Recent EUV-B Observation at KGAWO : A Summary Report

지구대기감시관측소에서의 최근 EUV-B 관측 결과

Song, Byung-Hyun;Hong, Gi-Man;Choi, Byoung-Chol;Cho, Hi-Ku
송병현;홍기만;최병철;조희구

  • Published : 2005.06.30

Abstract

Erythemally Weighted Untraviolet B (EUV-B) irradiance data measured every 10 minutes from 1999 to 2004 with UV-Biometer(Solar Light Model 501) at Korea Global Atmosphere Watch Observatory (KGAWO) was analysed and discussed. So the EUV-B intensity is mainly depends on solar zenith angle and total ozone amounts on clear day condition, the daily maximum occurs near solar noon time and the highest monthly accumulated EUV-B shows in July at KGAWO. The maximum daily variation occurs in July due to precipitation and clouds. 6-year trend of EUV-B shows slightly in decreasing. About above 50% of days on summer noontime EUV-B the UV index marked higher than category high or extremely high. We analyzed the relationship of EUV-B and total ozone observed in Seoul. Coincident relationship between ozone depletion and EUV-B increase could not be found with these data sets. Another EUV-B data measured in Pohang was analysed in order to comparison with the KGAOW data. There was no significant difference between two data set of clear day.

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References

  1. 기상연구소, 1996: 자외선 지수 예보법 개발 연구(I), 기상 연구소 기본연구보고서, MR96F0-03, 91pp
  2. 기상청, 2003: 지구대기감시보고서 2002, 88pp
  3. 기상청, 2004: 지구대기감시보고서 2003, 72pp
  4. 기상청, 산업기상정보 허브(자외선지수 발표 홈페이지), http://industry.kma.go.kr/APP $_{}$_APP12.htm
  5. 조희구, 이방용, 이준석, 박선옥, 2001: 한국 전역의 홍반 자외선 복사의 계절기후. 한국기상학회지, 37, 525- 539
  6. 조희구 등, 1996: 한국 상공의 오존층 감시. 연세대학교 지구환경연구소, 환경부-과학기술처 G7사업보고서, 103pp
  7. 태안군, 2005: 태안군 통계연보 2004, 충청남도 태안군 발행 군 종합 통계(2005년 6월 발간 예정)
  8. Koepke, P., J. Reuder and J. Schween, 2004: UV RADIATION IN PAST AND FUTURE - Modelling with all atmospheric parameters including clouds, Proceedings of International Radiation Symposium (IRS 2004), Busan, Korea, 158-159
  9. Long, C. S., A. J. Miller, H. T. Lee, J. D. Wild, R. C. Pazywarty, and D. Hufford, 1996: Ultraviolet Index Forecast Issued by the National Weather Service. Bill. of Amer. Met. Soc., 77, 729-748 https://doi.org/10.1175/1520-0477(1996)077<0729:UIFIBT>2.0.CO;2
  10. Madronich, S., L. O. Bjorn, M. Ilyas, and M. M. Caldwell, 1991: Change in biologically active ultraviolet radiation reaching the Earth's surface. Environmental Effects of Ozone Depletion : 1991 Update, UNEP, Nairobi, Kenya, 1-13
  11. Mckenzie, R. L., W. A. Mattews and P. V. Johnson, 1991; The relationship between erythemal UV and ozone, derived from spectral irradiance measurements. Geophys. Res. Lett., 18, 2269-2272 https://doi.org/10.1029/91GL02786
  12. Mims, F. M. and J. E. Frederick, 1994; Cumulus clouds and UV-B. Nature, 371, 291
  13. Nack., M. L. and A. E. S Green, 1974; Influence of clouds, haze, and smog on the middle ultraviolet reaching the ground. Appl. Opt., 13, 2405-2415 https://doi.org/10.1364/AO.13.002405
  14. Solar Light, 1993: UV-Biometer User`s Manual. Solar Light Co. 459pp
  15. UNEP/WMO, 1999: Scientific Assesments of Ozone Depletion: 1998, Global Ozone Research and Monitoring Project-Report No. 44, Geneva
  16. WCRP, 1997: Proceedings of the First Sparc General Assembly. Vol. 2, WCRP-90, WMO/TD-No. 814, 669pp
  17. WMO, 1994: Report of the WMO meeting of experts on UV-B measurements, data quality and standardization of UV-indices. WMO report No. 25, Les Diablerets, Switzerland
  18. WMO, 1995: WMO Antarctica Ozone Bulletin, 7/95