본 연구에서는 극궤도 위성 Aqua/Terra에 탑재된 MODIS 복사계와 정지궤도 위성 GOES-9의 2년간 관측 자료를 이용하여, 한반도 10개 공항 지역에 대한 안개 탐지 가시 경계값 및 적외 경계값을 각각 0.65μm에서의 반사율(R0.65) 그리고 3.7μm와 11μm 밝기온도 간의 차이(T3.7-11)에서 계절별로 유도하였다. 이들 경계값이 두 종류 위성에서 서로 다르게 나타나는 원인을 조사하기 위하여, 수도권 지역에 대한 극궤도 및 정지궤도 위성들의 동시 관측 자료를 이용하여 주야간 청천과 안개 시에 다음 변수들을 비교분석하였다; 3.7μm 밝기온도(T3.7), 11μm 밝기온도(T11), 그리고 T3.7-11. 주간 경우에는 R0.65도 사용되었다. 위 변수들은 공간 분포에서 두 위성 간에 0.5 이상의 유의적인 상관을 보였다. 이 분석에서 두 위성 간에 경계값 차이는 3.7μm 채널 파장대 불일치 뿐만 아니라 공간 분해능 불일치에도 기인하였다. 한편 GOES-9에서 유도된 안개 탐지 경계값은 청주 공항을 제외한 한반도 9개 공항의 안개 및 청천 시에 대한 통계적인 검증에서 주간에 약 60%, 그리고 야간에는 약 70%의 정확도를 보였다. 그러나 정확도는 여명, 안개층 위에 상층운 존재, 강수 동반, 그리고 짧은 지속 시간 하에서 발생하는 안개에 대하여 감소하였다. 안개 탐지에 사용되는 세 채널의 광학적인 특성을 조사하기 위하여, 파장에 따른 복사휘도 및 반사율의 민감도가 수치 실험을 통하여 여러기상 상태 하에서 분석되었다.

An experimental study of the fire protection performance of water mist spray subjected to thermal radiation was presented. Downward-directed water mist sprays to interact with an under. gasoline pool fire were experimentally investigated in underground environment. The mass mean diameters of water mist droplet were measured by PMAS under various flow conditions. The developed water mist spray nozzle was satisfied to the criteria of NFPA 750. The mechanism of the fire extinguishment by water mist spray was concluded to be cooling of the fire surface which lead to suppressed of' file1 evaporation. It was proved that the water mist spray system under. lower pressures could be applied to underground fire protection system.

Fog in Taechon which is located in the west coast of Korea is advection fog made by marine atmosphere which is higher than the temperature of sea water and cooled while moving toward land with wind. Huwevcr. the annual mean number of tog days is 15.1, obviously Icss than those of Susan, Kunsan and similar coastal cities. The number of fog occurrence days in April and May increases twice as many as that of the months from November to March. From August it decreases to half as many as that of the months from April to May and then maintains such an extent. So the phenomenon is different from other areas. 1 he characteristics of fog in Taechon arc due to little difference between sea surface temperature and marine air temperature and geographical characteristics of Taechon area.

수영만을 포함한 부산 지방 안개발생의 특징 및 안개 발생에 대한 부산 연안의 역할을 최근 5개년(1984~1988)의 기상 관측자료 및 지상 일기도, 그리고 해양관측자료를 사용하여 조사하였다. 또한 1989년 7월 한 달 동안 수영만에서 관측한 일기상 자료와 표면 수온을 부산지방의 일기상 자료, 표면수온과 비교하였다. 부산 지방의 안개는 5, 6, 7월에 집중적으로 발생하며, 안개 발생시의 주풍향은 수증기 공급이 용이한 남서풍 및 북동풍이었다. 안개 발생과 관련된 기압계 유형은 봄철(3, 4, 5월)이 pattern 7 (이동성 고기압형), 여름철(6, 7, 8월)이 pattern3(정체전선인 33˚N미만에 위치한 형)과 pattern 10(정체전선이 33~36˚N사이에 위치한 형)이었다. 또한 이류무의 발생은 전층 (850~500mb)에 걸친 대기 불안정도의 증가 보다는 하층 대기 (850~700mb)의 한.온 이류와 해표면의 난.한 수온과의 관계에 더 많은 관련성이 있었다. 내륙 지방인 대구 지방의 안개는 강한 야간 복사 냉각에 의해서 가을철 새벽에 발생하나 해안 지방인 부산은 남풍 계열의 바람이 부는 늦봄에서 여름철(5, 6, 7월)에 다량의 수증기 유입으로 높은 상대습도를 가지게 되어 대기가 약간의 복사 냉각에 의해서도 쉽게 과포화에 이르기 때문에 5, 6, 7월에 집중적으로 발생했다. 수영만과 부산지방의 일기상 자료, 표면 수온 및 안개발생일 등은 거의 비슷하며 안개 발생 mechanism 역시 거의 일치한다고 생각된다.

숙근(宿根)안개초(草)의 조직배양(組織培養)에 있어 배지(培地)에 첨가하는 agar농도(濃度) 및 auxins의 농도(濃度)가 vitrification에 미치는 영향(影響)을 조사(調査)한 결과(結果)는 다음과 같다. 1. 초장(草長), 생체중(生體重), 분지수(分枝數)는 agar농도(濃度)가 높아질수록 감소(減少)되는 경향(傾向)이었으며 auxins의 효과(效果)는 미약(微弱)하였다. 그러나 초장신장(草長伸長)에 있어서 IAA 1.0ppm+NAA 0.5ppm 및 IAA 2.0ppm+NAA 1.0ppm 첨가구에서는 그 결과(結果)가 매우 양호(良好)하였다. 2. 발근소요일수(發根所要日數)에 있어서는 auxins의 첨가효과(效果)가 적었다. 그러나 근(根)의 생육(生育)에 있어서는 IAA 1.0ppm+NAA 0.5ppm 및 IAA 2.0ppm+NAA 1.0ppm 첨가구에 있어서 분화(分化)된 근(根)의 생장(生長)이 매우 양호(良好)한 경향(傾向)이었다. 3. 건전주율(健全株率)에 있어서는 agar농도(濃度)가 높아질수록 증가(增加)하는 경향(傾向)이었으나 배지(培地)가 너무 경화(硬化)되면(1.5%) 지상부(地上部) 및 지하부(地下部)의 생육(生育)이 극(極)히 저조(低調)하였다. 4. 이상(以上)을 종합(綜合)해 보면 숙근(宿根)안개초의 조직배양시(組織培養時) 외부환경(外部環境)에 대(對)한 적응력(適應力)이 높은 강건한 묘(苗)의 육성(育成)을 위해서는 agar농도(濃度) 1.2%로 한 MS배지(培地)(RM1962)에 IAA 1.0ppm+NAA 0.5ppm 첨가배지(培地)를 사용(使用)하는 것이 바람직하다고 생각된다.

The study was aimed to investigate the correlation between tidal effects and fog occurrence in Incheon and Mokpo, which are located in the middle and southern coasts of the West Sea of Korea, respectively. The investigation used meteorological data obtained from the automated synoptic observing systems and automatic weather stations and ocean data from tide stations from 2010 to 2019. Fog occurrence frequency was highest at high tide (Incheon, 41%; Mokpo, 45%). During fog event days at high tide, the dew-point depression was low (Incheon, 0.5 ℃; Mokpo, 0.4 ℃) and the relative humidity was high (Incheon, 97%; Mokpo, 9 8%). The w ind speed w as 2 . 4 m/s in I ncheon a nd 2 .0 m/s in M okpo, a nd t he m ain wind d irections w ere west-southwesterly from Incheon and southwesterly from Mokpo. In the fog case study, tidal flats were covered with water before and after the fog started. During the fog period, both stations experienced negative air-sea temperature differences, low dew-point depression, and high relative humidity were maintained, with weak winds forming from the tidal flats to the shore.

Fog can have severe impacts on human life (e.g., accidents in transportation systems) because it causes low visibility. Areas prone to fog near the sea or a river require accurate fog forecasts. In this study, we analyzed the characteristics of fog occurrence around Gumi Reservoir, a part of the inland Nakdong River. We also simulated and predicted visibility using the Weather Research and Forecasting (WRF) model. Visibility was estimated using several point measurements and several different methods: Stoelinga and Warner (SW99), Rapid Update Cycle (RUC), the Forecast System Laboratory (FSL), Decision Tree (DT), revised visibility (RVIS) and Gultepe_06 methods. The DT method showed a pattern similar to the observed fog occurrences. In this study, the Gulteppe_06 method produced the best performance under the lowest visibility situation, although there is some discrepancy in microphysics' simulated results, followed by DT and RUC.

The detailed characteristics of fog over South Korea were analyzed using the three-years quality controlled (QC) 237 visibility meter data operated by Korea Meteorological Administration. The fog (dense fog: DFog) frequency varies greatly with season and geographic location. The fog frequency at inland is highest in autumn, but at the West Coast in spring and summer. Fog occurs frequently from spring to autumn in the mountainous regions. Unlike the fog, the DFog is mostly prevalent in summer at land, mountain, and coastal regions. The large coefficients of variation of fog and DFog at the three regions and four seasons indicate that the locality of fog over South Korea is very high. The formation and dissipation (FaD) of fog show strong diurnal variations irrespective of geographic location and season, strongest at inland and weakest at sea. Fog usually occurs from night to sunrise and dissipates from early morning to late morning. The maximum FaD time of fog show seasonal variation with the seasonal change in solar elevation angle. The frequency of fog is inversely proportional to the duration time, mostly less than 3 hours regardless of season and geographic location. Also, the duration of DFog is mostly within 1-3 hours.

Fog may have a significant impact on road conditions. In an attempt to improve fog predictability in Jeju, we conducted machine learning with various data mining techniques such as tree models, conditional inference tree, random forest, multinomial logistic regression, neural network and support vector machine. To validate machine learning models, the results from the simulation was compared with the fog data observed over Jeju(184 ASOS site) and Gosan(185 ASOS site). Predictive rates proposed by six data mining methods are all above 92% at two regions. Additionally, we validated the performance of machine learning models with WRF (weather research and forecasting) model meteorological outputs. We found that it is still not good enough for operational fog forecast. According to the model assesment by metrics from confusion matrix, it can be seen that the fog prediction using neural network is the most effective method.

We analyzed the micro-meteorological characteristics during typical steam fog over the Gumi Reservoir of Nakdong river with the field observation data for recent 2 year(1 April 2013~31 March 2015) collected by the national institute of meteorological research, KMA. Steam fog occur when the cold drainage flows over the warm water surface. As the sensible and latent heat from water are provided to the air, the instability of lower atmosphere is increased. The resultant vertical mixing of warm, moist air near water surface and cold air aloft causes the formation of status cloud. The convection strengthened by radiative cooling of the upper part of the stratus causes the fog to propagate downward. Also, the temperature at the lowest atmosphere is increased rapidly and the inversion near surface disappear by these processes when the fog forms. The increase of wind speed is observed because the downward transportation of momentum is caused by vertical mixing.

We analyzed the characteristics of fog formation in the Gumi Reservoir of Nakdong river with the field observation data for recent 2 years (1 April 2013~31 March 2015) collected by the national institute of meteorological research, KMA. In early morning, we frequently observe the steam rising from the water surface. The fog occurs from adding water vapor into the air. We call the fog as steam fog. Steam fogs occur when cold, dry air mixes with warm, moist air above a water surface. The steam fog appears mainly in autumn under the following conditions; (1) sensible heat is positive values (10~20 W/m2), (2) latent heat is more positive values (25~35 W/m2) than sensible heat, (3) cloudless nights with light winds (about 1.5 m/s), (4) under condition(3), mountainous winds easily blows into the reservoir.

석조문화재의 산성안개에 의한 손상을 예측하기 위하여 경주남산화강암, 응회암과 대리암에 pH4.0과 pH5.6의 인공안개를 적용하였다. 풍화된 경주남산화강암은 신선한 암에 비해 산성안개에 의한 무게감소가 더 크다. 응회암은 산성안개시험 매 회당 약 0.005 %의 무게감소율로 시험 대상 암석 중 가장 크게 변하였다. 응회암과 풍화된 화강암은 산성안개 보다는 산성비에 의한 무게감소가 더 크게 발생할 것이며, 대리암은 산성강우의 상태와 상관없이 무게감소가 나타날 것으로 예측되었다. 산성안개와 반응한 후 풍화암의 공극률과 흡수율이 월등히 증가한 결과를 보여, 풍화암이 신선한 암보다 산성안개에 취약할 것으로 예상된다. 대리암의 흡수율은 시험 후 약 50% 증가하였다. 암석의 색상이 시험 후 황색 쪽으로 약간 변화되었으며, 신선한 암보다는 풍화된 화강암에서 그 경향이 더 크다. 대리암은 산성안개와 반응 후 백색도가 증가하였다. 산성안개가 적용된 암석에서 검출되는 다량의 양이온은 반응에 의해 분해된 구성광물에서 기인한다.

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.

This study aimed to investigate the change of fog frequency and duration hours hours in South Korea. Using daily mean fog days(about 50 years) and fog duration hours(about 46 years) during the period of 1961~2010 for long-term observational data of 14 weather stations in South Korea, the change of temperature rise was analyzed. The change of fog days had a decreasing trend for the period of 1961~2010. There was a distinctly decreasing trend in Seoul and South-Eastern Coast area. The seasonal decreasing trend of fog days and fog duration hours was similar in spring and summer. On the other hand the change of Chupungnyeong in autumn and the West Coast in summer had a increasing trend. The change of fog duration hours was rarely changed. It was affected by the change of fog days. In addition, the change of fog days and fog duration hours of South-Eastern Coast area in autumn and winter had to decreasing trend. Otherwise the change of Jeonju in spring and Mokpo in summer had a increasing trend. There was a negative correlation between temperature element and fog days, and fog duration hours. But the change of fog days and fog duration hours was not decreasing trend in all areas. The decreasing trend of fog days was affected by temperature rise. However, there was not shown significant result of fog duration hours.

수치일기예보와 관측 시스템의 많은 발전에도 불구하고 안개 예측은 아직도 만족할 수준이 아니다. 본 연구에서는 기상청의 지상 안개 관측자료(1998~2007)를 이용하여 충청지방의 안개 발생 특성과 안개 발생에 영향을 주는 기상요소들에 대해 조사하였다. 또한 로지스틱 기법을 이용하여 계절별 안개예측 식을 개발하고 이를 검증하였다. 충청지역에서 연 평균 안개 발생일 수는 충주에서 56.5일, 추풍령에서 17.9일이 발생하는 등 강한 공간편차를 보이고 있다. 또한 대부분 지역에서 가을과 여름에 각각 최대와 최소로 발생하여 계절변동도 강하게 나타나고 있다. 안개의 발생은 주로 04~07시에 일어나고 지속시간은 약 3시간 반 정도이다. 다른 지역과 달리 서산에서는 바람이 강할 때도 안개가 발생하고 있어 이 지역에서는 이류무도 자주 발생함을 알 수 있다. 또한 강수발생 유무도 안개 발생에 많은 영향을 미침이 확인되었다. 로지스틱 안개예측 기법의 예측 수준을 2008년도 지상 관측자료를 이용하여 검증한 결과 현재 기상청의 예보 수준보다 향상된 예보 수준을 보였다.

In this study, meteorological characteristics concerning the occurrence of fog are analyzed using 4-years (2000-2003) data at Chuncheon. From the analysis of meteorological characteristics, the fog at Chuncheon occurred before sunrise time and disappeared after that time and lasted for 2-4 hours. When fog occurred, on the whole, wind direction was blew the northerly and wind speed was below 2.1 m/s. Especially, about 42 % of foggy day fell on the calm(0～0.2 m/s) conditions. The difference between air temperature and dew point temperature near the surface were mainly less than 2 ℃. For the lack of water surface temperature, the water surface temperature was calculated by using Water Quality River Reservoir System (WQRRS). In Chuncheon, there is close correlation between the frequency of fog day and outflow from Soyang reservoir and high frequency of occurrence due to the difference between air and cold outlet water temperature.

In this study, characteristics of fog at Mokpo as the west coastal area of Jeonnam were investigated, using statistical analysis of observed fog and meteorological data. Higher frequency of the fog occurrence at Mokpo was showed in spring(32%) and summer(34%) due to the seasonal high atmospheric pressure. Regional characteristics as radiation cooling, advection of fog and water vapor from surrounding sea and Yeongsan lake, and frontal fog had major effect on the coastal fog at Mokpo on the meteorological conditions of north-west/south wind and calm(0～2m/s). Also, as the results of analyzing data of before and after the construction of Yeongsan dam, the frequency of annual mean fog days increased 41%, specially increased 178% in autumn. The increase of fog days mainly resulted from evaporation during colder seasons and from temperature inversion during warmer seasons over the water surface of Yeongsan lake. The construction of Yeongsan dam had a little effect on the meteorological conditions concerning fog occurrence, because Yeongsan dam which only supplies the water for use do not always carry out outlet of the cold water. In addition, the sea fog at Heuksando located in offshore had not effect on the occurrence of fog at Mokpo.

하계 한국 남서연안 해역에는 저온수가 나타나고 안개가 자주 형성되는 것으로 알려져 있다. 본 연구에서는 저온수의 출현시기 및 장소와 이 해역에서 형성되는 안개에 미치는 저온수의 영향에 대해 조사·분석하였다. 그 결과, 저수온역은 초여름 대흑산도 부근해역에서 나타나기 시작하여, 이것은 점차 이동하여 7월 말~8월 초 진도 남서쪽 해역에 위치하고, 그 후 10월 중순경 이 해역에서 소멸된다. 그리고 이 해역에서는 주로 4~8월에 안개가 발생하는데, 특히 인근해역에 비해 해면온도가 현저하게 낮은 진도해역에서 안개 발생빈도가 높은 것으로 보아, 이 해역에 나타나는 저온수가 안개의 형성에 상당한 영향을 끼치는 것으로 사료된다.