要: 通过对五指山台形变观测资料产生影响的热带气旋信息统计及数据分析发现:该台的倾斜类仪器的热带气旋响应水平明显高于应变类仪器,特别是VP垂直摆的响应能力最强,SSY伸缩仪的风扰响应水平最弱;不同气旋引起的震颤波扰动信号的形态、振幅、频率、扰动强度不同;同一气旋对倾斜类仪器VP垂直摆北南向响应幅度最大,最大扰动强度幅度量级为20×10−3″/ms左右,持续时间与气旋的生命周期有关。Abstract: According to the statistics and data analysis of the tropical cyclone data which have influence to the deformation observation data at Wuzhishan Station, it is found that the response level of the tilt type instrument is obviously higher than that of the strain type instrument. In particular, the response of the VP vertical pendulum is the strongest, and the wind disturbance response of the SSY extensometer is the weakest. The maximum amplitude of the VP vertical pendulum is about 20×10−3″/ms, and the duration is related to the life cycle of the cyclone.
-
Key words:
- tropical cyclone /
- inclinometer /
- extensometer /
- tremor signal
-
表 1 不同台风对定点形变仪器的干扰特征
Table 1. Disturbance characteristics of fixed-point deformation instruments caused by different typhoons
台风
名称最大
风力
/级登陆点与
台站距离
/kmDSQ
-NSDSQ
-EWSSY
-NSSSY
-EWVP
-NSVP
-EW曲线形
态变化变幅
/10−3″曲线形
态变化变幅
/10−3″曲线形
态变化变幅
/10−8″曲线形
态变化变幅
/10−8″曲线形
态变化变幅
/10−3″曲线形
态变化变幅
/10−3″Kujira 10 98 无 36.0 无 38.6 无 280 无 276 粗、畸变 23.2 粗、畸变 32.2 Mujigae 15 260 无 36.4 无 46.4 无 432 无 430 粗、畸变 20.2 粗、畸变 36.8 Sarika 14 97 无 100 无 76.0 无 466 无 460 纺锥形 34.1 纺锤形 54.0 Sonca 9 325 无 36.9 无 42.0 无 293 无 316 无 27.1 无 41.0 Doksuir 14 347 粗、畸变 55.8 无 44.0 无 340 无 418 纺锤形 27.8 纺锤形 62.4 Khanun 14 200 无 48.2 无 56.2 无 406 无 324 粗、畸变 28.0 粗、畸变 55.2 表 2 不同热带气旋与定点形变仪器震颤波信号的主频对比(单位:赫兹)
Table 2. Comparison of main frequency of tremor signals between different tropical cyclones and fixed-point deformation instruments (unit:Hz)
台风名称 信号主频 DSQ-NS DSQ-EW SSY-NS SSY-EW VP-NS VP-EW Kujira 0.06 0.04 0.18 0.20 0.10 0.08 Mujigae 0.06 0.08 0.22 0.25 0.12 0.10 Sarika 0.12 0.08 0.18 0.28 0.20 0.08 Sonca 0.20 0.10 0.30 0.28 0.32 0.20 Doksuir 0.34 0.08 0.18 0.25 0.08 0.14 Khanun 0.20 0.08 0.18 0.22 0.20 0.08 -
[1] 于润玲,余晖,端义宏. 登陆华南热带气旋强度变化与大尺度环流的关系[J]. 大气科学学报,2013,36(5):619-625 doi: 10.3969/j.issn.1674-7097.2013.05.013Yu R L,Yu H,Duan Y H. Relationship between intensity change of tropical cyclone landing in South China and large-scale circulation[J]. Transactions of Atmospheric Sciences,2013,36(5):619-625 doi: 10.3969/j.issn.1674-7097.2013.05.013 [2] 蒋骏,张雁滨,林钢,等. 固体潮观测中的震颤异常波[J]. 地球物理学报,2012,55(2):462-471Jiang J,Zhang Y B,Lin G,et al. The tidal instruments recorded abnormal tremor wave[J]. Chinese Journal of Geophysics,2012,55(2):462-471 [3] 张燕,吕品姬,吴云. 宽频仪器观测的特定频段震颤波产生的原因分析[J]. 大地测量与地球动力学,2014,34(1):47-50Zhang Y,Lü P J,Wu Y. On the reasons generating high frequency tremor observed by broadband instruments[J]. Journal of Geodesy and Geodynamics,2014,34(1):47-50 [4] 张雁滨,蒋骏,李才媛,等. 昆仑山强震前的震颤波并非源自慢地震[J]. 地球物理学报,2013,56(3):869-877 doi: 10.6038/cjg20130316Zhang Y B,Jiang J,Li C Y,et al. The tremor wave before the Kunlun strong earthquake is not slow earthquake event[J]. Chinese Journal of Geophysics,2013,56(3):869-877 doi: 10.6038/cjg20130316 [5] 顾申宜,张慧,解晓静,等. 海南井水位对热带气旋响应特征分析[J]. 地震学报,2012,34(5):716-724 doi: 10.3969/j.issn.0253-3782.2012.05.013Gu S Y,Zhang H,Xie X J,et al. Analysis on features of well water response in Hainan Province to tropical cyclones[J]. Acta Seismologica Sinica,2012,34(5):716-724 doi: 10.3969/j.issn.0253-3782.2012.05.013 [6] 李盛,孙三健,张慧,等. 热带气旋对琼中台重力非潮汐变化影响研究[J]. 地震工程学报,2016,38(增刊1):101-105Li S,Sun S J,Zhang H,et al. Influence of tropical cyclones on the non-tidal gravity variation at Qiongzhong Station[J]. China Earthquake Engineering Journal,2016,38(S1):101-105 [7] 张雁滨,蒋骏,李胜乐,等. 热带气旋引起的震颤波[J]. 地球物理学报,2010,53(2):335-341 doi: 10.3969/j.issn.0001-5733.2010.02.011Zhang Y B,Jiang J,Li S L,et al. The tropic cyclone aroused the tremor[J]. Chinese Journal of Geophysics,2010,53(2):335-341 doi: 10.3969/j.issn.0001-5733.2010.02.011 [8] 张卓. 海南五指山地区早二叠世(强)过铝花岗岩成因及构造意义[D]. 南昌: 东华理工大学, 2014Zhang Z. Genesis and tectonic significance of Early Permian (strong) peraluminous granites in the Wuzhishan area of Hainan[D]. Nanchang: East China University of Science and Technology, 2014 -