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낙동강 유역 안개 발생시 기상 특성: 강정고령보 사례를 중심으로
박준상 ( Jun Sang Park ),임윤규 ( Yun Kyu Lim ),김규랑 ( Kyu Rang Kim ),조창범 ( Chang Bum Cho ),장준영 ( Jun Yeong Jang ),강미선 ( Misun Kang ),김백조 ( Baek Jo Kim ) 한국환경과학회 2015 한국환경과학회지 Vol.24 No.5
Visibility and Automatic Weather System(AWS) data near Nakdong river were analyzed to characterize fog formation during 2012-2013. The temperature was lower than its nearby city ? Daegu, whereas the humidity was higher than the city. 157 fog events were observed in total during the 2 year period. About 65% of the events occurred in fall (September, October, and November) followed by winter, summer, and spring. 94 early morning fog events of longer than 30 minutes occurred when south westerly wind speed was lower than 2 m/s. During these events, the water temperature was highest followed by soil surface and air temperatures due to the advection of cold and humid air from nearby hill. The observed fog events were categorized using a fog-type classification algorithm, which used surface cooling, wind speed threshold, rate of change of air temperature and dew point temperature. As a result, frontal fog observed 6 times, radiation 4, advection 13, and evaporation 66. The evaporation fog in the study area lasted longer than other reports. It is due to the interactions of cold air drainage flow and warm surface in addition to the evaporation from the water surface. In particular, more than 60% of the evaporation fog events were accompanied with cold air flows over the wet and warm surface. Therefore, it is needed for the identification of the inland fog mechanism to evaluate the impacts of nearby topography and land cover as well as water body.
이영순,조재진,강경선,김배환,남기환,서광원,강성근,임윤규,허강준,Lee, Yong-soon,Cho, Jae-jin,Kang, Kyung-sun,Kim, Bae-hwan,Nam, Ki-hoan,Seo, Kwang-won,Kang, Seong-keun,Lim, Yun-kyu,Heo, Kang-jun 대한수의학회 1994 大韓獸醫學會誌 Vol.34 No.3
This study was performed for assessing carcinogenicity of Folpet using medium-term carcinogenicity bioassay. Sprague-Dawley rats aged six weeks divided into four grout's and were initially given an intraperitoneal injection of diethylnirosamine at 200mg/kg body weight. Two weeks later, group 1(negative control) was treated with basal diet. A Folpet was given per oral administration to group 2(100 ppm) and goup 3(1,000 ppm). Group 4 was fed on water containing 0.05% phenobarbital sodium as a promtor for six weeks. At three weeks after beginning of the experiment, partial hepatectomy was performed in all rats. The tumor-promoting effects were examined by the numbers and areas per $cm^2$ of induced glutathion S-tranferase placetal form(GST-P) positive foci in liver, and silver stained nucleolar organizer regions(AgNORs) which have recently introduced as one of the indicators for the cell proliferative activity. As the results, Folpet didn't have tumor-promoting effects on GST-P positive foci developement and AgNORs during promoting stage after initiation, whereas phenobarbital sodium treatment group showed promoting effect. It was concluded that Folpet didn't have promoting effect at 500, 1,000 ppm using this midium-term carcinogenicity bioassay model.
서울지역 연직 오존 분포 : 2003년 6월 6~9일 오존존데 관측
황미경(Mi-Kyoung Hwang),김유근(Yoo-Keun Kim),오인보(In-Bo Oh),송상근(Sang-Keun Song),임윤규(Yun-Kyu Lim) 한국대기환경학회 2008 한국대기환경학회지 Vol.24 No.2
오존 농도와 기상 인자의 연직관측을 수행하여 오존분포와 하부 대기구조와의 관계를 분석하였다. 관측은 서울 방이동에서 2003년 6월 6~9일에 하루 2회씩(주ㆍ야간) 총 8회에 걸쳐 이루어졌으며, 고도 5㎞ 이내의 관측결과를 중심으로 대기경계층 일변화와 연직 오존농도 변화를 집중분석하였다. 관측 결과, 대기경계층 내 야간안정층 및 혼합층 발달에 따라 큰 오존농도 분포변화를 확인할 수 있었다. 야간에는 안정층 내에서 NO<SUB>x</SUB> 적정반응으로 0에 가까운 낮은 오존농도를 나타내었다. 한편 오후에는 혼합층 내에서 비교적 일정한 오존농도 분포를 나타내며, 대기경계층 상부에서 100 ppb 이상의 최고 농도가 관측되었다. 특히 지표부근 오존농도가 높았던 6월 8일의 관측결과를 통해, 오존의 생성ㆍ소멸과 관련한 국지효과뿐만 아니라 제한된 혼합층 발달이 고농도오존 발생에 중요한 영향을 미침을 확인할 수 있었다. 또한 관측 기간 중, 국지규모 이상의 수송효과에 의한 대기경계층 상부의 농도 상승과 종관기류 변화에 따른 수송 효과가 간접적으로 확인되었다. 연직 오존분포 분석에 있어 충분치 않은 관측 자료로 인해 정확한 시간적 변동을 고찰할 수 없는 한계를 보였다. 하지만 본 연구를 통해 서울지역 대기 하층의 오존 분포 변화와 기상학적 특징을 살펴봄으로서 고농도오존 현상의 역학적인 이해를 도울 것으로 생각되며, 관측 결과는 도시 오존제어를 위한 광화학 수치모델링의 기초 자료로 활용될 수 있을 것이다. Variability in vertical ozone and meteorological profiles was measured by 2Z electrochemical concentration cells (ECC) ozonesonde at Bangyi in Seoul (37.52˚N, 127.13˚E) during June 6~9, 2003 in oder to identify the vertical distribution of ozone and its relationship with the lower-atmospheric structure resulted in the high ozone concentrations near the surface. The eight profiles obtained in the early morning and the late afternoon during the study period clearly showed that the substantial change of ozone concentrations in lower atmosphere (~5 ㎞), indicating that it is tightly coupled to the variation of the planetary boundary layer (PBL) structure as well as the background synoptic flow. All profiles observed early in the morning showed very low ozone concentrations near the surface with strong vertical gradients in the nocturnal stable boundary layer due to the photochemical ozone loss caused by surface NO titration under very weak vertical mixing. On the other hand, relatively uniform ozone profiles in the developed mixing layer and the ozone peaks in the upper PBL, were observed in the late afternoon. It was noted that a significant increase in ozone concentrations in the lower atmosphere occurred with the corresponding decrease of the mixing height in the late afternoon on June 8. Ozone in upper layer did not vertically vary much compared to that in PBL but changed significantly on June 6 that was closely associated with the variation of synoptic flows. Interestingly, heavily polluted ozone layers aloft (a maximum value of 115 ppb around 2 ㎞) were formed early in the morning on 6 through 7 June under dominant westerly synoptic flows. This indicates the effects of the transport of pollutants on regional scale and consequently can give a rise to increase the surface ozone concentration by downward mixing processes enhanced in the afternoon.