• 제목/요약/키워드: urban surface temperature

검색결과 357건 처리시간 0.024초

도시 열환경 분석을 위한 공간정보 빅데이터 구축 (Construction of Spatial Information Big Data for Urban Thermal Environment Analysis)

  • 이준호;윤성환
    • 대한건축학회논문집:계획계
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    • 제36권5호
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    • pp.53-58
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    • 2020
  • The purpose of this study is to build a database of Spatial information Bigdata of cities using satellite images and spatial information, and to examine the correlations with the surface temperature. Using architectural structure and usage in building information, DEM and Slope topographical information for constructed with 300 × 300 mesh grids for Busan. The satellite image is used to prepare the Normalized Difference Built-up Index (NDBI), Normalized Difference Vegetation Index (NDVI), Bare Soil Index (BI), and Land Surface Temperature (LST). In addition, the building area in the grid was calculated and the building ratio was constructed to build the urban environment DB. In architectural structure, positive correlation was found in masonry and concrete structures. On the terrain, negative correlations were observed between DEM and slope. NDBI and BI were positively correlated, and NDVI was negatively correlated. The higher the Building ratio, the higher the surface temperature. It was found that the urban environment DB could be used as a basic data for urban environment analysis, and it was possible to quantitatively grasp the impact on the architecture and urban environment by adding local meteorological factors. This result is expected to be used as basic data for future urban environment planning and disaster prevention data construction.

Quantifying how urban landscape heterogeneity affects land surface temperature at multiple scales

  • Rahimi, Ehsan;Barghjelveh, Shahindokht;Dong, Pinliang
    • Journal of Ecology and Environment
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    • 제45권4호
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    • pp.190-202
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    • 2021
  • Background: Landscape metrics have been widely applied to quantifying the relationship between land surface temperature and urban spatial patterns and have received acceptable verification from landscape ecologists but some studies have shown their inaccurate results. The objective of the study is to compare landscape metrics and texture-based measures as alternative indices in measuring urban heterogeneity effects on LST at multiple scales. Results: The statistical results showed that the correlation between urban landscape heterogeneity and LST increased as the spatial extent (scale) of under-study landscapes increased. Overall, landscape metrics showed that the less fragmented, the more complex, larger, and the higher number of patches, the lower LST. The most significant relationship was seen between edge density (ED) and LST (r = - 0.47) at the sub-region scale. Texture measures showed a stronger relationship (R2 = 34.84% on average) with LST than landscape metrics (R2 = 15.33% on average) at all spatial scales, meaning that these measures had a greater ability to describe landscape heterogeneity than the landscape metrics. Conclusion: This study suggests alternative measures for overcoming landscape metrics shortcomings in estimating the effects of landscape heterogeneity on LST variations and gives land managers and urban planners new insights into urban design.

도로 포장 기술 개선에 따른 대기 경계층의 열 변화에 관한 연구 (A Study on the Impact of an Improved Road Pavement Technology on the Thermal Structure of Atmospheric Boundary Layer)

  • 이순환;김인수;김해동
    • 한국대기환경학회지
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    • 제24권5호
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    • pp.551-561
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    • 2008
  • In order to clarify the impact of anti-heat insulation pavement on the thermal structure of atmospheric boundary layer, field experiments and numerical simulations were carried out. Field experiment with various pavements were also conducted for 24 hours from 09LST 19 June 2007. And numerical experiment mainly focused on the impact of albedo variation, which is strongly associated with thermal characteristics of insulated pavement materials, on the temporal variation of planterly boundary layer. Numerical model used in this study is one dimension model with Planterly Boundary Layer developed by Oregon State University (OSUPBL). Because anti-heat insulation pavement material shows higher albedo value, not only maximum surface temperature but also maximum surface air temperature on anti-heat insulation pavement is lower than that on asphalt. The maximum value of surface temperature only reach on $49.5^{\circ}C$. As results of numerical simulations, surface sensible heat flux and the height of mixing layer are also influenced by the values of albedo. Therefore the characteristics of urban surface material and its impact on atmosphere should be clarified before the urban planning including improvement of urban heat environment and air quality.

도시 지표면 온도분포 특성 및 열섬완화방안 (A Study on the Distribution Characteristic of Urban Surface Temperature and Urban Heat Island Effects)

  • 도후조;이정민;나정화
    • 한국환경과학회지
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    • 제16권5호
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    • pp.611-622
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    • 2007
  • The purpose of this research was to three-criteria landuse-pattern, developing density, NDVI which were related to the heat island and find the distribution characteristic of urban surface temperature and urban heat island effects. The results of this study were as follows. According to the analysis of surface temperatures, the first grade was the outside-city like a mountain and its temperature was less than $12.18^{\circ}C$. The fifth grade was the downtown industrial area and its temperature was more than $23.54^{\circ}C$. It means Daegu-Metropolitan-City has the serious heat-island effect. the results of landuse pattern analysis, in case of fifth and forth grade, city area was occupied over 90% with residential, commercial and industrial areas, but in case of third grade, openspace was occupied over 70%. The results of developing density analysis, the temperature had high correlation with building ratio, road ratio, vegetation ratio and etc. To plan for the decrease of heat island effect needed the extension of green space, decrease of paving, but there was a limit to get the objective method for grade classification because of lacking in the basic data, the research of criteria will be accomplished continuously.

도시성장모델을 적용한 수도권 미래 기후변화 예측 (Prediction of Future Climate Change Using an Urban Growth Model in the Seoul Metropolitan Area)

  • 김현수;정주희;오인보;김유근
    • 한국대기환경학회지
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    • 제26권4호
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    • pp.367-379
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    • 2010
  • Future climate changes over the Seoul metropolitan area (SMA) were predicted by the Weather Research and Forecasting (WRF) model using future land-use data from the urban growth model (SLEUTH) and forecast fields from ECHAM5/MPI-OM1 GCM (IPCC scenario A1B). Simulations from the SLEUTH model with GIS information (slope, urban, hill-shade, etc.) derived from the water management information system (WAMIS) and the intelligent transportation systems-standard nodes link (ITS-SNL) showed that considerable increase by 17.1% in the fraction of urban areas (FUA) was found within the SMA in 2020. To identify the effects of the urban growth on the temperature and wind variations in the future, WRF simulations by considering urban growth were performed for two seasons (summer and winter) in 2020s (2018~2022) and they were compared with those in the present (2003~2007). Comparisons of model results showed that significant changes in surface temperature (2-meter) were found in an area with high urban growth. On average in model domain, positive increases of $0.31^{\circ}C$ and $0.10^{\circ}C$ were predicted during summer and winter, respectively. These were higher than contributions forced by climate changes. The changes in surface temperature, however, were very small expect for some areas. This results suggested that surface temperature in metropolitan areas like the SMA can be significantly increased only by the urban growth during several decades.

NOAA/AVHRR 위성자료를 이용한 한반도 표면온도의 시공간적 변동 추정 (Estimation of the Temporal and Spatial Variation of Surface Temperature Distribution in the Korean Peninsula using NOAA/AVHRR Data)

  • 서영상;이기철;이나경;조명희
    • 한국지리정보학회지
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    • 제8권3호
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    • pp.150-160
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    • 2005
  • 1991년, 1995년 및 2000년의 NOAA/AVHRR 위성자료와 split-window 방법을 사용하여 한반도 표면온도의 시공간적인 변동을 분석하였다. 한반도 전지역의 낮과 밤의 온도차는 $3{\sim}15^{\circ}C$로 나타났다. 대도시에서 온도차의 계절적 변동과 년별 변동은 교외지역보다 낮게 나타났으며, 도시화의 영향이 분명하게 나타났다. 도시열섬 영향의 특성은 대도시 부산에서 낮과 밤의 온도차를 근거로 알 수 있었다. 또한 북한 및 남한에서 하계 $30^{\circ}C$ 이상 고온을 나타내는 20개 도시 지역을 모니터링 할 수 있었다. 도시환경계획을 위해 본 기술의 사용을 제안한다.

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도시열섬완화를 위한 토지 이용 유형별 합리적 녹지율 분석 (An Analysis of Rational Green Area Ratio by Land Use Types for Mitigating Heat-Island Effects)

  • 송봉근;박경훈
    • 한국지리정보학회지
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    • 제18권2호
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    • pp.59-74
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    • 2015
  • 본 연구는 다양한 토지이용유형별로 도시열섬현상을 완화하기 위한 합리적 녹지율을 분석하고자 하였다. 토지이용유형은 단독주택과 공동주택, 공공시설, 상업지역, 공업지역의 5가지 유형을 고려하였고, 녹지지역은 토지피복도에서 수목 속성을 추출하여 활용하였다. 열섬효과는 주간 및 야간에 촬영된 다중시기의 ASTER TIR 영상의 표면온도를 이용하였다. 주간시간은 야간시간보다 녹지의 표면온도 저감 효과가 큰 것으로 나타났다. 토지이용유형별로는 주간시간에 단독주택에서 녹지율에 따른 표면온도 저감효과가 가장 뚜렷했지만, 야간시간에는 토지이용유형별로 차이가 크지 않았다. 공업지역은 녹지의 표면온도 저감 효과가 낮았다. 토지이용유형별 도시열섬완화를 위한 합리적 녹지율을 산출한 결과, 주간시간은 단독주택과 공동주택, 상업지역에서 녹지율이 40~50% 사이일 때, 표면온도가 가장 낮았고, 야간시간은 녹지율별로 표면온도 변화가 크지 않았다. 따라서 본 연구의 결과는 도시개발계획 단계에서 도시열섬완화를 위해 효과적인 녹지면적을 제시할 수 있을 것으로 판단된다.

Landsat 위성영상을 활용한 재건축 지역의 지표 온도 변화에 관한 연구 : 서울특별시 강동구의 고덕동과 둔촌동을 중심으로 (A Study on Land Surface Temperature Changes in Redevelopment Area Using Landsat Satellite Images : Focusing on Godeok-dong and Dunchon-dong in Gangdong-gu, Seoul)

  • 한지훈;손철
    • 한국지리정보학회지
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    • 제26권2호
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    • pp.42-54
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    • 2023
  • 우리나라 대도시 지역에 인구가 집중되고 이에 따른 수요를 충족시키기 위하여 저밀도 주거지가 재개발·재건축을 통하여 고밀도 주거지화 되고 있다. 그러나 단시간에 이루어진 대규모의 재건축은 도시녹지 면적 감소에 의한 열섬현상을 발생시키는 등 도시 기후에 부정적인 영향을 끼치게 된다. 본 연구에서는 Landsat 8 위성영상을 활용하여 서울특별시 강동구 고덕동, 둔촌동 재건축 지역의 2013년에서 2022년까지의 지표 온도의 변화를 분석하였다. 고덕동 지역에서는 재건축이 진행되는 대상지와 산림지역, 산림과 시가지가 혼재된 지역, 저층주거지역에 대한 지표 온도의 차이를 분석하였으며, 둔촌동 지역에서는 대상지와 산림지역, 저층주거지역에 대한 지표 온도의 차이를 분석하였다. 분석은 지표 온도 차이에 대한 다중회귀분석을 통하여 진행되었다. 고덕동 지역과 둔촌동 지역에서 공통적으로 재건축 전단계까지 전반적으로 지표 온도가 산림보다 높고 저층주거지역보다 낮게 나타났다. 이러한 특징들은 고덕동, 둔촌동의 저층주거지역이 대상지보다 녹지율이 낮고 건폐율이 높기 때문에 발생하였음을 알 수 있다. 본 연구를 통해 저밀도 지역이 고밀도화가 되더라도 녹지와 건폐율을 적절하게 관리한다면 도시열섬현상을 완화시킬 수 있음을 알 수 있다.

A Preliminary Analysis of the Impact of Urban Green Spaces on the Urban Heat Island Effect Using a Temperature Map

  • Myeong, Soo-Jeong
    • 대한원격탐사학회지
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    • 제26권6호
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    • pp.675-680
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    • 2010
  • Temperature is one of the main issues in climate change, and the urban heat island effect in highly developed urban areas is an important issue that we need to deal with. This study analyzed the extent of the cooling effects of urban green spaces. The study used a surface temperature map of Seoul. It found that the cooling effects of green space was observed within limited distances, although it varied a little depending on the parks investigated. The cooling effect distance ranged from 240m to 360m, averaging about 300m. It also found the size of an urban green space does not make much difference in cooling the surrounding areas. Although further investigation with diverse urban areas should be conducted on this matter, the results did imply that many small green spaces in the neighborhood are more effective than a single big green space in mitigating the heat island effects of cities.

알베도 증가에 따른 도시 기온 하강 효과에 관한 수치연구 (Numerical Study on the Air Cooling Effect due to Increased Albedo in Urban Area)

  • 이현주;이귀옥;이순환;이화운
    • 한국대기환경학회지
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    • 제24권4호
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    • pp.383-392
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    • 2008
  • In order to clarify the influence of the change of urban surface albedo on mesoscale meteorological factors during the summertime, numerical experiments with various albedo of urban surface were carried out. Numerical model used in this study is PSU/NCAR MM5 V3.6. As a result of the numerical simulation intended of Busan assumed the increase of albedo of roofs, buildings, or roads, the increase of albedo can make decrease radiation effect of surface, so that it caused drops in ambient air temperature from $0.5^{\circ}C$ to $1^{\circ}C$ on the average, and the downtown of Busan formed along the trough presented a substantial drop in ambient air temperature about $1.5^{\circ}C$. Modeling studies suggest the increased surface albedo in urban area can reduce surface and air temperatures near the ground and affect related meteorological parameters such as winds and the depth of the mixed boundary layer.