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1.
华南地区电离层在汶川地震前VTEC异常的研究   总被引:2,自引:1,他引:1  
基于华南地区GPS监测网数据.解算出华南地区电离层VTEC在汶川地震前出现的异常。从时间序列和空间等值线分布两方面分析了VTEC的变化.时间序列分析表明5月4日至5月12日电离层VTEC负异常扰动明显.5月4日至5月13日的空间分布也表明了同样的结论,并同时指出负异常有向低纬度区域漂移的趋势。并对异常判断依据和机理作了初步的讨论.  相似文献   

2.
地震前兆:电离层F2层异常   总被引:1,自引:2,他引:1       下载免费PDF全文
本文简述了目前提出的地震引起电离层异常扰动的物理机理,重点介绍了近几年国内外对震前F2层异常扰动的研究进展.大量的研究结果显示地震活动引起的电离层扰动不仅确实存在,而且在震级大于5级的地震发生前的几天到几个小时会发生电离层扰动.由于地震引起的电离层F2层变化具有独一无二的特性,这就意味着我们可以利用强震前的F2层异常变化作为地震短临预报的工具.  相似文献   

3.
通过平行方位相关分析,纯异常矢量比和功率谱分析,Pc地电脉动,动电暴湾扰等多种方法论证了岱山中学地电场的短周期变化属于大地电位变化,该观测点是观测大地电位变化的敏感点。  相似文献   

4.
利用地基GPS观测数据研究与地震有关的电离层异常   总被引:3,自引:0,他引:3  
马新欣  金红林  孟国杰 《地震》2008,28(4):80-90
利用中国大陆GPS连续站观测数据, 根据电离层单层模型, 计算得到中国大陆上空电离层电子总含量TEC(Total Electron Content)值的时间序列。 选取2001—2008年发生在中国大陆地区的11个MS≥6.0地震, 分析了这11个地震前后TEC值时间序列的变化特征。 分析结果显示, 地震活动期间距离震中700 km以外的GPS连续观测站上空TEC值的异常现象不明显, TEC值变化基本在0.5 TECU之内。 11个震例中有6个震例TEC值出现了负异常现象, 主要表现在震前1~5 d, 并且观测站距离震中越近, TEC值变化越明显, 少数震例在地震发生期间TEC值明显增加。 研究认为, 利用GPS连续观测数据研究与地震有关的电离层前兆是可能的。  相似文献   

5.
新疆天山地区定点形变群体异常特征与地震活动   总被引:1,自引:1,他引:0  
杨又陵  曲延军 《地震》2002,22(1):91-96
利用定义的形变异常密度和趋势分析法研究了1990~ 2000年新疆天山地区定点形变异常的时空分布、群体异常特征及与中强地震活动的关系。结果表明,各分区形变资料显示的高密度异常在时间上与b 值异常有一定的相关性,与该地区的中强地震活动有较好的对应关系;一组中强地震前2~ 4年能观测到形变趋势项的转折、加速等变化。  相似文献   

6.
云南楚雄地区成组强震与单个强震的前兆差异性研究   总被引:1,自引:1,他引:0  
石绍先  曹刻  徐彦  和宏伟 《地震研究》2004,27(2):111-118
以1995与2000年发生在云南楚雄地区武定、姚安的两次6.5级强震为例,研究了成组强震和单个强震的前兆差异性。发现在远源区、近源区及源区的前震活动、地震序列、前兆群体异常及边界动力条件方面的差异十分显著。同时指出这些差异对于识别成组强震和单个强震及后续强震预报具有重要意义。  相似文献   

7.
华北地震活动中短期异常图像研究   总被引:2,自引:0,他引:2  
系统研究了多种地震活动性方法后认为, 1970年以来华北地区发生的MS≥5.8中强震前, 约83%具有3级或4级地震异常条带、 孕震空区及信号震出现。 震前有信号震的比例占92%, 83%的信号震距主震150 km以内, 距主震发生时间小于1年的占67%。 条带时间形成进程在2年内的约占90%, 震前条带形成后到主震发生83%在5个月内。 空区形成进程在1年半内的占83%, 空区形成后到主震发生91%在50天内, 为有意义的地震活动图像短期异常特征。 文中还探讨了异常条带图像的定量判别指标及其与未来强震的关联。  相似文献   

8.
Meun.  JM 陈忠义 《地震研究》1991,14(4):309-315
在地球及其电离层的静电理论的范畴内,能简单地解释一切跟地震有关的电气现象。电离层由于电子的康普顿散射通常是正电的,地球深部由于电子静电泵离电离层也是正电性的。这些电于形成约1800安的规则连续电流,而正离子必然是突发式流动而形成雷电、火山喷发以及某些类型的地震。地震的主要成因显然是构造应力的释放,但是地震目录中的某些地震可能是被静电爆发作用所触发的。这种地震具备下列两个必要条件:位于深处的正离子能贯穿高电阻的上地幔;在电离层中存在吸引正离子的局部负电异常。大气层电场和“地震—大地电流”的同步联测可能是预报地震的时间和地点的两单而又准确的方法。  相似文献   

9.
The specific features of a method for radiosounding the lower ionosphere over earthquake epicenters using LF electromagnetic signals of thunderstorm sources (atmospherics) have been considered. The effects of shallow-focus earthquakes with magnitudes larger than 4.0 and their precursors manifest themselves in amplitude characteristics of atmospherics. It has been assumed that variations in the signal characteristics are related to disturbances in the lower ionosphere. According to the results of azimuthal scanning, cross-sectional dimensions of disturbed regions, as a rule, correspond to the dimensions of the first two Fresnel zones for signals at a frequency of 10 kHz. Azimuthal scanning also indicated that the positions of disturbed regions during and before earthquakes could have a certain dynamics and differ from the projection onto the earthquake epicenter. The ratio of the amplitudes of electric and magnetic signal components, in the variations of which seismic effects before earthquakes can also be observed, has been considered. An analysis of the ratio makes it possible to increase the probability of predicting earthquakes when using the characteristics of the electromagnetic signals of lightning discharges as an additional method of complex monitoring of disturbances in the lower ionosphere caused by seismic processes.  相似文献   

10.
广东潮州井水化学地震前兆异常特征分析   总被引:1,自引:0,他引:1  
根据广东潮州井24年的水化学观测资料,通过对强震以及中等地震前水化学异常研究得到,潮州井水化学资料在中等地震前以中短期异常为主,而强震前水化学测项出现长趋势异常变化。研究还表明,同样的震前异常持续时间,未来地震的震中距越大,其震级也应更大。从异常形态对比可见,震中距越小的地震,其异常变化的幅度和速率也较大。  相似文献   

11.
The data, obtained using the methods of partial reflections and ionosphere vertical sounding on the Kola Peninsula and in Scandinavia, at Tumannyi (69.0° N, 35.7° E) and Sodankyla (67.37°N, 26.63°E) observatories, have been analyzed in order to detect earthquake responses. The strong earthquakes have been considered: one earthquake with a magnitude of 7.7 occurred at 0819:25 UT on July 17, 2006, on the western coast of Indonesia (9.33° S, 107.26° E), and another earthquake with a magnitude of 6.2 occurred 2253:59 UT on May 26, 2006, on Yava (7.94° S, 110.32° E). These earthquakes, the epicenters of which were located in the same region and at identical depths (10 km), were observed under quiet conditions in the geomagnetic field (ΣK p = 5.7 and 6.3) and during small solar flares. The response of the ionosphere to these flares was mainly observed in the parameters of the lower ionosphere in the D and E regions. It has been found out that the period of variations in the ordinary component of the partially reflected signal at altitudes of the E region increased before the earthquake that occurred on July 17, 2006. The f min variations at Sodankyla observatory started 20 h before the earthquake. The periods of these variations were 3–6 h. The same periods were found in the variations in other ionospheric parameters (foEs and h’Es). The variations in the ordinary component of partially reflected signals with periods of 2–5 hours were observed on the day of another earthquake (May 26, 2006). Internal gravity waves with periods of several hours, which can be related to the earthquakes, were detected in the amplitude spectra of the ordinary component of partially reflected signals and in other parameters in the lower ionosphere.  相似文献   

12.
This paper summarizes the results of more than 10 years spent by the authors studying the variations in the ionosphere over seismically active regions several days or hours before strong earthquakes. The physical mechanisms of such variations established by the authors and published previously are submitted in the references. This article is aimed mainly at determining the major characteristic parameters of the observed effects (temporal and spatial variations, range in amplitude, etc.) to provide the means to separate the seismogenic effects from other forms of ionospheric variability. Data obtained by ground-based ionosondes and by topside vertical sounding from satellites are used in conjunction with local probe measurements. The topside vertical profiles of the electron concentration are analyzed. It is shown that the most characteristic effect is that of scale height changes in the vertical distribution of ions and electrons implying a decrease in the mean ion mass within the F-layer due to seismogenic effects. This result is supported by direct mass-spectrometer measurements. Differences between magnetic storm ionospheric disturbances and seismogenic variations within the ionosphere are also discussed.  相似文献   

13.
中国西南区域孕震区电离层TEC变化长时间序列分析   总被引:2,自引:1,他引:1       下载免费PDF全文
通过中国地壳运动网络提供的GPS观测数据,获取了高精度电离层TEC分布,采用滑动四分位法分析了中国西南区域2008年4—10月(太阳和地磁活动平静时段)6次连续的MW6.0以上地震期间孕震区电离层TEC长时间变化及其异常分布;并在此基础上利用GIM数据对比分析了全球TEC变化特征。鉴于电离层主要受到太阳和地磁等空间天气的影响,将TEC变化与太阳EUV辐射、行星际磁场南向分量IMF Bz以及地磁活动指数Dst和Kp进行了比较。结果发现,该时段内电离层TEC异常扰动与太阳和地磁活动有很好的相关性;除汶川地震外,其他地震前没有发现明显的跟地震相关的TEC异常扰动现象。同时,对比分析了与上述研究区位于同一地磁纬度的"检验区"(30°~50°E,15°~35°N)的GPS TEC随时间变化和异常分布情况,结果显示TEC异常分布的时空特征与研究区域较为一致。由于电离层是一个复杂的系统,其扰动具有多源性,而且地震电离层扰动现象是复杂多变的,因此需要联合地基和天基手段共同观测,并加强其机理研究。  相似文献   

14.
利用调制比时空扫描方法,对1973—2014年云南地区MS≥6.0地震进行回溯性研究,分析强震前区域小震调制比时空演化过程。结果显示,从小震调制比异常开始至发震的持续时间为1.5 a之内,调制比异常的最高值需大于0.57,强震多发生在调制比为最高值时或其后14个月内异常区边界或内部调制比显著高值附近,震级随异常持续时间的延长大致呈增加的趋势;小滇西—滇西北地区的强震多发生在调制期内;从分区来看,滇西南强震多发生在调制比为最高值(Rm≥0.57)后6个月内的异常边界处,尤其是3个月内,滇西北强震多发生在最高值(Rm≥0.67)后7—12月内异常区内显著高值附近,滇东北强震多发生在最高值(Rm≥0.67)时的异常区内。  相似文献   

15.
Introduction The behavior of ground water is influenced by many factors, such as rainfall, exploitation ofground water, atmospheric pressure, tidal gravitation, ground stress variation, effect of surfacewater-body loads (or other loads) and other unknown factors. These factors change the dynamicstate of ground water to different extents and result in the diversification of ground water behavior.As for their mechanism, our knowledge is still superficial. Based on various images of water le…  相似文献   

16.
粤闽地区水化学地震前兆异常特征分析   总被引:3,自引:0,他引:3  
研究了粤闽两省及其近海近年来2次强震以及6个中等地震水化学前兆资料,结果表明,中等地震与强震的水化学前兆异常在数量上有着显著的差异,中等地震震前以中短期及短临异常变化为主,而强震前则超过三分之一的水化学测项出现持续1~4年的长趋势异常变化。同时研究表明,单凭水化异常出现的集中程度对未来震中作出预测是无统计依据的。  相似文献   

17.
六年来,我们用无阻尼水平摆地倾仪,在1.7秒—5秒的周期范围内,在一系列的强震发生前,分别记录到了一种明显的波动异常。並用它对不少的强震,诸如1976年8月16日松潘7.2级地震、1976年11月7日盐源6.9级地震,作了比较好的临震预报。实践证明这是一种有苗头的临震前兆。本文是对六年来探索工作的一个总结,並对其成因机制作了初步的探讨。  相似文献   

18.
On the basis of our predecessors' research,we study the distribution and the space-time evolution characteristics of the seismic apparent strain field in Yunnan since the 1970's using the seismic data of Yunnan and its surrounding areas.The result shows that there is a rather strong corresponding relationship between the anomaly region of seismic apparent strain and strong earthquakes.In the nine earthquakes studied,anomaly areas of seismic apparent strain had appeared before eight earthquakes,including five occurring in the anomaly region and three on the edge.Finally,the investigative result is demonstrated primarily.  相似文献   

19.
IntroductionEarthquakemonitoringandpredictionisstillatthestageofexplorationandempiricalprediction.Thebasisistheanomalyvariationconsistingofseismometryindexandtheobservedresultsusingtheprecursoryapproaches.Althoughthesevariationshowsvarietyandcomplexityanditsrelationwithearthquakesisnotcertain,throughcarefullystudyingonMs>7earthquakeswecanfindthattheanomalyvariationbeforeearthquakestillshowssteadyreappearanceandhasregularity.Theyareallrelativetotheseismogenicprocess.Inthispaperwefocusonstronge…  相似文献   

20.
利用云南省123个气象台站1960年以来的降雨量资料,使用年降雨量距平百分率方法,分析楚雄强震与降雨量的关系,结果发现:年降雨量距平百分率≥0.25的台站数大于8,次年云南地区皆有Ms≥6.0地震,也是楚雄地区发生6级强震背景条件;楚雄地区强震前表现涝异常,即该区域强震具有涝—震特征.  相似文献   

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