이 연구에서는 국토해양부 위성항법중앙사무소가 운영하고 있는 17곳 DGNSS 기준국의 신호수신환경을 파악하기 위해 관측자료의 TEQC 프로그램 품질평가, 가시성 분석 및 현장조사를 병행하였다. TEQC 프로그램 수행결과 팔미도, 어청도, 거문도, 평창, 성주, 충주 기준국의 일부 지수가 상대적으로 저조하게 나타났다. 6곳을 제외한 품질평가지수는 평균 98%의 데이터수신율과 0.19m의 L1 의사거리 다중경로 오차, 0.71m의 L2 의사거리 다중경로 오차가 나타났으며, 사이클슬립은 1000회 관측당 평균 1.3회 수준으로 나타나 대부분의 기준국들은 최적의 환경에 놓여 있었다. 그러나 팔미도와 어청도의 경우 데이터수신율이 낮았다. 이는 L2C 신호를 송출하는 위성들의 P2 신호를 기록하지 못하여 수신율을 저하시키는 요인으로 확인되었다. 거문도의 경우 주변 장애물은 존재하지 않았으나 설치된 관측장비 또는 설비문제로 인하여 품질지수가 저하된 것으로 사료된다. 평창은 남쪽에서 북서쪽으로 이어지는 야산이 폭 넓게 위치하고 있어 데이터 수신율이 상대적으로 좋지 않은 기준국으로 확인되었다. 4개의 품질평가지수가 모두 좋지 않은 성주와 충주는 주변 환경이 다른 기준국과 큰 차이는 없었으나, 설치된 관측장비에 의해 신호품질이 저하된 것으로 추정되어 비교실험을 통한 추가 분석이 필요하다.

Mass mortalities of cultivated organisms have occurred frequently in Korean coastal waters causing enormous losses to cultivating industry. The preventive measures require continuous observation of farm environment and real-time provision of data. However, line hanging aquaculture farm are generally located far from monitoring buoys and has limitations on installation of heavy equipments. Substituting battery pack for solar panels and miniaturizing size of buoy, newly developed system can be attached to long line hanging aquaculture farm. This system could deliver measured data to users in real-time and contribute to damage mitigation and prevention from mass mortalities as well as finding their causes. The system was installed off Gijang and Yeongdeck in Korea, measuring and transmitting seawater temperature at the sea surface every 30 minutes. Short term variation of seawater temperature, less than one day, in Gijang from June to July 2009 corresponded tidal period of about 12 hours and long term variation seemed to be caused by cold water southeast coast of Korea, particularly northeast of Gijang. Seawater temperature differences between Gijang station and the other station that is about 500 m away from Gijang station were 1 ℃ on average. This fact indicates that it is need to be pay attention to use substitute data even if it is close to the station. Daily range of seawater temperature, one of crucial information to aquaculture, can be obtained from this system because temperature were measured every 30 minutes. Averages of daily range of temperature off Gijang and Yeongdeok during each observation periods were about 2.9 ℃ and 4.7 ℃ respectively. Dominant period of seawater temperature variation off Yeongdeok was one day with the lowest peak at 5 a.m. and the highest one at 5 p.m. generally, resulting from solar radiation.

근래에 이상기상과 지구 온난화로 인한 해수면 상승과 해사채취, 난개발에 의해 국내외 연안역에 여러 형태의 침식피해가 발생되고 있다. 이에 대한 침식방지 및 보호대책 공법이 적용되고 있으나 큰 실효를 거두지 못하고 있다. 연안보호 구조물로 PC 콘크리트 호안블럭이 국내외 연안에 시공되고 있으나 대부분의 기존 구조물들은 사람의 접근성이 어려운 구조물로 시공되어 있어 친수성이 부족한 실정이다. 본 연구에서는 이런 점들을 보완하여 사람들의 접근성이 좋으면서 연

This study aims to produce fundamental database for Environment Impact Assessment by monitoring vertical structure of the atmosphere due to the mountain valley wind in spring season. For this, we observed surface and upper meteorological elements in Sangin-dong, Daegu using the rawinsonde and automatic weather system(AWS). In Sangin-dong, the weather condition was largely affected by mountains when compared to city center. The air temperature was low during the night time and day break, and similar to that of city center during the day time. Relative humidity also showed similar trend; high during the night time and day break and similar to that of city center during the day time. Solar radiation was higher than the city, and the daily maximum temperature was observed later than the city. The synoptic wind during the measurement period was west wind. But during the day time, the west wind was joined by the prevailing wind to become stronger than the night time. During the night time and daybreak, the impact of mountain wind lowered the overall temperature, showing strong geographical influence. The vertical structure of the atmosphere in Dalbi valley, Sangin-dong had a sharp change in air temperature, relative humidity, potential temperature and equivalent potential temperature when measured at the upper part of the mixing layer height. The mixing depth was formed at maximum 1896m above the ground, and in the night time, the inversion layer was formed by radiational cooling and cold mountain wind.

To verify the accuracy of the numerical experiment of Part I, measurements at the matured rice canopy located around Junam reservoir were performed at August 14, 1995. According to the measured data, the foliage temperature recorded the highest value, and the ground temperature was the lowest around noon, and these results coincided with those of the numerical experiment using the combined model of Part I. From the estimation using measured data, the maximum value of the latent heat flux was 380 Wm2, the highest value among energy balance terms, and the energy redistribution ratio of the latent heat flux was averaged as 0.5, the highest values among redistribution ratios. These results are the same as those of the numerical experiment in tendency, but they reveals a little lower in the absolute values than those from the numerical experiment.