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Observational Study of Thermal Characteristics by Distribution Ratio of Green Area at Urban in Summer Season

하절기 관측을 통한 도시의 지역별 공간녹지분포율에 따른 열환경 특성 연구

  • Jung, Im-Soo (Dept. of Architecture, Graduate School, Catholic University of Daegu) ;
  • Choi, Dong-Ho (Dept. of Architecture, Catholic University of Daegu) ;
  • Lee, Bu-Yong (Dept. of Environmental Science, Catholic University of Daegu)
  • 정임수 (대구가톨릭대학교 대학원 건축학과) ;
  • 최동호 (대구가톨릭대학교 건축학부) ;
  • 이부용 (대구가톨릭대학교 환경과학과)
  • Received : 2011.04.12
  • Accepted : 2011.04.28
  • Published : 2011.06.30

Abstract

The objective of this study is to analyze the characteristic of thermal environment in the summer season by conducting the field observation of temperature, relative humidity, and globe temperature in some parts of the city. Observation point was divided to a densely populated area, a residential area, a green area, a waterfront green area and a suburban district by the distribution ratio of green area. In this study, the correlation between maximum temperature and globe temperature, study on index for intensity of the tropical night and the temperature distribution characteristic of measurement points by the distribution ratio of green area were analyzed. The results of this study are as follows. (1) The difference between temperature and globe temperature by the distribution ratio of green area is confirmed. The difference of nighttime is more clearly that of daytime. (2) The average temperature and globe temperature of the densely populated area($29.2^{\circ}C$, $33.7^{\circ}C$) are higher than that of the waterfront green area($27.9^{\circ}C$, $32.0^{\circ}C$) by $1.3^{\circ}C$ and $1.7^{\circ}C$, respectively. (3) The number of tropical nights has different days of tropical nights by the distribution ratio of green area of 17days for the Daegu weather station, 14days for adensely populated area, 14days for a residential area, 6days for a green area, 2days for a waterfront green area, and 2days for a suburban district. (4) The results of the slope of trend line for the effects of the temperature on globe temperature change and the intercept for the size of the impact of radiant energy gained around by the analysis of the correlation between the maximum temperature and globe temperature can be utilized objective evaluation index of the each point's artificial effects.

Keywords

References

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