Quantification of incoming-salt in the air is absolutely critical for the use of the boundary conditions in chloride resistance design. Thus, as a result of collecting incoming-salt by using multidirectional incoming-salt collector, it was confirmed that incoming-salt was collected not only in the direction of viewing the coast but also in the opposite direction. For this, it is believed that it is necessary to analyze the relationship between the effective defense incoming-salt and the non-effective defense incoming-salt that is delivered through a local flow of surrounding wind

본 연구에서는 하천 범람에 따른 도시지역 내 홍수흐름의 특성을 수치적으로 모의하고 이에 대한 결과를 분석하였다. 적용된 수치모형은 well-balanced HLLC 기법에 근간을 둔 2차원 유한체적모형이다. 대상영역은 경상남도 거제시에 위치한 고현천 주변의 도시지역으로 2003년 9월에 발생한 태풍 “매미” 기간 동안 집중호우로 인해 하천이 범람되어 피해가 발생되었다. 본 연구에서는 도시지역 내 범람에 대한 홍수흔적 자료를 이용하여 수치모형을 검증하였으며, 향후 발생 가능한 집중호우의 강도의 증가 또는 감소에 의한 유입량의 변화에 따른 도시지역 내에서의 홍수흐름의 특성에 대한 모의 및 분석을 수행하였다.

This study was carried out to determine the characteristics of the marine environment, including nutritional content, in order to clearly understand the outbreaks of Gonyaulax polygramma in the southern coastal areas in August, 2009. Samples were collected at 13 sites and water temperature and salinity were measured using a CTD. Field surveys were twice: the first between August 5-7, the second between August 22-24. The cell density of G. polygramma was 6,500-10,000 cells ml-1 during the 1st survey, whereas during the 2nd survey the range of the cells was recorded from 8,000 to 12,500 cells ml-1. Cochlodinium polykrikoides ranged from 0 to 105 cells l-1 during the field survey. In water environments, the majority stations during the 1st survey showed a nearly homogeneous water column below 1℃ in temperature, as well as similar profiles of salinity. However, the stratification between the surface and bottom was observed in the 2nd survey. Regarding nutrients, Dissolved Inorganic Nitrogen (DIN) in the surface ranged from 0.144 to 0.236 mg l-1 during the 1st survey, and 0.082-0.228 mg l-1 during the 2nd survey. DIP (Dissolved Inorganic Phosphorus) did not show any difference in concentration between the 1st and 2nd survey. During August of 2009, the wind speed in the southern waters remained at around ≤2 m s-1 for about 60% of time, and there was very little precipitation during the month. Irradiance of ≥10 hr was shown in the late of August. It is thought that a low level of DIN and salinity play an important role as an essential factor for rapid growth, wide distribution and longer duration of red tide in G. polygramma.

본 연구에서는 2차원 수치모형을 이용하여 폭풍해일고에 따른 해안도시지역 내에서의 범람모의 및 분석을 수행하였으며, 적용된 대상지역은 2003년 태풍 "매미" 내습 시 가장 피해가 컸던 지역인 경남 창원시 마산 합포구 신도시 지역 일부이다. 적용된 수치모형의 검증차원에서 태풍 "매미" 발생기간 동안 관측된 폭풍해일고 자료와 대상지역 내의 주요 지점에 대한 침수흔적 자료를 이용하여 비교 분석을 수행하였다. 또한 향후 발생 가능한 수퍼 태풍에 의한 영향을 분

The effects of high-resolution wind profiler (HWP) data on the wind distributions were evaluated in two different coastal areas during the study period (23-26 August, 2007), indicating weak-gradient flows. The analysis was performed using the Weather Research and Forecasting (WRF) model coupled with a three-dimensional variational (3DVAR) data assimilation system. For the comparison purpose, two coastal regions were selected as: a southwestern coastal (SWC) region characterized by a complex shoreline and a eastern coastal (EC) region surrounding a simple coastline and high mountains. The influence of data assimilation using the HWP data on the wind distributions in the SWC region was moderately higher than that of the EC region. In comparison between the wind speed and direction in the two coastal areas, the application of the HWP data contributed to improvement of the wind direction distribution in the SWC region and the wind strength in the EC region, respectively. This study suggests that the application of the HWP data exerts a large impact on the change in wind distributions over the sea and thus can contribute to the solution to lack of satellite and buoy data with their observational uncertainty.

대수층 바닥이 해수면보다 낮은 해안 지역에서는 관정에서의 적정양수량이 해수침투 여부에 의하여 결정될 수 있다. 이러한 지역에서 관정의 적정 양수량을 초과하는 수요를 만족시키기 위하여 과잉양수를 시행해야하면 우기의 잉여 지표수를 대수층에 주입함으로서 과잉 양수정을 연중 보호할 수 있다. 본 연구에서는 최소의 주입으로 과잉 양수정을 보호할 수 있는 주입정의 위치와 우기의 주입량을 계산하는 전산모델을 개발하였다. 경계면모델과 최적화방법을 조합하여 개발된 수치

본 연구는 해양건축물 또는 워터프런트 개발계획에 있어 특히 워터프런트에 입지하는 주거단지 계획에 역점을 투어 사용자의 측면에서 기존 워터프런트 주거단지의 거주환경 만족도를 조사, 분석 하였다. 또한 통일 주거단지 내에서도 각층별, 방위별, 위치별 쾌적성에 대해 분석하여 가장 선호하는 층, 방위 위치 통에 관한 근거를 제시하고자 하였다. 본 연구의 결론은 다음과 같다. 1) 만족도의 순서는 남향, 남동향, 동향, 남서향의 순으로 나타났으며 남향, 남동향의 선호 경향이 절대적으로 우세한 것으로 나타났다. 2) 전체 응답자의 67%이상이 향보다는 외부로의 조망이 좋아야 한다고 응답하여 워터프런트 주거단지에 있어서는 조망에 대한 중요성이 매우 크다는 사실을 알 수 있었다. 3) 경관 선호도를 분석한 결과는 안벽형 워터프런트, 호안형 워터프런트 덴 하천형 워터프런트의 세가지 Type의 경관별로 약간의 차이는 있었으나 공통적으로 고층부 경관이 가장 높은 선호도를 보였으며 저층부 경관이 상대적으로 가장 낮은 선호도를 보여주었다.

Long-term trends and distribution patterns of water quality were investigated in the Asan coastal areas of Yellow Sea, Korea from 1975 to 2005. Water samples were collected at 3 stations and physicochemical parameters were analyzed including water temperature, salinity, suspended solids (SS), chemical oxygen demand (COD), dissolved oxygen (DO) and nutrients. Spatial distribution patterns were not clear among stations but the seasonal variations were distinct except COD, SS and nitrate. The trend analysis by principal component analysis (PCA) during twenty years revealed the significant variations in water quality in the study area. Annual water qualities were clearly discriminated into 4 clusters by PCA; year cluster 1988-1991, 1994-1997, and 1992-1993/1998- 2005. By this multi-variate analysis we can summarize the annual trends as the followings; salinity, suspended solids and dissolved oxygen tended to increase from late 1980's, increased pH and COD from 1992, and decreased salinity and increased nitrogen and COD from 1990 due to the runoff frow agricultural lands causing eutrophication.

In Korean coastal areas, land reclamations are main development projects that should be based on environmental impact assessment(EIA), because those human interventions can change coastlines, damage tidal flats, and pollute adjacent areas to threat seafood safety and devaluate overall ecosystem service value. Existing procedures of the EIA for land reclamation projects were diagnosed and evaluated to enhance them. Problems were identified in the designation of survey areas, the consistency in survey sites and periods, the standardization of survey methods and reports, the confidence of survey results and the verification of predictions. Lack of integration was noticeable and could be improved by synthesizing different assessments from topography․geography, marine physics, marine chemistry and marine biology. We suggest that successful precautionary marine environment management requires readjusting the cost of EIA, recruiting experts in marine environment, constructing database and establishing specialized assessment system.

We report the distributions of Sb and As in the surface sediment of the Yellow Sea and the coastal areas of Korea. The mean concentrations of Sb and As range from 0.68 ppm to 1.01 ppm and from 7.4 ppm to 15.8 ppm, respectively, and show relatively the high concentrations at the coast of Weolseong in the East Sea for Sb and at the coast of Gadeok Island in the South Sea for As. This may be due to the anthropogenic input of these elements via river and atmosphere from industry complex and agriculture regions around the study areas. Because of the difference of clay to silt proportion, the correlation between silt plus clay contents and Sb, As in the coastal surface sediment of Korea is not shown, the concentrations of Sb and As vary widely for the sample in which the silt plus clay contents are the same. Therefore, we suggest that the distribution patterns of Sb and As in surface sediment of the Yellow Sea and the coastal areas of Korea are mainly controlled by the anthropogenic inputs and the sediment characteristics. On the other hand, the Sb concentrations are lower than those of the lowest effect level which is the standard of judgment for contamination, while the As concentrations are higher than those of the lowest effect level. This implies that the surface sediments of the Yellow Sea and the coastal areas of Korea are considerably contaminated for As.

In an attempt to evaluate the possibility of producing an organic fertilizer using sediments from coastal farming areas, the chemical composition, bacteriological quality and heavy metals in the sediments alkalized by quicklime and magnesium hydroxide were analyzed. The optimum reaction was obtained from the following conditions : a 1:4 mixture of dry sediment to food wastes and the addition of 30% quicklime to the mixture. According to the classification standard for compost constituent by Higgins, all composts had a low or intermediate grade in T-N and K2O content, a low grade in P2O5 and a high grade in CaO and MgO content. Stabilization by quicklime and magnesium hydroxide is likely to inhibit the bacterial decomposition of organic matter and the activity of pathogenic organisms. Raising the pH of stabilized sediments to 12 for 2 hours(PSRP criteria of EPA) allowed 99.99% of the coliform group, fecal group and viable cell count to be reduced. The results suggested that the crude fertilizer produced by alkaline stabilization method was innoxious and thereby the sediments from coastal farming areas could be used as organic fertilizer.

The magnitudes of sea surface temperature (SST) anomalies at 13 coastal stations along the Korean peninsula in the summer and winter for the past 29years (1969-1997) are more larger than those in the spring and autumn. The periods of positive SST anomalies (negative SST anomalies) longer than 1℃ were 75(74.5) months in the eastern coast of Korea, 47.8(51.6) months in the southern coast of Korea and 69.5(69.8) months in the western coast of Korea during the past 348 months (1969-1997). The predominant periods of the low-pass filtered monthly SST anomalies are 3 years or 13 months, even another predominant period is 24 months. The spatial variation of SST anomalies were confined by regional seas of the Korean peninsula, such as the East Sea, the South Sea and the West Sea itself.

Recently, upwelling of anoxic bottom water mass have been frequently observed in northeast part of Tokyo Bay in Japan during summer to autumn. Since the colour of water surface becomes milky-blue or milky-green, the upwelling phenomenon is called `Blue Tide`. The data analysis of field surveys during `Blue Tide` appearance have been performed for understanding the physical features of the `Blue Tide` phenomena in Tokyo Bay. It becomes clear that (1) the formation of the anoxic bottom water correlates well with the temperature difference between the surface and bottom waters, (2) there are two necessary conditions for generating `Blue Tide` ; that is, strong stratification and off-shore wind. The strong southwest(on-shore) wind before the `Blue Tide` appearance may play an important role to make the stratification strengthen. When these conditions are larger and the northeast or east-northeast (off-shore) wind stronger than 5 m/s blows in succession, the `Blue Tide` upwelling appears at the head of Tokyo Bay.