• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2008년도 International Symposium on Remote Sensing
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• pp.68-71
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• 2008

Our goal is to obtain a better scientific understanding how to define the nature and role of remotely sensed land surface parameters and energy fluxes in the heat island phenomena, and local and regional weather and climate. By using the MODIS visible and thermal imagery data and analyzing the surface energy flux images associated with the change of the landcover and landuse in study area, we will estimate and present how significant is the magnitude of the heat island heat effect and its relation with the surface parameters and the energy fluxes in Taiwan. To achieve our objective, we used the energy budget components such as net radiation, soil heat flux, sensible heat flux, and latent heat flux in the study area of interest derived form remotely sensed data to understand the island heat effect. The result shows that the water is the most important component to decrease the temperature, and the more the consumed net radiation to latent heat, the lower urban surface temperature.

• 한국건축시공학회:학술대회논문집
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• 한국건축시공학회 2018년도 춘계 학술논문 발표대회
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• pp.251-252
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• 2018

Cool roof coating materials generally use white color which has the highest reflectance, but it is a tendency to apply various colors because it can cause glare and fatigue of a nearby building user due to the urban beauty and high reflection. This study when applying color diversity material cool roof coating was carried out as a basic research for the degree of solar radiation reflectance change. Experiment result. As a result of the measurement of the reflectance of each specimen, white showed the best reflectance in the near infrared region, and black had the lowest reflectance. Also, in case of brown, it was confirmed that the reflectance of solar radiation in the near extrinsic region is lower than that of gray.

• 국제초고층학회논문집
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• 제2권4호
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• pp.293-314
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• 2013

Double-Skin Façade (DSF), which is a kind of passive indoor environmental control technique, is effective way to control environmental loads while maintaining the transparency especially in perimeter zone and hence the adoption example of DSF keep increasing recently. The objective of this study was to perform a field survey of air quality environment with natural ventilation through DSF and thermal environment within office building with six stories during a mild climate period in Japan. Moreover, to understand the comprehensive environmental performance of the target building, questionnaire survey was conducted to subjectively evaluate the productivity and satisfaction with the environmental factors in office space. In this field measurement, there was a positive correlation between the DSF internal ventilation flow and the amount of solar radiation on the DSF normal surface; the primary driving force for ventilation in the DSF was considered to be the buoyancy force caused by solar radiation. The results of questionnaire survey with regard to productivity level indicated the need for improvement in the thermal (temperature) and spatial environment (room size and furniture placement).

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2003년도 Proceedings of ACRS 2003 ISRS
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• pp.319-321
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• 2003

It is our goal to obtain a better scientific understanding of how to define the nature and role of remotely sensed land surface parameters and energy fluxes in the heat island phenomena, and local and regional weather and climate. By using the TRMM (Tropical Rainfall Measuring Mission) visible and thermal imagery data and analyzing the surface energy flux images associated with the change of the landcover and land use in the study area, we present how significant is the magnitude of the heat island heat effect and its relation with the surface parameters and the energy fluxes in the Taichung area of Taiwan. We used the energy budget components such as net radiation, soil heat flux, sensible heat flux, and latent heat flux in the study area of interest derived form remotely sensed data to understand the island heat effect in Taichung. The results show that water is the most important component to decrease the temperature, and the more the consumed net radiation to latent heat, the lower the urban surface temperature.

• 한국환경과학회지
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• 제30권10호
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• pp.821-831
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• 2021

The relationship between night cooling rate and meteorological elements was investigated over the past five years (2016-2020), using weather data from the new (Daegu(143)) and old (Shinam(860)) Daegu Regional Meteorological Agency located in the suburban and urban regions, respectively. There was a correlation between the total daily amount of solar radiation (S_tot) and the night cooling rate in the both regions. However, a higher correlation was observed at the new Daegu Regional Meteorological Agency station (Daegu(143)). In particular, data from the new Daegu Regional Meteorological Administration's observatory, which experiences a low thermal storage effect caused by artificial structures, showed a higher correlation between nighttime cooling and weather factors. The reason for this is that the lesser the heat storage effect caused by the artificial structures, the better the effect of surface radiation cooling on temperature reduction. These findings confirm that the correlation between night cooling and weather factors can be used to assess the impact of artificial structures in cities.

• Coupled systems mechanics
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• 제11권2호
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• pp.107-119
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• 2022

The aim of the work presented in this paper is development of numerical model for prediction of temperature distribution in pavement according to the measured meteorological parameters, with introduction of non-linear heat transfer coefficient which is a function of temerature difference between the air and the pavement. Developed model calculates heat radiated from the pavement back in the air, which is an important part of the heat trasfer process in the open air surfaces. Temperature of the pavement surface, heat radiation together with many meteorological parameters were measured in series during two years in order to validate the model and calibrate model parameters. Special finite element method for temperature heat transfer towards the soil together with the time integration scheme are used to solve the governing equation. It is proved that non-linear heat transfer coefficient, which is a function of time and temperature difference between the air and the pavement, is required to decribe this phenomena. Proposed model includes heat tranfer coefficient callibration for specific climate region, through the iterative inverse procedure.

• Journal of Radiation Protection and Research
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• 제30권3호
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• pp.99-105
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• 2005

원자력 시설의 사고로 대기로 누출된 방사성 핵종의 도시환경 오염에 따른 사고결과해석을 위한 기본 단계로써 도시환경에 대한 오염평가 모델 METRO-K를 개발하였다. 모델은 3가지 방사성 핵종 $(^{137}Cs,\;^{106}Ru,\;^{131}I)$을 고려하며, 그 중에서 요오드는 3가지 다른 화학적 형태 (입자형태, 유기형태, 원소형태)를 구분하여 다루고 있다. 모델은 도시환경을 구성하는 5가지 주요표면 (지붕, 포장도로, 벽, 잔디/토양, 나무)에 대해 시간에 따른 방사성물질의 농도를 평가한다. 개발된 모델을 사용하여 강우량에 따른 표면의 오염영향과 아울러 체르노빌 사고시 유럽지역에서 측정된 공기중 $^{137}Cs$ 농도와 강우량 자료를 사용한 적용결과를 고찰하였다. 고찰결과 대부분 표면에서 강우량은 오염에 중요한 영향을 나타냈으며, 이러한 영향의 정도는 표면과 핵종에 따라 상이한 결과를 보였다. $^{137}Cs$의 오염은 $^{131}I$ (원소형태)에 비해 강우에 보다 민감한 영향을 나타냈다.

• 한국조경학회지
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• 제42권1호
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• pp.41-49
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• 2014

본 연구는 미국 샌프란시스코시 수목 음영이 개별 건물 지붕 및 옥상에 입사되는 태양에너지 잠재량에 미치는 영향을 LiDAR를 이용한 고해상도 3차원 수치모델을 이용하여 공간적으로 정량화하였다. 최근 분산형 태양광 발전이 기후변화 대응에 중요한 부분으로 주목받고 있으나, 이러한 도심 태양광 발전은 주변부의 지형, 건물, 지붕모양, 수목 등의 음영에 의해 발전량이 제한되는 특성이 있다. 특히 건물 주변의 수목의 경우 도시열섬현상의 저감, 냉난방 에너지 수요량의 절감 등의 순기능과 태양광 발전량 감소의 역기능을 동시에 가지고 있어 두 가지 효용의 상충을 최소화하기 위해 해당 위치에 대한 공간적 분석이 요구된다. 샌프란시스코시 전체 건물 지붕면적의 태양에너지 총량은 년간 18,326,671 MWh으로, 수목의 음영에 의한 감소량은 326,406 MWh로 총량의 1.78%에 해당하였다. 건물지붕의 단위 면적당 일조량은 $34.4kWh/m^2/year$에서 $1,348.4kWh/m^2/year$ 범위로 산출되었다. 본 연구를 통해 도심 수목에 의한 건물별 일조에너지 감소량의 공간자료가 구축되었으며, 개별 건물지붕에 일조량의 변이를 주변 수목의 밀도, 평균수고, 수고의 분산값을 이용한 회귀모델을 통해 설명하였다. 본 연구는 도심수목의 환경적 순기능을 유지함과 동시에 태양광 발전 감소량의 최소화 할 수 있는 방법을 제공함으로써 지속가능한 도시를 구축하는데 기여할 것으로 기대된다.

• 한국토양비료학회지
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• 제45권5호
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• pp.848-852
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• 2012

도시지역의 식물에 의한 도시열섬 현상 저감 효과를 구명하기 위하여 서울, 부산, 대구, 대전, 광주, 수원 등 6개 도시지역의 근래 30년간 (1979-2008) 폭염기의 최고온도, 식물에 의한 온도 하강, 작물 증발산량, 대기오염 방지 기능 등을 조사 분석한 결과는 다음과 같다. 1. 서울, 수원 등 6개 도시의 30년간 (1979-2008) 년 중 폭염기인 7월 하순과 8월 상순의 순 평균최고기온의 평균값은 $35.03^{\circ}C$ 이었다. 2. 6개 도시의 폭염기 (7월하순 - 8월상순) 동안 벼와 콩의 최대 일평균증발산량은 각각 $6.86ton\;10a^{-1}day^{-1}$ 및 $6.00ton\;10a^{-1}day^{-1}$ 이었다. 3. 수원시 중심지에 위치한 도시 농경지의 도시열섬 저감 효과의 지표로 볼 수 있는, 벼 및 콩 군락의 온도와 기온과의 차이는 각각 $10.5^{\circ}C$ 및 $3.0^{\circ}C$ 이었다. 4. 안성시 외각에 위치한 도시농경지에서 폭염기간 동안벼 및 콩 군락과 대기의 온도 차이는 각각 평균 $2.6^{\circ}C$ 및 $2.2^{\circ}C$ 이었다. 5. 2012년 년 중 최고 폭염일 (8월 5일)의 수원시 중심지에 위치한 도시 정원 식물 체 잎 표면온도는 대기온도 대비 $2.0^{\circ}C$, 도시건물 외벽 대비 $14.5^{\circ}C$ 더 낮았다. 6. 수원시 중심지의 식물에 의한 도시열섬 저감효과를 전력량으로 비교하면 벼 5,250. 콩 2,200, 도시정원 식물 $1,000MW\;day^{-1}$ 이었다. 7. 수원시 중심지 폭염기의 작물 증발산량과 잠열에 의한 도시 열섬 현상 저감 효과를 원유의 양으로 비교하면, 벼 462.9, 콩 401.4 L원유 $10a^{-1}day^{-1}$ 이었다. 8. 수원시 중심지 폭염기의 작물에 의한 $CO_2$ 흡수량은, 벼 20.27, 콩 $15.54kg\;CO_2\;10a^{-1}day^{-1}$ 이었다. 9. 수원시 중심지 폭염기의 작물에 의한 $O_2$ 발생량은 벼 14.74, 콩 $11.30kg\;O_2\;10a^{-1}day^{-1}$ 이었다. 10. 수원시 중심지 폭염기의 작물에 의한 오존 농도 저감 효과는 벼 21.0, 콩 8.8 및 도시정원 식물 4.0 ppb 이었다.

• 대기
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• 제27권4호
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• pp.423-433
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• 2017

The spatial and temporal variations in radiative forcing (RF) and mean temperature changes of greenhouse gases (GHGs), such as $CO_2$, $CH_4$, and $N_2O$, were analyzed at urban center (Yeon-dong) and background sites (Gosan) on Jeju Island during 2010~2015, based on a modeling approach (i.e., radiative transfer model). Overall, the RFs and mean temperature changes of $CO_2$ at Yeon-dong during most years (except for 2014) were estimated to be higher than those at Gosan. This might be possibly because of its higher concentrations at Yeon-dong due to relatively large energy consumption and small photosynthesis and also the difference in radiation flux due to the different input condition (e.g., local time and geographic coordinates of solar zenith angle) in the model. The annual mean RFs and temperature changes of $CO_2$ were highest in 2015 ($2.41Wm^{-2}$ and 1.76 K) at Yeon-dong and in 2013 ($2.22Wm^{-2}$ and 1.62 K) at Gosan (except for 2010 and 2011). The maximum monthly/seasonal mean RFs and temperature changes of $CO_2$ occurred in spring (Mar. and/or Apr.) or winter (Jan. and/or Feb.) at the two sites during the study period, whereas the minimum RFs and temperature changes in summer (Jun.-Aug.). In the case of $CH_4$ and $N_2O$, their impacts on the RF and mean temperature changes were very small (an order of magnitude lower) compared to $CO_2$. The spatio-temporal differences in these RF values of GHGs might primarily depend on the atmospheric profile (e.g., ozone profile), surface albedo, local time (or solar zenith angle), as well as their mass concentrations.