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東京工業大学 理工学研究科 基礎物理学専攻 寺澤研究室 修士2年 樋口千夏
Statistical study of lightning activity: Periodicity and possible link with solar activity 東京工業大学 理工学研究科 基礎物理学専攻 寺澤研究室 修士2年 樋口千夏
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Contents Introduction Analysis and result discussion summary
・Solar activity ・Lightning activity Analysis and result discussion summary 1
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Contents Introduction Analysis and result discussion summary
・Solar activity ・Lightning activity Analysis and result discussion summary
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Variation on solar related parameter
F10.7 TSI GCR year [count] [W/m^2] [ 10^-22W /m^2Hz] F10.7:solar radio flux(10.7cm) proxy of UV flux TSI:Total Solar Irradiance GCR:Galactic Cosmic Ray (Using neutron monitor data) GCR 11-year period min max 2
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Variation on solar related parameter
F10.7 PSD[/Hz] TSI GCR E GCR Solar flare CMEs period[day] 27~30-day period 3
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Contents Introduction Analysis and result discussion summary
・Solar activity ・Lightning activity Analysis and result discussion summary
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Schumann resonance(SR)
(Sato,2003) Freq[Hz] Spectral intensity 7.8 14 20 5
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28-day periodicity of global lightning activity
<observation> ・at Syowa station in Antarctica (69.018S,39.506E) ・using search coil magnetometer <data> ・2000/2~2003/1 ・1~100Hz magnetic field data <SR power spectrum> (Sato,2003) 28-day 11 4~6 ・~5,~10-day periodicity ⇒Correlated with planetary wave activity in the tropical region ・~28-day periodicity ⇒Influence of solar activity? Power spectrum [day] 6
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Cross-spectral analysis
between global lightning activity and solar parameters (Sato,2003) parameter Period at the power-spectral peak[day] Period at the cross-spectral peak[day] Coherence Phase(θSR-θpar) [°] (timelags[day]) F10.7 27.8 26.9 0.56 +20-90(2-7) Cosmic Ray(CR) 30.7 30.5 0.47 - Sun Spot Number(SSN) 27.7 27.0 0.57 Kp 26.2 25.6 0.53 0(0) Dst 27.2 25.3 MeV electron 28.6 29.9 0.52 +110(8) MeV ion 33.1 31.6 0.58 Tropical cloud coverage(>8km) 24.0 0.65 ±180(0) ※Kp/Dst:Geomagnetic disturbance index 7
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Possible scenario of solar influence on lightning activity
<regional influence> Exp. UV ---temperature/wind modulation in stratosphere⇒vertical circulation⇒convective activity in troposphere GCR ---ionization⇒CCN⇒cloud ---ionization⇒electric breakdown Indirect influence <global influence> Exp. GCR ---ionization⇒modulation of conductivity in atmosphere through global electric circuit Direct influence 8
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Madden – Julian Oscillation
What is MJO? Madden – Julian Oscillation --intraseasonal(20-60days) variability in the tropical atmosphere --eastward propagation at 4-8m/s through the Indian and Pacific ocean --characterized by pressure,cloud amount,rainfall (Madden and Julian,1972) 9
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Contents Introduction Analysis and result discussion summary
・Solar activity ・Lightning activity Analysis and result discussion summary
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1.Lightning activity in Japan (45 prefectures)
<data> ・ extract from the weather record in JMA ・1989/1~2010/12 ・in Japan(except Hokkaido and Okinawa) Time profile of lightning data in Japan Monthly distribution [%] where lightning activity occurs The number of prefectures year 10 month
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※method of Histogram analysis
② ③ ④ ⑤ ⑥ ① where lightning activity occur The number of prefecture day period[day] 1 2 3 4 5 6 power 1(④) 1(⑥) 2(①⑤) 1(②) 1(③) power Period[day] 11
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Histogram analysis of lightning activity in Japan(45)
(a)The number of prefectures where lightning activity occurs:more 1 (b)more 5 (d)more 11 (e)more 12 (f)more 13 (g)more 14 (c)more 10 period[day] power ― 3σ ― average There is a ~29-day periodicity in lightning which occur in more 12 prf. 12
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1.Lightning activity in Japan (32 prefectures)
<data> ・extract from the weather record in JMA ・1989/1~2010/12 ・In Japan(except Hokkaido and Okinawa) ・except the area along the sea of Japan Time profile of lightning data in Japan Monthly distribution [%] where lightning activity occur The number of prefectures year month 13
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Histogram analysis of lightning activity in Japan(32)
― 3σ ― average ― 3σ ― average 28-29-day 51-day ― 3σ ― average <data> ・extract from the weather record in JMA ・1989/1~2010/12 ・in Japan ・except the area along the sea of Japan period[day] power ・March-October ・the number of prefectures where lightning activity occurs: more 9 ・the number of prefectures where lightning activity occurs: more 8 ・the number of prefectures where lightning activity occurs: more 7 28-29,51-day periodicity ⇒influence of solar activity? MJO? 14
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※method of corrrelation analysis
34day 34 34 34 parameter peak ・・・・ lightning C + parameter ・・・・ = ・・・・= lightning 15
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Correlation between F10.7/GCR-lightning(J)
F10.7 time lag[day] Lightning(J) GCR F10.7 time lag[day] ( ,Mar-Oct) ― 3σ ― 2σ 16
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Correlation between F10.7-lightning
( /9,Mar-Oct) time lag[day] Lightning(J) F10.7 Lightning In Africa ― 3σ ― 2σ between F10.7 and ・lightning in Africa: positive correlation (time lag:0day) ・lightning in Japan (time lag:20day) negative correlation (time lag:7day) 18
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Possible scenario of solar influence on lightning activity
<regional influence> Exp. UV ---temperature/wind modulation in stratosphere⇒vertical circulation⇒convective activity in troposphere GCR ---ionization⇒CCN⇒cloud ---ionization⇒electric breakdown Indirect influence <global influence> Exp. GCR ---ionization⇒modulation of conductivity in atmosphere through global electric circuit ? Direct influence 19
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Contents Introduction Analysis and result discussion summary
・Solar activity ・Lightning activity Analysis and result discussion summary
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Similarity between spectrum of lightning and OLR in WPWP
(Takahashi,2010) Lightning in Japan OLR in WPWP period[day] PSD ― max ― min PSD 20
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Possible scenario for F10.7-MJO-lightning
~28-day ~40-60-day F10.7 ~27-day ? MJO ~6m/s ~20day ~28-day low low low pressure low low low Africa ~12000km Japan 21
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Contents Introduction Analysis and result discussion summary
・Solar activity ・Lightning activity Analysis and result discussion summary
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summary <periodicity of lightning in Japan>
・There are ~28,51-day periodicity for 3 sigma significance in lightning which occur in more 9 prefectures except along the sea of Japan . ⇒influence of solar activity or MJO ?? <correlation between solar activity and lightning> ・There is a good correlation between lightning in Japan and F10.7/GCR for 3 sigma significance. The response is indirect influence of F10.7/GCR on lightning since there are response time lags. ・There is a good correlation with no time lag between lightning in Africa and F10.7 for ~3 sigma significance. ⇒possible link between F10.7, MJO and lightning 22
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