• 한국환경과학회지
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• 제14권11호
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• pp.1015-1026
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• 2005

The southeastern coastal area of the Korean peninsula has a complex terrain including an irregular coastline and moderately high mountains. This implies that mesoscale circulations such as mountain-valley breeze and land-sea breeze can play an important role in wind field and ocean forcing. In this study, to improve the accuracy of complex coastal rind field(surface wind and sea surface wind), we carried out the sensitivity experiments based on PBL schemes in PSU/NCAR Mesoscale Model (MM5), which is being used in the operational system at Korea Meteorological Administration. Four widely used PBL parameterization schemes in sensitivity experiments were chosen: Medium-Range Forecast (MRF), High-resolution Blackadar, Eta, and Gayno-Seaman scheme. Thereafter, case(2004. 8. 26 - 8. 27) of weak-gradient flows was simulated, and the time series and the vertical profiles of the simulated wind speed and wind direction were compared with those of hourly surface observations (AWS, BUOY) and QuikSCAT data. In the simulated results, the strength of rind speed of all schemes was overestimated in complex coastal regions, while that of about four different schemes was underestimated in islands and over the sea. Sea surface wind using the Eta scheme showed the highest wind speed over the sea and its distribution was similar to the observational data. Horizontal distribution of the simulated wind direction was very similar to that of real observational data in case of all schemes. Simulated and observed vertical distribution of wind field was also similar under boundary layer(about 1 km), however the simulated wind speed was underestimated in upper layer.

• 한국해안해양공학회지
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• 제18권4호
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• pp.301-307
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• 2006

서해안과 같이 큰 조차를 가진 연안해역에서 항만건설과 매립사업이 널리 진행되고 있으며, 대부분의 사업은 방조제 건설을 필요로 한다. 대부분의 방조제는 내부와 외부사이에 해수가 교환되지 않으나, 사석만을 사용해서 축조된 방파제와 가호안의 투수성 제방에서는 해수가 교환된다. 내부의 수면은 외부 조위의 변화에 따라 시간에 따라 변화하나 그 조차는 해수교환시 제방에서의 큰 마찰로 인하여 외부보다는 작다. 지금까지의 연구에서는 제방을 통한 해수교환을 무시하는 것이 조석모델링에서 일반적이다. 이는 내부의 해수면 변화를 계산할 수 없을 뿐 아니라 물막이 공사와 같이 일부 개방구간이 존재하는 경우에 개방구간만을 통한 해수교환량만을 고려하고, 제체를 통한 해수교환량을 무시하여 내부의 조위와 실제 해수교환량을 부정확하게 계산한다. 본 연구에서는 지하수이론을 이용하여 해수유동모의시 투수성 제체를 통한 해수교환량을 정확히 고려할 수 있도록 하였다.

• 한국지반신소재학회논문집
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• 제22권2호
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• pp.13-21
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• 2023

최근 지구온난화 등으로 인하여 지구의 평균해수면이 상승하는 추세이다. 삼면이 바다인 국내의 경우 연안침식이 초래되어 국토 손실 및 연안의 위험성을 높일 가능성이 있다. 미생물에 의한 탄산칼슘 형성(MICP) 기술은 미생물에 의한 탄산칼슘침강 기술이며, 지반의 강성과 강도를 증진시키는 친환경적 방법이다. 본 연구에서는 연안 침식 저감을 위하여 MICP 기술을 제안하였다. 연안 조건을 고려하여 용매로 해수를 사용하고 탈염수와 그 성능을 비교하였다. 탈염수와 해수 조건하에서 미생물에 의한 요소분해능을 조사하였다. 소일칼럼을 제작하여 MICP 처리된 모래의 강도 평가를 실시하였다. MICP 처리는 표면살포법에 의해 처리되었는데, 이러한 방식은 기존의 혼합 방식과 달라 전통적인 강도 평가 방식은 적절하지 않음을 확인하였다. 미세 구조 분석을 통해 다른 용매가 사용된 경우의 광물적 변화를 관측하였다. 실험 결과, 해수는 미생물에 의한 요소분해 반응을 느리게 만드는 것을 확인하였다. 표면 경화된 모래는 침관입시험을 통해 효과적으로 평가할 수 있었다. 이 연구에서는 해수를 용매로 사용하여도 탈염수 수준으로 충분히 MICP 기술 적용이 가능함을 확인하였다.

• 한국수산과학회지
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• 제27권3호
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• pp.314-325
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• 1994

Characteristics of climate in the eastern coastal regions of Korean Peninsula were studied using the meteorological and coastal sea surface temperature (SST) data which were compiled from 1961 to 1990. In the winter half year (from October to March), air temperature (AT) and precipitation of the eastern coastal regions were considerably higher than those of the western and inland regions, but relative humidity was $8{\sim}15\%$ lower. AT of coastal regions was closely related to the variation of coastal SST. These characteristics were more noticeable in the eastern coastal areas and in lower latitude regions. Quantitatively, the $1.0^{\circ}C$ variation of coastal SST may have resulted in the $1.0^{\circ}C{\sim}1.5^{\circ}C$ variation for AT in coastal regions. In the same way as temperature, vapor pressure in coastal regions was also influenced by coastal SST. Relative humidity change corresponding to the $1.0^{\circ}C$ variation of coastal SST was $3.7\%{\sim}6.5\%$. Net heat exchange amounts were positive (sea surface gaining energy) in all coastal regions. Sea surface gained net heat from March to September, and lost it from October to February. Variation of AT in coastal regions was also related to the sensible and latent heat exchanges. Sensible and latent heat amount corresponding to the $1.0^{\circ}C$ variation of AT were $10Wm^{-2}$ at Kangnung, and $8Wm^{-2}$ at Pohang and $13Wm^{-2}$ at Pusan.

• 한국해양학회지
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• 제11권2호
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• pp.43-50
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• 1976

해양과 대기간의 열교환에 관한 문제는 세계적으로 여러 학자들의 연구에 의해서 강조되어 온 바와 같이 해양학과 기상학에서 매우 중요한 비중을 차지하고 있는 분야 로서 선진제국의 이에 대한 관심과 연구열은 매우 다대하다. 한국근해에서의 해양과 대기간의 열교환에 관하여는 Jacobs(1951), Manabe(1957, 1958), Ninomiya(1964,1968) Wyrtki(1965, 1968), Takahashi(1969), Moriyasu(1952, 1969), Ishida(1970) 및 한( 1970, 1972) 등의 조사보고가 있으나 이들은 대개 한국근해를 중심으로 다루어진 것이 아니거나 시기적으로 또는 지역적으로 국한되어 있는 것이므로 우리나라 근해에서의 전반적인 열교환에 관하여는 보고된 바가 거의 없는 실정이다.

• 한국환경과학회지
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• 제23권2호
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• pp.261-274
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• 2014

This work investigates the relationship between the sea breeze circulation and ozone concentrations during cold water events in the southeastern coastal area of the Korean Peninsula, where coastal upwelling frequently occur. This analysis was performed based on the classification of two categories, such as cold water and non-cold water events, over the period of 2000-2009. The low air temperature ($0.5^{\circ}C$), low SST ($5^{\circ}C$) and the wind direction(southerly) are the features of the cold water events in the Southeastern coastal area. Moreover, ozone concentrations in the cases of the sea breeze circulation and cold water events were significantly lower (below 30 ppb) than those (70~100 ppb) in the non-clod water events, because of the low air temperature ($10{\sim}20^{\circ}C$) and high wind speed (3~5 m/s) around the southeastern coastal area.

• 한국수산과학회지
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• 제53권5호
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• pp.761-772
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• 2020

In order to study about species composition and community structure of fish in the coastal water off Boryeong were investigated from January 2018 to December 2019. A total of 10,863 individuals of 87 species of 44 families were collected. The dominant species were Liparis tanakai accounted for 19.8 percent of the total with Amblychaeturichthys hexanema and Collichthys niveatus accounted for 12.4 percent and 11.0 percent of the total number. A cluster analysis based on the Bray-Curtis similarity revealed that the fish community divided into two groups, According to season. The fish species that appeared summer and autumn were mainly migratory, while the fish species that appeared in spring and winter were mainly resident species. Fish caught by stow net had a high percentage of immature fish. It presented that coastal water off Boryeong is located an important spawning and nursery for fisheries resource.

• 한국대기환경학회지
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• 제27권4호
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• pp.416-425
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• 2011

To analyze the physical processes of sea-breeze development over a coastal urban area, numerical simulation for seabreeze (SB) and its frontogenesis was examined based on urbanized MM5 (uMM5) with urban canopy parameterization. On 6 August 2006, SB and its front were well developed in Busan under a weak offshore flow. As a result of wind vector, ZVB (Zero Velocity Boundary), potential temperature obtained the uMM5, at 0900 LST, SB advanced below 200 m height in the coastal areas and the internal boundary grew with the urban coastal region. At noon, the height of the SB head with updraft was approximately one and a half times (~600 m) higher than its depth in central urban. Applying the frontogenesis function, the SB structure for frontogenesis and frontolysis were complicated spatially; the dynamic effects of wind (i.e. convergence and tilting term) could play an important role in the growth of SB, especially the convergence effect.

• 환경영향평가
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• 제12권4호
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• pp.291-302
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• 2003

This paper examined the impacts of the regional developments and dwellers behavior on the Seacoast. Seacoast features a variety of landforms which are created by the action of waves and tidal flows. The coastal landforms are found mainly in the interface between land and sea. Although erosional landforms constitute prominent landscape features as sea stack, sea arch, and rock cliff do, it is nonetheless the depositional features such as beaches, tidal flats, offshore bars, deltas, sanddunes, and coastal plains that have various ramifications for human communities. Among these, beaches and coastal sanddunes are special in that their formation is attributable to the combined action of waves, tidal flows, and winds. The main line of discussion in this dissertation is concerned with the transformation of group of beaches sanddunes along the coastline of Chungcheong-Namdo Province. To some extent, the erosion of coastal dunes has been a global phenomenon. The degradation process occurs most actively when the spring tides attack beaches, berms, and foredunes. Also involved in the transformation of coastal dunes are factors of human agency. The extent, speed, and pattern of their morphological changes are a function of land-use pattern. The reclamation of swale and the exploitation of sands as construction material and silica sand, for example, ruin the feature of coastal dunes.

• Journal of the korean society of oceanography
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• 제37권4호
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• pp.212-223
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• 2002

Cochlodinium polykrikoides bloom in 1995 was studied with a focus on an unusual coastal environment in the South Sea of Korea. Data on temperature, salinity, and zooplankton biomass during 1965-1998 and nutrients during 1990-1998 and chlorophyll-a during 1995-1998 were used in this study. These data were obtained from the serial oceanographic observations in Korean waters carried out by the National Fisheries Research and Development Institute. In 1995 the C. polykrikoides bloom began in the coastal area around Narodo Island in August and consequently occurred to the whole coastal area of the South and East Seas of Korea. During June-October 1995, the coastal environment was unusual compared with the long-term means during 1965-1998. In June 1995, sea surface temperature was 1-2$^{\circ}C$ warmer than in other years in all coastal areas, while salinity was high only to the east of Jeju Island. In August 1995, a strong coastal front appeared inshore of a line between Jeju and Tsushima Islands. In particular, a strong coastal front which showed the characteristics of upwelling front occurred in the coastal area around Narodo and Sorido Islands, not only because of a strong intrusion of the Tsushima Warm Current but also because of the upwelling of cold bottom water. Salinity was low in the neighboring waters of western side of Jeju Island. Nutrients and chlorophyll-a were high in the inshore area between Narodo and Sorido Islands in 1995 in contrast with the other years and areas. Zooplankton showed an unusually high abundance in the coastal area in October 1995. We conclude that the Tsushima Warm Current strongly influenced the South Sea of Korea in 1995 and created strong upwelling front bordering cold upwelled water in the coastal area around Narodo and Sorido Islands. It leads us that these physical structures introduce the favorable environment for the development of C. polykrikoides blooms. We suggest that C. polykrikoides has a bio-physical tolerance of high shear and stress and prefers frontal and upwelling relaxed areas as its habitat. We also find that nutrients were not supplied to the coastal area from the offshore where a low salinity water mass with high nutrients appeared around Jeju Island. Because the strong upwelling front protect the reach of offshore low saline water mass. The main source of nutrients was the upwelled water mass in the coastal area of Wando-Narodo-Sorido.