• 생태와환경
• /
• 제40권2호
• /
• pp.234-243
• /
• 2007

청계천 복원이후 하천수질의 생태학적 평가를 하기 위하여 청계천을 비롯한 인접수역 중랑천 및 한강 본류를 대상으로 강우 전후 조류 및 수질변화와 현장수에 대한 조류성장잠재력(AGP)을 조사하였다. 조사는 청계천(정점 1, 2), 중량천(정점 3), 두 하천의 합류부(정점 4), 한강 본류의 상류(정점 5)및 하류(정점 6)등 총 6개 정점을 선정하여 2006년 하계(강우 이 전 7월 25일, 강우 이 후 8월 28일)에 각각 1회씩 실시하였다. 한편, AGP조사를 위해 각 정점에서 채수한 현장수를 공시종 남조 Microcystis aeruginosa 배양계에 1/6, 2/6, 3/6씩 각각 첨가하고, 온도 $25^{\circ}C$, 광조건 100 ${\mu}mol$ photons $m^{-2}s^{-1}$ (14h : 10h LD cycle)에서 11일간 배양하였다. 조사결과, 총질소는 중랑천과 청계천의 합류부에서 높았는데, 특히 후자는 강우 전후 각각 14.4, 18.5 mg $L^{-1}$를 기록하며 가장 높았다. 총인 역시 중랑천과 청계천의 합류부에서 높았는데, 총질소의 경우와 같이 정점 4의 총인은 강우 전후 각각 1.1, 1.3 mg $L^{-1}$를 기록하며 가장 높았다. 엽록소-${\alpha}$는 강우 후에는 중랑하수처리장 방류지점을 포함하고 있는 청계천과 중랑천의 합류부인 정점 4에서 매우 높았으며 가장 우점한 조류는 Cyclotella sp.로 조사되었다. 현장수에 대한 AGP조사결과, 강우 전에는 대조구에 비해 모든 정점에서 높은 성장을 보였으나, 강우 후에는 대조구에 비해 전반적으로 낮은 성장을 나타냈다. 다만, 강우 후에는 현장수 첨가량이 증가함에 따라 대조구와 큰 차이를 보이지 않았는데 이는 강우에 의한 영양물질의 증가가 원인인 것으로 판단되었다. 따라서 청계천을 포함한 조사하천들은 평상시에는 비교적 안정된 생태계를 유지하고 있으나 집중강우시 영양물질 유입으로 인한 하류의 조류번식 가능성이 우려되며, 특히 중량천의 수질개선이 시급한 것으로 판단되었다.

• 한국방재학회:학술대회논문집
• /
• 한국방재학회 2007년도 정기총회 및 학술발표대회
• /
• pp.487-491
• /
• 2007

Recently, rainfall induced hazard has been increased gradually, for example, typhoon Rusa in 2002 and Maemi in 2003. In addition, localized heavy rainfall has been also caused tremendous damage to railroad systems. Measured data from the Meteorological Adminstration sometimes, However, are not in accordance with those of rain gauges in local area, because of its good distance. This study develop automatic alarming software to estimate and prevent these kind of rainfall induced hazards in railroad system with online transportation.

• 한국대기환경학회:학술대회논문집
• /
• 한국대기환경학회 2003년도 춘계학술대회 논문집
• /
• pp.241-242
• /
• 2003

울산지역은 1962년 공업 특구로 지정된 후 지난 30년 동안 우리나라의 기간 산업인 석유화학, 제련, 자동차, 조선공업 등 대단히 크고 많은 생산시설이 입주하여 운영 중에 있다. 특히 1974년부터 가동된 온산 국가공업단지에 많은 비철금속관련 업체들이 들어서면서 해양, 토양 뿐 아니라 대기중의 중금속 오염도를 가속 시켜 왔다. 최근 환경부 대기중의 중금속 측정망 분석 결과에 따르면 울산은 국내 여러 공단 도시에 비해 중금속의 오염정도가 매우 심각한 것으로 나타나고 있다. 특히, 온산공단의 대기나 토양의 카드뮴의 오염은 국내 최고치를 나타내고 있다. (중략)

• 대한전기학회:학술대회논문집
• /
• 대한전기학회 2004년도 추계학술대회 논문집 전기기기 및 에너지변환시스템부문
• /
• pp.240-241
• /
• 2004

JP Nagoya. Inc started special work(passenger order} to transmit information to the passenger from 2001 following the eastern area' heavy rain in 2000. They introduced 'Passenger Information System' which uses self communication network(LAN, PHS) mainly and wire/wireless and internet jointly. As an information transmission method of this system, there is "train information transmission using PHS" which transmits info to LED display in special train. This system configured by adding new equipments and using existing equipments, network in maximum, this study reviewed the system, which transmits real time operation condition unified by these passenger order to passenger in high quality, more promptly.

• 동굴
• /
• 제7호
• /
• pp.37-39
• /
• 1998

The Bullock Creek Caves are located adjacent to the usually dry river bed of Bullock Creek, which reaches the sea about a kilometer north of Punakaiki. The caves have been comprehensively written up by Rodgers(l972). Under conditions of normal water flow Bullock Creek submerges where the stream meets limestone on the west side of thier Punakaiki syncline. In flood conditions it overflows the first submergence and progressively floods a series of smaller submergences down valley until it comes to the caves shown on the map. All these with the exception of Wazpretti Cave and Dry Valley Cave are probably more or less flooded during and after heavy rain.(omitted)

• Journal of Electrical Engineering and information Science
• /
• 제2권6호
• /
• pp.116-122
• /
• 1997

The audible noise produced by corona discharge in high voltage transmission lines is the most important line design consideration. In this paper, more accurate and useful formulas for predicting the A-weighted audible noise during heavy and light rain in alternative current (AC) transmission lines are proposed through comparison with the existing formulas. The proposed formulas are developed by the applications of evolutionary computations (ECs) to audible noise data base from long-term measurement.

• 한국방재학회:학술대회논문집
• /
• 한국방재학회 2008년도 정기총회 및 학술발표대회
• /
• pp.719-722
• /
• 2008

Forest management is done to keep ecological health of forest and to enhancement of its function. Nowadays, the abnormal climate and heavy rain happen frequently. Therefore, there are opinions that the thinning slash allowed in the mountain is flowed in rivers, which can influence in flood damage. This study, we grasp moving characteristics of thinning slash through field survey and achieved basic study about the effect of thinning slash on the discharge capacity of rivers and stream structure.

• 동굴
• /
• 제8호
• /
• pp.19-42
• /
• 1998

The Bullock Creek Caves are located adjacent to the usually dry river bed of Bullock Creek, which reaches the sea about a kilometer north of Punakaiki. The caves have been comprehensively written up by Rodgers(972). Under conditions of normal water flow Bullock Creek submerges where the stream meets limestone on the west side of their Punakaiki syncline. In flood conditions it overflows the first submergence and progressively floods a series of smaller submergences down valley until it comes to the caves shown on the map. All these with the exception of Wazpretti Cave and Dry Valley Cave are probably more or less flooded during and after heavy rain.(omitted)

• 한국환경과학회지
• /
• 제21권12호
• /
• pp.1511-1521
• /
• 2012

An attempt is made to analyse characteristic features of heavy rainfalls which occur at the metropolitan area of the Korean peninsular the on- and off- Changma season. For this, two representative heavy rainfall episodes are selected; one is the on-Changma season wherein a torrential rain episode happened at Goyang city on 12 July 2006, and the other is the off-Changma season, a heavy rainfall event in Seoul on 21 September 2006. Both recorded considerable amounts of precipitation, over 250mm in a half-day, which greatly exceeded the amount expected by numerical prediction models at those times, and caused great damage to property and life in the affected area. Similarities in the characteristics of both episodes were shown by; the location of upper-level jet streak and divergence fields of the upper wind over heavy rainfall areas, significantly high equivalent potential temperatures in the low atmospheric layer due to the entrainment of hot and humid air by the low-level jet, and the existence of very dry air and cold air pool in the middle layer of the atmosphere at the peak time of the rainfall events. Among them, differences in dynamic features of the low-level jet and the position of rainfall area along the low-level jet are remarkable.

• International Union of Geodesy and Geophysics Korean Journal of Geophysical Research
• /
• 제26권1호
• /
• pp.15-29
• /
• 1998

The numerical simulation of heavy precipitation event occurred in the central Korean Peninsula on July 26-28, 1996 was performed using the fine mesh model. ARPS (Advanced Regional Prediction System) developed by the CAPS (Center for Analysis and Prediction of Storms). Usually, the heavy rainfalls occurred at late July in the Korean Peninsula were difficult to predict, and showed very strong rainfall intensity. As results, they caused a great loss of life and property. As it usual, this case was unsuccessful to predict the location of rain band and the precipitation intensity with the coarse-mesh model. The same case was, however, simulated well with fine-mesh storm-scale model, ARPS. Moisture band at 850 hPa appeared along the Changma Front in the area of China through central Korea passed Yellow Sea. Also the low-level jet at 700 hPa existed in the Yellow Sea through central Korea and they together offered favorable condition to induce heavy rainfall in that area. The convective activities developed to a meso-scale convective system were observed at near the Yangtze River and moved to the central Korean Peninsula. Furthermore, the intrusion of warm and moist air, origninated from typhoon, into the Asia Continent might result in heavy rainfall formation through redistribution of moisture and heat. In the vertical circulation, the heavy rainfall was formed between the upper- and low-level jets, especially, the entrance region of the upper-level jet above the exit the region of the low-level jet. The low level convergence, the upper level divergence and the strong vertical wind were organized to the very north of the low level jet and concentrated on tens to hundreds km horizontal distance. These result represent the upper- and low-level jets are one of the most important reasons on the formation of heavy precipitation.