Aftershock Trend Analysis after 2011 Tohoku Earthquake

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Explore the trend analysis of aftershocks following the 2011 Tohoku Earthquake, the most powerful earthquake to ever hit Japan. Data obtained from the Japan Meteorological Agency reveals a significant decrease in aftershock numbers over time, with regression analysis showing interesting patterns in earthquake frequency. The conclusion highlights the ongoing nature of aftershocks post-disaster.

  • Aftershocks
  • Tohoku Earthquake
  • Trend Analysis
  • Japan
  • Seismic Activity

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  1. Trend Analysis of Aftershocks after 2011 Tohoku Earthquake EAS 4480 ZHONGDUO ZHANG 4/20/2017

  2. Background Date: 11 March 2011 Magnitude: 9.0 9.1 (Mw) Most powerful earthquake ever hit Japan 70km off coast 29km deep Caused by rupture of upper plate subducted by the Pacific Plate with a length of 500 km Lingering aftershocks

  3. Range of Aftershocks Shown in the red box Includes earthquakes occurred on the plate boundaries, as well as other earthquakes proximate to the main shock of 3.11 Earthquake

  4. Data for Analysis Obtained from Japan Meteorological Agency (JMA) Aftershock information currently available from March 2011 to March 2016 (5 years) Only includes earthquakes with magnitude greater than 4.0

  5. Overall Trend 7211 aftershocks in total Significant decrease in number within first year after main shock For the analysis, only use data beginning from one year after the main shock (13th month)

  6. Regression Analysis 4-Year Period (4/2012 3/2016) Average earthquakes per month: 39 LS Slope: -1.1794/month CI: [-4.711, 2.3519] Bootstrap Slope: -1.1654/month CI: [-1.1489, -1.1818]

  7. Regression Analysis The slope of decrease in the last 12 months of the sampling period is about one half of that for entire 4-year period Last 12 Months (4/2015 3/2016) Average earthquakes per month: 21 Bootstrap Slope: -0.5132/month CI: [-0.4877, -0.5387] LS Slope: -0.5490/month CI: [-3.5208, 2.1529]

  8. Frequency Analysis Lomb-Scargle Method No significant frequency found

  9. Conclusion The number of aftershocks tapers off as time elapses However, as the time elapses, the decrease rate of aftershocks becomes slower The aftershocks may still last for years No periodicity implication for the aftershocks

  10. Thank You!

  11. Source Japan Meteorological Agency (2016). Aftershock Activity of 2011 Tohoku Pacific Coast Earthquake. [http://www.jma.go.jp/jma/index.html] Earth Observatory of Singapore (2011). The great East Japan (Tohoku) 2011 earthquake: Important lessons from old dirt. [http://www.earthobservatory.sg/news/great-east-japan- tohoku-2011-earthquake-important-lessons-old-dirt]

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