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울릉도 온실기체 관측자료를 이용한 배경대기 평균농도 산정

An Estimation of Mean Background Concentrations of Greenhouse Gases Observed on Ulleungdo

  • 임윤규 (한국교원대학교 환경교육과) ;
  • 문윤섭 (한국교원대학교 환경교육과) ;
  • 김진석 (한국표준과학연구원 대기환경표준센터) ;
  • 송상근 (부산대학교 지구환경시스템학부) ;
  • 홍지형 (국립환경과학원 대기공학연구과)
  • Lim, Yun-Kyu (Department of Environmental Education, Korea National University of Education) ;
  • Moon, Yun-Seob (Department of Environmental Education, Korea National University of Education) ;
  • Kim, Jin-Seog (Cent for gas analysis, Korea Research Institute of Standards and Science) ;
  • Song, Sang-Keun (Division of Earth Environmental System, Pusan National University) ;
  • Hong, Ji-Hyung (Atmospheric Engineering Research Division, National Institute of Environmental Research)
  • 투고 : 2011.11.10
  • 심사 : 2012.02.21
  • 발행 : 2012.02.29

초록

본 연구에서는 울릉도 온실기체 관측장비(CRDS)에서 관측된 $CO_2$$CH_4$ 농도를 정형화된 QA${\cdot}$QC 처리절차를 통해 온실기체 평균 배경대기 농도값으로 활용하기 위한 정확도를 향상시켰다. QA${\cdot}$QC 처리절차는 총 3단계로 구성되었다. 첫 번째는 관측자료의 시간별 평균값을 구하기 위한 물리적 한계검사, 기후범위 검사 및 1시간 측정 자료수가 50% 이하인 자료는 제외시키는 과정으로 이루어져 있다. 두 번째는 일평균자료 산출을 위한 단계검사, 앞뒤로 같은 값일 경우는 제외, 하루 중 관측횟수가 15회 이상 및 일관측 자료의 표준편차가 일표준편차 평균의 3배 이하인 자료만 허용하는 과정이다. 세 번째는 기후적 특성분석 활용을 위한 Curve-fitting methods를 이용한 FFT 적용단계이다. 이상의 QA${\cdot}$QC 절차에 의한 $CO_2$$CH_4$의 월평균농도 값을 안면도 지구대기감시센터 자료와 일본 료리 관측자료와 비교 분석한 결과 $CO_2$에 있어서는 울릉도 관측자료 누락에 의한 영향이 다소 크게 나타나 안면도 관측값이 배경대기 평균농도 값으로 유효하였고, $CH_4$는 안면도 보다 오히려 울릉도 관측값이 한반도 배경대기 평균농도 값으로 더 적절한 것으로 추정되었다.

Mean background concentrations of greenhouse gases such as $CO_2$ and $CH_4$ were estimated on Ulleungdo using PICARRO Cavity Ring-Down Spectroscopy (CRDS) analyzer. To improve the accuracy of $CO_2$ and $CH_4$ concentrations, a standardized QA${\cdot}$QC (Quality Assurance Quality Control) procedure was employed with three steps: 1) the inspection procedure of physical limitation (e.g. the exclusion of data corresponding to the number of data of ${\leq}$50%) for hourly mean values, 2) a stage inspection (e.g. the use of data corresponding to ${\geq}15$ observations per day) for daily mean values, and 3) a fast fourier transform (FFT) analysis using curve-fitting methods for the investigation of climatic characteristics. The monthly mean concentrations of $CO_2$ and $CH_4$ derived from three-step QA${\cdot}$QC procedure were then compared with those observed at Anmyundo (Korea) and Ryori (Japan). Overall, the error of mean $CO_2$ and $CH_4$ concentrations estimated in this study distinctly decreased. However, in comparison with their concentrations monitored at Ryori, the $CO_2$ concentration at estimated at Ulleungdo is soemwhat lower than that of Anmyundo due to the missing data, which is statistically significant. On the other hand, the former has a statistically significant higher value of $CH_4$ that of the latter.

키워드

참고문헌

  1. 기상청 관측국 기술노트, 2006, 기상관측자료 실시간 품질 관리시스템(I) 활용법, 2006-2.
  2. 기상청, 2007, 지구대기감시보고서, 기상청.
  3. Cho, C.H., Kim, J.S., and Yoo, H.J., 2007, Atmopheric carbon dioxide variations at Korea GAW center from 1999 to 2006, Journal of the Korean Metrorological Society, 43, 359-365.
  4. Conway, Y.J., Tans, P.P., Waterman, L.S., Thoning, K.W., Kitzis, D.R., Masarie, K.A., and Zhang, Ni, 1994, Evidence for interannual variability of the carbon cycle from the National Oceanic and Atmosphric Administration/Climate Monitoring and Diagnostics Laboratory Global Air Sampling Network, Journal of Geophysical Research, 99, 22831-22855. https://doi.org/10.1029/94JD01951
  5. JMA, 2007, Observation Results for 2005, Annual Report on Atmospheric and Marine Environment Monitoring No.7, Japan Meteorological Agency.
  6. Keeling, C.D., Bacastow, R.B., Bainbridge, A.E., Ekdahl, C.A., Guenther, P.R., Waterman, L.S., and, Chin, J.F.S., 1976, Atmosphric carbon dioxide variations at Mauna Loa observatoty, Hawaii, Tellus, 28, 538-551 https://doi.org/10.1111/j.2153-3490.1976.tb00701.x
  7. Keeling, C.D., Bacastow, R.B., Carter, A.F., Piper, S.C., Whorf, T.P., Heimann, M., Mook, W.G., and Roeloffzen, H., 1989, A three-dimensional model of atmospheric $CO_{2}$ transport based on observed winds, 1. Analysis of observational data, Geophysical Monograph, 55, 65-236.
  8. Keeling, C.D., Whorf, T.P., Wahlen, M., and van der Plicht, J., 1995, Interannual extremes in the reate of rise of atmospheric carbon dioxide since 1980, Nature, 375, 666-670. https://doi.org/10.1038/375666a0
  9. Masarie, K.A. and Tans, P.P., 1995, Extension and integration of atmospheric carbon dioxide data into globally consistent measurement record, Journal of Geophysical Research, 100, 11593-11610. https://doi.org/10.1029/95JD00859
  10. Thoning, K.W., Tans, P.P., and Komhyr, W.D., 1989, Atmospheric carbon dioxide at Mauna Loa observatory, 2. Analysis of the NOAA GMCC data, 1974-1985, Journal of Geophysical Research, 94, 8549-8565. https://doi.org/10.1029/JD094iD06p08549
  11. WMO, 2006, WMO WDCGG DATA SUMMARY, WDCGG No. 30, Volume IV-Greenhouse Gases and Other Atmospheric Gases, JMA, 88pp.