Journal of the Korean Society of Environmental Restoration Technology (한국환경복원기술학회지)

The Korea Society of Environmental Restoration Technology (한국환경복원기술학회)
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A Study on Nocturnal Inversion at Urban Area in Winter

동절기 도심지 야간 기온역전에 관한 연구

  • Zheng, Hai-Yan (Department of Landscape Architecture, Sungkyunkwan University) ;
  • Lee, Kyoo-Seock (Department of Landscape Architecture, Sungkyunkwan University)
  • 정해연 (성균관대학교 조경학과 대학원) ;
  • 이규석 (성균관대학교 조경학과)
  • Received : 2009.12.28
  • Accepted : 2010.02.02
  • Published : 2010.02.01
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Abstract

In urban area, inversion layer prevents air pollutants from being dispersed. To determine nocturnal inversion characteristics at SookMyung Girls' High School near high-rise residential commercial complex buildings in Seoul, air temperature and humidity data were observed at 10minute interval from December 1st, 2007 to May 2nd, 2008. Temperature-Humidity (T-H) sensors were installed at SMG (SookMyung_Ground) and SMR (SookMyung_Roof), and then these two data were compared, analyzed and examined to illustrate air temperature differences of SMG and SMR. After the analysis, the maximum nocturnal inversion was observed by $3.3^{\circ}C$ at 18:10 on December 26th 2007, at that time the weather condition was clear and weak wind. Nocturnal inversions began 2-3 hours before sunset and it reached maximum inversion just after sunset and continued through nighttime until sunrise or 1-2 hours after sunrise. In terms of seasonal variation nocturnal inversions occurred dominantly in March and April rather than winter season.

Keywords

References

  1. 이부용.김두석.문승의. 1994. 일본 쯔쿠바에서의 한후기 동안 기온역전의 특성에 관한 연구. 한국환경과학회지 3(3)：217-228.
  2. 이지연.이동인.한영호.옥곡. 1997. 기온 역전 발생에 따른 대기경계층에서의 $O_{3}$, $NO_{2}$ 농도의 연직분포에 관한 연구. 한국기상학회지 33(2)：315-326.
  3. 정유란.서희철.윤진일. 2003. 구릉지 과원의 고도에 따른 기온변이. 한국농림기상학회지 5(1)：43-47.
  4. Ahrens, D. C. 2008. Essentials of Meteorology. An Invitation to the Atmosphere 5th ed. Belmont. Thomson Learning Inc.
  5. Demarrais Gerard A. 1960. Vertical Temperature Difference Observed over an Urban Area. bulletin American Meteorological Society, 42(8)：548-554
  6. Godowitch, J. M., Ching, J. K. S., and Clarke, J. F. 1985. Evolution of the Nocturnal Inversion Layer at an Urban and Nonurban Location. Journal of Applied Meteorology, 24(8)： 791-804. https://doi.org/10.1175/1520-0450(1985)024<0791:EOTNIL>2.0.CO;2
  7. Landsberg, Helmut E. 1981. The urban climate. Academic Press. pp.20-21, p.54.
  8. Oke, T. R. 1987. Boundary Layer Climates, 2nd ed. Routledge. p.288.
  9. Oke, T. R. 2004. Initial guidance to obtain representative meteorological observations at urban sites. IOM Report NO.81, WMO/TD NO.1250, Geneva：World Meteorol Organization.
  10. Ologson, K., Frans G., Andersson Patrik U., Hallquist Mattias, Ljungstrom Evert, Lin tang, Deliang Chen, and Pettersson Jan B. C. 2009. Urban aerosol evolution and particle formation during wintertime temperature inversion. Atmospheric Environment, 43(2)：340- 346. https://doi.org/10.1016/j.atmosenv.2008.09.080
  11. Serreze, Mark C., Kahl, Jonathan D., and Schnell, Russell C. 1992. Low-level Temperature Inversions of the Eurasian Arctic and Comparisons with Soviet Drifting Station Data. American Meteorological Society, 5(6)： 615-629
  12. Whiteman, C. David, Xindi Bian and Shiyuan Zhong. 1999. Wintertime Evolution of the Temperature Inversion in the Colorado Plateau Basin. Journal of Applied Meteorology, 38(8)：1103-1117. https://doi.org/10.1175/1520-0450(1999)038<1103:WEOTTI>2.0.CO;2
  13. http://www.kma.go.kr/sfc/sfc_03_05.jsp 기상청.
  14. http://www.kasi.re.kr/Knowledge/sunmoon_map.aspx 한국천문연구원.
  15. http://www.google.com Google Earth.