张会苑,杨晶琼. 云南台网区域自动地震速报及人工速报定位偏差[J]. 华北地震科学,2020, 38(3):38-43, 59. doi:10.3969/j.issn. 1003−1375.2020.03.007.
引用本文: 张会苑,杨晶琼. 云南台网区域自动地震速报及人工速报定位偏差[J]. 华北地震科学,2020, 38(3):38-43, 59. doi:10.3969/j.issn. 1003−1375.2020.03.007.
ZHANG Huiyuan,YANG Jingqiong. Location Results Error of Regional Automatic Earthquake Reporting and Manual Earthquake Reporting in Yunnan Seismic Network[J]. North China Earthqauke Sciences,2020, 38(3):38-43, 59. doi:10.3969/j.issn.1003− 1375.2020.03.007.
Citation: ZHANG Huiyuan,YANG Jingqiong. Location Results Error of Regional Automatic Earthquake Reporting and Manual Earthquake Reporting in Yunnan Seismic Network[J]. North China Earthqauke Sciences,2020, 38(3):38-43, 59. doi:10.3969/j.issn.1003− 1375.2020.03.007.

云南台网区域自动地震速报及人工速报定位偏差

Location Results Error of Regional Automatic Earthquake Reporting and Manual Earthquake Reporting in Yunnan Seismic Network

  • 摘要: 选取2009年7月1日至 2017年12月31日云南地震台网区域自动地震速报及人工地震速报定位结果,对比全国统一编目结果,对定位偏差进行分析,结果显示:①自动速报用时不受台站分布的影响,但漏报地震较多;人工速报用时与台站分布有密切的关系,台站分布均匀合理地区地震速报用时明显减少;②对于震中位置的确定,1类地震基本在规定范围内,但2、3类地震区域自动速报存在较大问题,人工速报虽有改善但仍需进一步优化;③区域自动速报系统对于M≥4.5地震震级的确定偏差较大,人工速报基本不存在问题;④震源深度偏差基本都在规定范围内,偏差超过规定范围的地震基本分布在台站稀少、分布不合理地区,人工速报对于结果的改善没有明显效果。最后分析了漏报和误报情况,为云南台网地震速报的提高提供一定的参考。

     

    Abstract: The location result error of regional automatic earthquake reporting and manual earthquake reporting of Yunnan seismic network was compared and analyzed base on officially published earthquake catalog from Jul. 1, 2009 to Dec. 31, 2017, the results shows that: ① The time of automatic quick report is not affected by the distribution of stations, while the time of manual quick report is closely related to the distribution of stations. ② For the determination of epicenter location, category 1 earthquakes are basically within the specified range, but there are big problems in automatic reporting of category 2 and 3 earthquakes. Although manual earthquake reporting has been improved, it still needs further optimization. ③ The regional automatic earthquake reporting system has a larger deviation in determining the magnitude of earthquakes with M≥4.5, and there is basically no problem in manual earthquake reporting. ④ The errors of origin time and depth are basically within the specified range, and the earthquakes with error exceeding the specified range are basically distributed in areas with fewer stations and unreasonable distribution of stations. Manual earthquake reporting has no obvious effect on improving the results. The missing report and false report are also analyzed to provide some references for the improvement of the earthquake report in Yunnan network.

     

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