• 한국환경과학회지
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• 제13권11호
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• pp.965-985
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• 2004

The investigation of driving mechanism for the formation of tropical night in the coastal region, defined as persistent high air temperature over than 25$^{\circ}C$ at night was carried out from August 14 through 15, 1995. Convective boundary layer (CBL) of a 1 km depth with big turbulent vertical diffusion coefficients is developed over the ground surface of the inland basin in the west of the mountain and near the top of the mountain, while a depth of thermal internal boundary layer (TIBL) like CBL shrunken by relatively cool sea breeze starting at 100 km off the eastern sea is less than 150 m from the coast along the eastern slope of the mountain. The TIBL extends up to the height of 1500 m parallel to upslope wind combined with valley wind and easterly sea breeze from the sea. As sensible heat flux convergences between the surface and lower atmosphere both at the top of mountain and the inland coast are much greater than on the coastal sea, sensible heat flux should be accumulated inside both the TIBL and the CBL near the mountain top and then, accumulated sensible heat flux under the influence of sea breeze circulation combined with easterly sea breeze from sea to inland and uplifted valley wind from inland to the mountain top returning down toward the eastern coastal sea surface should be transported into the coast, resulting in high air temperatures near the coastal inland. Under nighttime cooling of ground surface after sunset, mountain wind causes the daytime existed westerly wind to be an intensified westerly downslope wind and land breeze further induces it to be strong offshore wind. No sensible heat flux divergence or very small flux divergence occurs in the coast, but the flux divergences are much greater on the top of the mountain and along its eastern slope than on the coastal inland and sea surfaces. Thus, less cooling down of the coastal surface than the mountain surface and sensible heat transfer from warm pool over the coast into the coastal surface produce nocturnal high air temperature on the coastal inland surfaces, which is not much changed from daytime ones, resulting in the persistence of tropical night (nocturnal thermal high) until the early in the morning.

• 한방안이비인후피부과학회지
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• 제26권4호
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• pp.60-69
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• 2013

Objective : This case series study was designed to assess the effect of Gamisungmagalguntang for chronic urticaria identified as "Wind-Heat" pattern by retrospective methods. Methods : We treated 19 patients for chronic urticaria with Gamisungmagalguntang(加味升麻葛根湯), who visited to care chronic urticaria at the department of Ophthalmology, Otolaryngology and Dermatology of Korean Medicine at Kyunghee University Korean Medical Center from 1st January 2013 to 31st August 2013. We analyzed information and body conditions of 19 patients. And by using Urticaria Activicy Score(UAS), frequency and number of wheals, itch severity and total score on a 4-point(0-3) scale were assessed in 19 patients. The change of each criterion and total scores between baseline and follow up were analyzed using paired t-test and Wilcoxon test(p<0.05). Results : 1. UAS improvement was statistically significant(p<0.001). Effects of symptom improvement were excellent(31.58%) that means symptom remission and good(42.10%) that means symptom improved over 50%. 2. Heat sensitivity as suspected provocation factor could be a marker for the Wind-Heat pattern urticaria. 3. Among the Wind-Heat pattern urticaria patients, normal digestion(52.63%) and no thirst(78.95%) were higher than abnormal conditions. Whereas about sweat item, abnormal conditions(57.89%) were higher than normal. That means abnormal sweat conditions could be a marker for a defense qi(衛氣) dysfunction of the Wind-Heat pattern urticaria. Conclusions : Our findings suggest that Gamisungmagalguntang could be effective on the Wind-Heat pattern urticaria.

• 지구물리
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• 제8권3호
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• pp.159-167
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• 2005

Turbulent fluxes of sensible heat and latent heat were analyzed at King Sejong station in the austral summer of 2002 (December) and 2003 (January and February). Monthly mean air temperatures of January and February (2.2oC) were similar to those averaged over 1988 to 2001. Precipitation was less in January and greater in February than those averaged over last 14 years. In December of 2002 and January, there was precipitation primarily when easterly wind blew usually. The frequency of snowfall was equal to or larger than that of rainfall. In the mean while, precipitation primarily in forms of rainfall occurred with westerly wind in February. In addition, while for easterly wind, temperature and humidity was low, temperature and humidity were high in case of westerly wind. Based on flux footprint, measured flux mainly came from within 300 m with maximum of 40 m upwind, indicating the insignificant role of the sea around the study site. Half-hourly downward short wave radiation amounted up to ∼ 1000 Wm-2 and net radiation ranged from -50 to 600 Wm-2. Half-hourly sensible heat flux was positive at daytime with maximum of ∼ 400 Wm-2, except the 27th and 28th in February of 2003 when it was negative all day despite of positive net radiation at short daytime. Latent heat flux was positive with maximum of ∼ 130 Wm-2. Depending on wind direction, the partitioning of net radiation into the sum of sensible heat flux and latent heat flux was larger than 0.8, indicating the strong source of the land surface for the atmospheric heating. The daytime averaged Bowen ratio (=sensible heat flux /latent heat flux) was significantly greater than 1, indicating that sensible heat flux was the main source to heat the atmosphere over the site.

• 한국안전학회지
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• 제16권4호
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• pp.22-28
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• 2001

Heat transfer and pressure distribution for heat exchanger type of domestic gas boiler are different from shape, pitch, thickness of fin and array of pipe respectively. In order to measure the pressure distribution across the heat exchanger, a suction type wind tunnel was constructed and velocity distribution was measured for pilot tube(4 point) of rack type. The experiments were performed for 5 different air flow mass, rpm=3,6,9,12,15 and transverse axis of heat exchanger(x-length) is 5cm respectively. Results showed that above 9.5m/s, pressure distribution dispersion for wet type of heat exchanger is on the increase and above 5.5m/s, pressure distribution dispersion for dry type of heat exchanger is on the increase. Also, pressure distribution dispersion by comparing two different types heat exchanger, dry type of heat exchanger showed a higher augmentation than wet type of heat exchanger.

• 동의생리병리학회지
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• 제26권5호
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• pp.577-587
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• 2012

Warm disease: Any of various heat disease characterizer by rapid onset and shifts, pronounced heat signs, and a tendency to form dryness and damage yin. Exterior heat sign: exterior heat patterns are characterizer by pronounced heat signs, such as a red sore pharynx and a relatively red tongue with dry fur, the pulse is floating and rapid, cough and the production of thick white or yellow phlegm. If wind-heat evil exist in weifen, it becomes exterior syndrome, and a remedy about that is dispelling wind-heat but when wind-heat evil invades in nasal and throat part so the disease occurs, you need to add relieving sore throat worsens invades in lung it makes disharmony of diffuse in lungs. So a remedy about it is diffuse the lung. disharmony of diffuse in lungs makes metabolic disorder of qi and liquid and humor malfunction therefore it occurs cough and heat-phlegm syndrome. heat from weifen invades the whole of lungs and form lung heat. So a remedy about lung heat is clearing away lung heat, this lung heat makes inevitably bleed in lungs, therefore a remedy in this case is clearing the lung to stop bleeding, or moistening the lung. Exterior heat sign means that exterior syndrome coexists with heat syndrome and it means that a remedy of this syndrome need to mix prescriptions for relieving exterior syndrome and heat-clearing prescriptions to treat this syndrome.

• 국제초고층학회논문집
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• 제11권3호
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• pp.145-156
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• 2022

Application examples of computational fluid dynamics (CFD) in the planning stage of high-rise buildings are introduced. First, we introduce examples of applications in the environmental field. The pedestrian wind environment was one of the earliest practical examples of CFD. CFD was also employed to validate the heat island mitigation measures proposed as part of the new construction plan. Second, application examples of wind-force evaluations are introduced. Prediction examples are presented for the peak wind pressure around a complex-shaped building and the wind force evaluation for a base-isolated building. The results prove that the results of the proper execution of CFD are equivalent to those of the wind tunnel experiment. As examples of CFD applications of other issues related to high-rise building planning, we introduce snow accretion on outer walls and high-temperature exhaust from emergency generators. Finally, the future prospects for the use of CFD are discussed.

• 한방안이비인후피부과학회지
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• 제15권1호
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• pp.177-197
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• 2002

The result were achived from 29 kinds of the medical literature of many generation is like this. 1. Oriental medical expressions of Xerophthalmia are "Baksab(白澁)", "Kunsabhonhwa(乾澁昏花)", "Sinsoojanggo(神水將枯)", "Donginkunkyul(瞳人乾缺)", "Taljung(奪精)", etc. "Baksab(白澁)" is very close to Xerophthalmia. 2. The cause of Xerophthalmia is Wind, Wind-heat Pathogen, Damp-heat of spleen and lung, DefIciency of body fluid, Yin-deficiency of liver and kidney, Liver deficiency syndrome, Deficiency of blood, Fire, Fire of deficiency type, Liver heat, etc. 3. In the frequency of prescription used Xerophthalmia are "Sangbakpi-Tang(桑白皮湯)", "Eunkyosan(銀翹散)", etc as Excess type, "Kikookjihwang-Tang(杞菊地黃湯)", "Samooloja hwan(四物五子丸)", etc as Deficiency type. 4. In the frequency of medical herbs of Xerophthalmia use much Rehmannia root nourishing Yin and clearing away heat and Divaricate Saposhnikovia root(expelling pathogenic wind.

• 수산해양기술연구
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• 제31권4호
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• pp.402-412
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• 1995

본 연구의 결과를 요약하면 다음과 같다. (1) 유압 펌프, 유량조절 밸브(오리피스)등을 주된 구성 요소로 하는 구조가 간단하고, 운전.관리가 용이한 유압식 풍력.열 변환 장치를 개발하였다. (2) 실험 결과로부터 본 장치의 에너지 변환 효율이 매우 높음을 확인하였다. (3) 출력 에너지가 열 에너지이므로 온수 탱크를 사용하여 쉽게 에너지를 저장할 수 있음을 실험적으로 확인하였다. (4) 본 장치는 대량 생산되는 유압 부품들만을 사용하여 구성이 가능하므로 매우 저렴한 가격으로, 신뢰성이 우수한 장치를 제작할 수 있다

• 대기
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• 제20권1호
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• pp.13-26
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• 2010

The Urban Canopy Model (UCM) implemented in WRF model is applied to improve urban meteorological forecast for fine-scale (about 1-km horizontal grid spacing) simulations over the city of Seoul. The results of the surface air temperature and wind speed predicted by WRF-UCM model is compared with those of the standard WRF model. The 2-m air temperature and wind speed of the standard WRF are found to be lower than observation, while the nocturnal urban canopy temperature from the WRF-UCM is superior to the surface air temperature from the standard WRF. Although urban canopy temperature (TC) is found to be lower at industrial sites, TC in high-intensity residential areas compares better with surface observation than 2-m temperature. 10-m wind speed is overestimated in urban area, while urban canopy wind (UC) is weaker than observation by the drag effect of the building. The coupled WRF-UCM represents the increase of urban heat from urban effects such as anthropogenic heat and buildings, etc. The study indicates that the WRF-UCM contributes for the improvement of urban weather forecast such nocturnal heat island, especially when an accurate urban information dataset is provided.

• 대한기계학회:학술대회논문집
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• 대한기계학회 2004년도 춘계학술대회
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• pp.1358-1363
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• 2004

The objective of this work is to propose calibration facility in which a thin film type heat flux sensor can be calibrated under convective flow condition by using a small wind tunnel with the constant temperature plate condition. A small wind tunnel has been built to produce a boundary layer shear flow above a constant temperature copper plate. 12-independent copper blocks, thin film heaters, insulators and temperature controllers were used to keep the temperature of flat plate constant at a specified temperature. Three commercial thin film-type heat flux sensors were tested. Convective calibrations of these gages were performed over the available heat flux range of $1.4{\sim}2.5kW/m^2$. The uncertainty in the heat flux measurements in the convective-type heat flux calibration facility was ${\pm}2.07%$. Non-dimensional sensitivity is proposed to compare the sensitivity calibrated by manufacturer and that of experiment conducted in this study.