• 한국태양에너지학회 논문집
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• 제31권3호
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• pp.133-144
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• 2011

The objective of this study is to analyze the characteristic of radiation environment in the urban and rural through the field observation in the summer. The radiation balance was compared through the measurement of the shortwave radiation and long-wave radiation in the urban, sub-urban, and rural. The following conclusion could be obtained from this research. (1)In the results of observation including the rain-day, it was found that the short wave radiance in the urban is lower about 10% than the rural. (2)The upper part of atmosphere layers in the urban are aabsorb much short wave radiation energies compared with the rural relatively. It can increase the temperature of the upper part of atmosphere layers and the emittance of long wave radiation. (3)The ratio of the downward short wave radiation to the downward long wave radiation was 1.24 for the urban, 1.28 for sub-urban and 1.35 for rural. It can be estimated that the atmosphere condition of the rural is better than that of other areas. (4)The net radiation of the rural was lower that of the urban. It was found that the energy in and outflow of the rural is easier than that of the urban. (5)The temperature variation for the long-wave radiation change of the rural showed more sensitive than that of the urban. It was came from the radiation characteristics of the surrounding environment and can be used as the important index to evaluate the thermal environment characteristic of urban.

• 한국태양에너지학회:학술대회논문집
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• 한국태양에너지학회 2011년도 추계학술발표대회 논문집
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• pp.105-110
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• 2011

The objective of this study is to analyze the characteristic of radiation environment in the urban and rural through the field observation in the summer. The radiation balance was compared through the measurement of the shortwave radiation and long-wave radiation in the urban, sub-urban, and rural. The following conclusion could be obtained from this research. (1) In the results of observation including the rain-day, it was found that the short wave radiance in the urban is lower about 10% than the rural. (2) The upper part of atmosphere layers in the urban area absorb much short wave radiation energies compared with the rural relatively. It can increase the temperature of the upper part of atmosphere layers and the emittance of long wave radiation. (3) The ratio of the downward short wave radiation to the downward long wave radiation was 1.24 for the urban, 1.28 for sub-urban and1.35 for rural. It can be estimated that the atmosphere condition of the rural is better than that of other areas.

• 대한설비공학회:학술대회논문집
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• 대한설비공학회 2009년도 하계학술발표대회 논문집
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• pp.565-572
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• 2009

Deterioration of the outdoor thermal environment in urban areas such as heat island has become worse due to urbanization and overpopulation, etc. In this study, a new method which is coupled simulation of convection and radiation to evaluate outdoor thermal environment in urban area will be proposed. Because the solar radiation affects on outdoor thermal environment massively, therefore the radiation calculation is very important in outdoor thermal environment prediction. The coupled simulation proposed in this study can assess the outdoor thermal environment with accurate.

• 한국태양에너지학회 논문집
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• 제32권4호
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• pp.71-81
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• 2012

This study for the understanding of the radiation environment according to the altitude in urban area in the summer observes the long and short wave radiation environment at the 4 urban areas with different height and the 1 suburban area. The results of this study are as follows. (1) When the altitude was high, the more short wave radiation was observed. (2) As the altitude was high, the temperature of atmosphere got lower. And because of that the downward long wave radiation was also lower. This general trend was confirmed through the study. (3) Through the observation of long wave radiation, the upper atmosphere of suburban area had the atmosphere characteristic which the temperature was rising and decreasing faster. Therefore, the difference radiation characteristics between the urban and suburban area were confirmed. (4) The result of the ratio of short wave radiation to long wave radiation(short wave radiation/long wave radiation) according to the altitude and location, the value was increased when the distance was far from the artificiality structure or a heat source, and the urban effect became smaller. Thus, it is expected that the ratio will be an evaluation index for evaluating urbanization effect.

• Journal of Radiation Protection and Research
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• 제36권3호
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• pp.148-153
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• 2011

국제원자력기구(IAEA)에서 주관하는 국제비교프로그램 EMRAS-2(Environmental Modelling for RAdiation Safety, Phase 2) 내 도시오염평가분과에서 설계한 가상 방사능오염 시나리오에 대해 국내모델 METRO-K를 사용하여 도시환경을 구성하는 오염표면의 선량률에 대한 중요도를 분석하였다. 선량률에 대한 오염표면의 기여는 평가위치와 사건 발생 후 시간에 따라 뚜렷이 다른 차이를 나타냈다. 또한 사건이 발생한 당시 강우의 유무와 강우의 강도에 따라서도 오염표면의 기여는 뚜렷한 차이를 나타냈다. 결과적으로 만일 원자력발전소의 사고나 방사능분산장치의 폭발 등과 같은 불의의 사건이 발생하여 도시지역을 오염시킬 경우 방사능피폭에 따른 인체 위해 뿐 아니라 경제적 사회적 영향을 최소화하기 위해서는 해당 환경을 구성하고 있는 표면의 특성을 고려하여 적절한 대응행위를 선택하는 것이 중요하다는 사실을 알 수 있었다.

• 한국태양에너지학회:학술대회논문집
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• 한국태양에너지학회 2012년도 춘계학술발표대회 논문집
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• pp.134-139
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• 2012

This study observed downward long and short-wave radiant environment with selecting 4 areas which have different height in downtown and 1 suburban area to figure out the characteristic of radiant environment in each altitude. The purpose of this study is to collect the preliminary data for interpreting urban thermal environment in summer season by analyzing thermal characteristic of atmosphere in the upper of downtown. The results of this study are as follows. 1) The higher altitude has the lower temperature, and temperature difference was more huge in day time than night time. 2) The short wave radiation according to altitude was higher as altitude was high. 3) Generally, the higher altitude has the lower air temperature, and also the higher altitude has the lower downward long wave radiation by the atmospheric radiation. 4) The ratio short wave radiation of long wave radiation was lower as altitude was high. And the urbanization effect was higher as the ratio was low.

• 한국태양에너지학회 논문집
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• 제37권4호
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• pp.13-22
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• 2017

In this study, long and short-wave radiations were observed in urban and suburban areas during the summer season, and frequency analysis was performed for each radiation intensity by a new analysis method. The following results were obtained. (1) Long-wave radiation values were found to be larger in the afternoon than in the morning, in both urban and suburban areas, unlike short-wave radiation values. (2) Short-wave radiation showed a right-skewed frequency distribution. In the high energy area greater than $900W/m^2$, the frequency was significantly higher in the suburbs than in the urban areas. (3) Long-wave radiation was in the range of $290{\sim}479W/m^2$, its frequency distribution resembled a normal distribution, and the frequency of 410, $420W/m^2$ was the highest.

• 한국지구과학회지
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• 제39권1호
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• pp.89-102
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• 2018

차세대도시농림융합기상사업단의 에너지수지타워 관측자료를 이용하여 수도권 기상과 복사특성에 대하여 분석하였다. 서울 수도권에 위치한 총 14개 에너지수지타워의 기온, 풍속, 상대습도, 지표면 온도, 강수량, 단파 및 장파 복사량과 복사관측자료를 이용하여 산출한 알베도와 방출률을 분석하였다. 월별 자료에 따르면, 도시에 위치한 중랑지점에서 알베도는 낮고 방출률은 높은 특성을 나타냈고 교외지역인 부천지점에서는 반대의 특성이 나타났다. 자연적인 지표상태에서는 태양복사에너지를 효과적으로 반사하여 대부분 중랑지점보다 알베도가 높게 나타났다. 연 평균 기온이 비교적 높게 나타난 지점들은 서울 도심에 위치하고 있었으며, 알베도가 대체적으로 낮게 분포되었다. 가좌지점과 뚝섬지점은 관측 기온이 높았지만, 관측소 주변 유리벽 건물 및 한강으로 둘러싸인 환경으로 알베도가 비교적 높게 나타났다. 교외지역에 위치하고, 기온이 낮았던 지점들은 대체로 낮은 방출률을 나타냈다. 그 중 부천지점에서는 다소 높은 방출률이 나타났는데, 이는 관측지점 주변이 논과 밭으로 구성되어 있어 교외지역의 관측지점보다 지표면 온도가 상대적으로 낮게 관측되었기 때문이다. 결과적으로 도심지일수록 알베도는 감소하고, 방출률은 증가하는 경향을 확인할 수 있다. 또한, 서울 지역의 순 복사량이 $100Wm^{-2}$ 이하로 나타나 에너지가 대기 중에 흡수된 것으로 볼 수 있다.

• 한국태양에너지학회 논문집
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• 제33권4호
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• pp.101-110
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• 2013

The propose of this study is to understand the phenomenon of radiation and comparison of analysis of two methods. One is analysis method of same-time data and the another is analysis method of rank data. We confirmed that two methods of correlation analysis had the effectiveness and suitability. The followings are main results from this study. 1) The seasonal correlation coefficient of long and short-wave radiation is higher in winter than in summer because of high humidity in the summer season can makes easily cloud in the sky locally. 2) According to analysis method, there is big difference in correlation coefficient from 0.494(Analysis method of same-time data) to 0.967(Analysis method of rank data) with short-wave radiation by the location during summer. These results have significant value in solar radiation research and analysis. It has explored a new way for solar radiation research of analysis method as well.

• 한국환경복원기술학회지
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• 제26권1호
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• pp.47-59
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• 2023

Due to climate change and urbanization, abnormally high temperatures and heat waves are expected to increase in urban and deteriorate thermal comfort. Planting of street trees and changing the albedo of urban surfaces are the strategies for mitigating the thermal environment of urban, and both of these strategies affect the exposure and blocking of radiative fluxes to pedestrians. After measuring the shortwave and longwave radiation according to the ground surface with different albedo and the presence of street trees using the CNR4 net radiometer, this study analyzed the relationship between this two strategies in terms of thermal environment mitigation by calculating the MRT(Mean Radiant Temperature) of each environment. As a result of comparing the difference between the downward shortwave radiation measured under the right tree and at the control, the shortwave radiation blocking effect of the tree increased as the downward shortwave radiation increased. During daytime hours (from 11 am to 3 pm), the MRT difference caused by the albedo difference(The albedo of the surfaces are 0.479 and 0.131, respectively.) on surfaces with no tree is approximately 3.58℃. When tree is present, the MRT difference caused by the albedo difference is approximately 0.49℃. In addition, in the case of the light-colored ground surface with high albedo, the surface temperature was low and the range of temperature change was lower than the surrounding surface with low albedo. This result shows that the urban thermal environment can be midigate through the planting of street trees, and that the ground surface with high albedo can be considered for short pedestrians. These results can be utilized in planning street and open space in urban by choosing surfaces with high albedo along with the shading effect of vegetation, considering the use by various users.