Statistical Characteristics of Lighting over the Korean Peninsula for 1996-2000

1996-2000년에 한반도에서 발생한 낙뢰의 통계적 특성

Lim, Eun-Ha;Lee, Tae-Young
임은하;이태영

  • Published : 20050200

Abstract

Lightning data for the five-year period of 1996-2000 have been analyzed to understand the statistical features of lightning and the relationship between heavy rainfall and lightning frequency over the Korean peninsula. Analysis indicates that lightning occurs most frequently in July and August. And lightning occurs more frequently in the afternoon hours of 06 - 11 UTC (3 - 8 pm, Korean local time). Geographically, it occurs much more frequently over the western part of the peninsula near the west coast. Area of maximum rainfall amount does not coincide well with that of highest lightning frequency. It has been found that heavy rainfalls occur without any lightning at 68% of heavy rainfall stations during summer and at 82% of heavy rainfall stations for June. Rainfall amount does not show a systematic variation with lightning frequency. Band-type convection shows largest number of lightning among the heavy precipitation systems considered in this study, mainly due to its stationary behavior and sustained strength.

한반도 낙뢰의 통계적 특징과 집중호우와 낙뢰빈도의 관계를 이해하기 위하여 1996년부터 2000년까지 5년 동안 한반도에서 관측된 낙뢰 자료를 분석하였다. 7월과 8월에 낙뢰가 가장 많이 발생하였으며, 오후 3 - 8시 (06 - 11 UTC)에 발생 빈도가 높았다. 낙뢰 자료의 공간 분포에서는 서해안에 가까운 한반도 서부지역에서 훨씬 더 많은 발생 빈도를 나타냈으며, 최대 강수량 지역과 낙뢰가 가장 빈번하게 발생하는 지역은 서로 일치하지 않았다. 여름의 집중호우 지점 (일강수량이 100 mm 이상인 지점) 중, 68%가 낙뢰를 동반하지 않았으며, 6월의 경우는 82%가 낙뢰를 동반하지 않은 것으로 나타났다. 강수량은 낙뢰 발생 빈도에 따른 계통적 변화를 보이지 않았다. 본 연구에서 고려된 집중호우 형태 중에서 밴드형 대류계에서 낙뢰가 가장 많이 발생하였는데, 이는 밴드형 대류계의 정체적인 특징과 지속되는 강도 때문인 것으로 보인다.

Keywords

References

  1. Dye, J.E, J.J. Jones, W.P. Winn, T.A. Cerni, B. Gradiner, D. Lamb, R.L. Pitter, J. Hallet, and C.P.R. Saunders, 1986: Early electrification and precipitation development in a small isolated Montana cumulonimbus. J. Geoohys. Res., 91, 1231-1247 https://doi.org/10.1029/JD091iD01p01231
  2. Hodanish, S., D. Sharp, W. Collins, P. Waylon, and R.E. Orville, 1997: A 10-yr Monthly Lightning Clima- tology of Florida: 1986-95. Weather and Forecasting, 12,439-448
  3. Holle, R H., and Lopez, R E, 1993: Overview of Real-Time Lightning Detection Systems and their Meteorological Uses. NOAA Technical Memorandum ERL NSSL-102, National Severe Storm Laboratory, Norman, Oklahoma, October 1993
  4. Hondl, K.D., and M.D. Eilts, 1994: Doppler radar characteristics of thunderstorm initiation in the Central Florida environment. Mon. Wea. Rev., 122,1818-1836 https://doi.org/10.1175/1520-0493(1994)122<1818:DRSODT>2.0.CO;2
  5. Jayaratne, E.R, C.P.R Sounders, and J. Hallett, 1983: Laboratory studies of the charging of soft hail during ice crystal interactions. Quart. J. Roy. Meteor. Soc., 109, 609-630 https://doi.org/10.1002/qj.49710946111
  6. Krumm, H.C., 1962: Der weltzeitliche tagesgang der gewitterhaufigkeit. Z. Geophys. 28. 85-104
  7. Lee, T.-Y., Y.-Y. Park and Y.-H. Kim, 1998: A numerical modeling study of heavy rainfall development over the Changma front. Proceeding of the International Conference on Monson and Hydrologic Cycle April 22-25, 1998, Kyongju, Korea, 72-75
  8. Lee, T.-Y , Y.-Y. Park , C.-S. Shin, S.-H. Park, and Y.-H. Kim, 2004: A cyclogenesis and heavy rainfall over the Changma front. To be submitted
  9. Lim, E., 2002: Effect of lightning data assimilation on the prediction of precipitation system derived by a cold front. Ph. D. Dissertation, Yonsei University, Seoul, Korea, 148pp
  10. Lim, E, and T.-Y., Lee, 2001: Effect of lightning assimilation on the prediction of precipitation system associate with a cold front. Proceeding of International Conference on Mesoscale Meteorology and Typhoon in East Asia. Taipei, Taiwan, 415-419
  11. Lim, E, Y-S. lung, and J.-C. Nam, 2000: Characteristics of hail occurred in Korea, J. of Korea Water Resources Association, 33, 229-235
  12. Orville, R.E, 1991: Lightning ground flash density in the contiguous United States -1989, Mon. Wea. Rev., 119, 573-577 https://doi.org/10.1175/1520-0493(1991)119<0573:LGFDIT>2.0.CO;2
  13. Orville, R.E, R.W. Henderson, and L.F. Bosart, 1987: Meteorological applications of lightning data, Review of Geophysics, 25, U.S. National Report to International Union of Geodesy and Geophysics 1983-1986, American Geophysical Union, Washington D.C., 411-414
  14. Rust, W.D., D.R MacGorman, and RT. Arnold, 1981: Positive c1oud-to-ground lightning flashes in severe storm. Geophys. Res. Lett., 8, 791-794 https://doi.org/10.1029/GL008i007p00791
  15. Samsury, C.E., and R.E. Orville, 1994: Cloud-to-ground lightning in tropical cyclones: A study of Hurricanes Hugo (1989) and Jerry (1989). Mon. Wea. Rev., 112, 1887-1896
  16. Sheridan, S.C., J.F. Griffiths, and R.E. Orville, 1997: Warm season cloud-to-ground lightning-precipitation relationship in the south-central United States. Wea. and Forecasting, 12,449-458 https://doi.org/10.1175/1520-0434(1997)012<0449:WSCTGL>2.0.CO;2
  17. Shin, C.-S. and T.-Y. Lee, 2004: Development Mechanisms for Heavy Rainfalls of 6-7 August 2002 over the Middle of the Korean Peninsula. J. Meteor. Soc. Japan, in review
  18. Solomon, R, and M. Barker, 1994: Electrification of New Mexico thunderstorms. Mon. Wea. Rev., 122, 1878-1888 https://doi.org/10.1175/1520-0493(1994)122<1878:EONMT>2.0.CO;2
  19. Sun, J., and T. Y. Lee, 2002: A numerical study of an intense quasi-stationary convection band over the Korean Peninsula. J. Meteor. Soc. Japan, 80,1221- 1245 https://doi.org/10.2151/jmsj.80.1221