• 제목/요약/키워드: Complex Coastline

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해안선의 형태를 고려한 지하수 해안 유출량 평가 기법 (Assessment of Coastal Ground Water Discharge for Complex Coastlines)

  • 한수영;홍성훈;박남식
    • 한국수자원학회논문집
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    • 제37권11호
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    • pp.939-947
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    • 2004
  • 해안을 통하여 유출되는 지하수량은 하천 유출량에 비하여 상대적으로 크기는 작으나 해안 지역의 지하수자원의 개발과 연안의 오염과 관련하여 중요성을 가진다. 선행 연구에서는 관측정 수위, 투수계수 등의 간단한 자료만을 가지고 지하수의 해안 유출량을 평가하는 방법을 제시하였다 본 연구에서는 남해안과 서해안과 같이 해안선의 형태가 복잡한 경우에 평균동수경사, 해안선의 폭과 담수층의 평균 두께를 산정하는 방법을 제시하여 지하수 해안유출량 평가의 정확도를 높이는 방법을 제안하였다. 제안된 평가 방법은 경계면모델을 이용한 수치해와 비교하여 평가되었다. 해안선의 복잡성을 고려하지 않은 Darcy의 법칙의 적용에 비하여 정확도가 대폭 개선되었다.

지형적 특징이 해풍시작에 미치는 영향에 대한 연구 (A Study on Modification of Geographical Features Affecting Onset of Sea Breeze)

  • 정우식;이화운
    • 한국대기환경학회지
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    • 제19권6호
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    • pp.757-772
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    • 2003
  • We simulate the geographical effects on the onset time of sea breeze at Suyoung and Haeundae districts by using the LCM (Local Circulation Model). The following can be found out from the numerical simulation on Case I (real terrain) which considered the real geography of Busan metropolitan area. Especially, as a result of analyzing the land breeze path, it could be found along the coastline as it flows out through low land coastal area. To find out more about the effects of terrain and geography on the onset time of sea breeze, the results of numerical simulation of virtual geography are as follows. In Case II (flat terrain), to find out how the terrain slope affects the onset of sea breeze, flat land and the ocean was considered. As a result, convergence of nighttime air mass at a Suyoung area and nighttime strong wind speed phenomenon was not shown. In Case III (modified flat terrain), to find out the effects of the irregularity of coastline affecting the onset of sea breeze, numerical simulation was carried out by simplifying the complex coastline into segments of straight coastline. So land breeze system and changing process of sea breeze after sunrise at Suyoung and Haeundae was simulated almost in a similar manner. Through this we could find the effects of coastal irregularities on onset of sea breeze.

The study of masan barber's coastal line change during 100years

  • Choi, Chul-Uong;Kim, Young-Seop;Cho, Sung-Hwan
    • 대한원격탐사학회:학술대회논문집
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    • 대한원격탐사학회 2002년도 Proceedings of International Symposium on Remote Sensing
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    • pp.273-273
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    • 2002
  • Masan barber was situated in S.Korean southern central coast. And it is contributing greatly in S.korea's economy development to international trading port of Heaven's blessing that possess natural, geographical situation. Also, because there are Masan free tax area and chanwon heavy industrial complex, sachon air industrial complex etc. on back, it is important permanency in our country. Specially, because inland transport routes such as southern highway, Guma highway and national road system are developed well, the importance is very high. Masan harbor 1899.05.01 be that opened, the 1st and 2nd (central pier) was build 1938∼1944 year, and the 3rd pier was 1973∼1978 year. the 4th pier was 1974∼1983 year, 5th pier was 1984∼1988, 6th pier (west pier) was 1985∼1992 year. it was developed over 100 years. But, it did great many harbor and bay development of last 100 yens but research about coastline change and seashore reclamation is insufficient. Therefore, this research executed research about coastline change of Masan bay of last 100 years, In this study, we analyzed aerial photographs and tide data for the past 100 years using digital aerial photo analysis and GIS techniques for each 3-year interval. We abstracted beach DEM (digital elevation model) and ortho aerial photographs, and conducted a space analysis. As a result, we were able to identify changes in the area As a result, we drew 10 years cycle coastline change of Masan bay. and we can detect bay coastal line change and calculate refill rate.

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현장관측에 의한 친환경 해안조성을 위한 침식방지 호안공 개발에 관한 기초적 연구 (Basic Research on Revetments Development of Erosion Protection for Coastline Creation of Hydrophilic Environment by Field Observation)

  • 이종석;한재명
    • 한국수자원학회논문집
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    • 제41권10호
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    • pp.983-993
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    • 2008
  • 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 연안침식 방지 보호 능력이 우수한 친수성 호안공을 개발하고자 한다. 개발한 호안공의 성능과 기능의 확보를 위해 모형실험이 반사율, 파량, 월파고에 대해 수행되었다. 그 결과는 일반 계단형 보다 훨씬 좋은 결과를 나타냈다. 또한 호안공의 실용화를 위해 현장실험은 노출부 일단면의 식생실험과 해안역의 침식구간에 시공실험을 실시하였다. 후자의 경우는 실험구간에서 많은 양의 모래가 짧은 시간에 퇴적되어 연안침식 방지 및 보호용 친수 호안공으로서의 현장 적용성을 확인하였다.

연안지역 특성에 따른 상세 토지피복도 적용 효과 및 기상장에 미치는 영향 분석 (The Application of High-resolution Land Cover and Its Effects on Near-surface Meteorological Fields in Two Different Coastal Areas)

  • 정주희;김유근
    • 한국대기환경학회지
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    • 제25권5호
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    • pp.432-449
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    • 2009
  • In this study, the effects of high-resolution land cover on the simulation of near-surface meteorological fields were evaluated in two different coastal regions using Weather Research and Forecasting (WRF) model. These analyses were performed using the middle classification land cover data upgraded by the Korean Ministry of Environment (KME). For the purpose of this study, two coastal areas were selected as follows: (1) the southwestern coastal (SWC) region characterized by complex shoreline and (2) the eastern coastal (EC) region described a high mountain and a simple coastline. The result showed that the application of high-resolution land cover were found to be notably distinguished between the SWC and EC regions. The land cover improvement has contributed to generate the realistic complex coastline and the distribution of small islands in the SWC region and the expansion of urban and built-up land along the sea front in the EC region, respectively. The model study indicated that the improvement of land cover caused a temperature change on wide areas of inland and nearby sea for the SWC region, and narrow areas along the coastal line for the EC region. These temperature variations in the two regions resulted in a decrease and an increase in land-breeze and sea-breeze intensity, respectively (especially the SWC region). Interestingly, the improvement of land cover can contribute large enough to change wind distributions over the sea in coastal areas.

복잡 연안지역의 지표면 자료 상세화에 따른 수치 기상장 분석 (Analysis of Numerical Meteorological Fields due to the Detailed Surface Data in Complex Coastal Area)

  • 이화운;전원배;이순환;최현정
    • 한국대기환경학회지
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    • 제24권6호
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    • pp.649-661
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    • 2008
  • The impact of the detailed surface data on regional meteorological fields in complex coastal area is studied using RAMS. Resolutions of topography and land use data are very important to numerical modeling, because high resolution data can reflect correct terrain height and detail characteristics of the surface. Especially, in complex coastal region such as Gwangyang area, southern area in Korean Peninsula, high resolution topography and land use data are indispensable for accurate modeling results. This study investigated the effect of resolutions of terrain data using SRTM with 3 second resolution topography and KLU with 1 second resolution land use data. Case HR was the experiment using high resolution data, whereas Case LR used low resolution data. In Case HR, computed surface temperature was higher than Case LR along the coastline and wind speed was $1{\sim}2m/s$ weaker than Case LR. Time series of temperature and wind speed indicated great agreement with the observation data. Moreover, Case HR indicated outstanding results on statistical analysis such as regression, root mean square error, index of agreement.

해양경계획정제도에 대한 중국의 입장과 통킹만 사례고찰 (Maritime Boundary Delimitation Regime for the Gulf of Tonkin Dispute and China's Position)

  • 양희철;박성욱;권문상
    • Ocean and Polar Research
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    • 제26권4호
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    • pp.669-678
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    • 2004
  • Coastal states are adopting maritime boundary delimitation as their primary maritime policy because maritime jurisdiction directly relates to vast economic interest. This becomes specially important and sensitive when complex maritime boundary issues are involved between neighboring coastal states. China has not actively carried out nor declared maritime boundary delimitation until recently with any country except Agreement between China and Viet Nam on the demarcation of the territorial water, the exclusive economic zones and the continental shelf of China and Vet Nam in the Gulf of Tonkin on 25 December 2000 (hereinafter, the Gulf of Tonkin Agreement). The principles that governs maritime boundary delimitation are to consider primarily an agreement between States concerned, however, if no agreement can be reached, all relevant circumstances are considered to achieve an equity between concerned States. Relevant circumstances are length of coastline, form of coastline, existence and position of island or islands, speciality of geology/topography, and factor of economy and deffnce. Factors which sinologists are considering in regard to continental shelf delimitation of the Yellow Sea are as follows; i) geographical factor, ii) geological factor, iii) topographical factor, iv) environment and ecological (factor, v) historic interest, and vi) social and economic interest. The 'Gulf of Tonkin Agreement' is completed by basically applying the principle of delimitation according to median line which seems that China has adopted the maritime boundary delimitation principle of 'half and half' which was the intention of chinese government. At the same time, China recognized Viet Nam's dominion and sovereign right over the partial exclusive economic zone and the continental shelf of Dao Bach Long Vi in Gulf of Tonkin. This case can be considered as an example of mutual concession or compromise in delimiting maritime boundary for states of concerned.

풍력자원 평가를 위한 한반도 수치바람모의 (Numerical Simulation to Evaluate Wind Resource of Korea)

  • 이화운;김동혁;김민정;이순환;박순영;김현구
    • 한국신재생에너지학회:학술대회논문집
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    • 한국신재생에너지학회 2008년도 춘계학술대회 논문집
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    • pp.300-302
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    • 2008
  • For the evaluation of wind resources, numerical simulation was carried out as a tool for establishing wind map around the korean peninsula. Initial and boundary condition are given by 3 hourly RDAPS(Regional Data Assimilation and Prediction System) data of KMA(Korea Meteorology Administration) and high resolution terrain elevation land cover(30 seconds) data from USGS(United States Geological Survey). Furthermore, Data assimilation was adopted to improve initial meteorological data with buoy and QuikSCAT seawinds data. The simulation was performed from 2003 to 2006 year. To understand wind data correctly in complex terrain as the korean peninsula, at this research, Wind map was classified 4 categories by distance from coastline and elevation.

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한반도 남동해안 해상풍 모의에 적합한 경계층 물리방안 연구 (Study on planetary boundary layer schemes suitable for simulation of sea surface wind in the southeastern coastal area, Korea)

  • 김유근;정주희;배주현;송상근;서장원
    • 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.

C-밴드 다중시기 SAR 위성 영상을 이용한 녹산국가산업단지 일대의 지반침하 관측 (Ground Subsidence Measurements of Noksan National Industrial Complex using C-band Multi-temporal SAR images)

  • 조민지;이창욱
    • 대한원격탐사학회지
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    • 제30권2호
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    • pp.161-172
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    • 2014
  • 녹산국가산업단지가 설립된 부산 낙동강 하류는 국내에서 연약지반이 가장 깊이 분포하고 있는 지역 중에 하나이다. 연약지반의 깊이가 깊은 해안 매립지의 경우, 장기간에 걸쳐 상당히 큰 잔류침하가 발생하게 된다. 본 연구는 RADARSAT-1과 Envisat의 다중시기 SAR 영상을 이용한 차분간섭기법과 SBAS 시계열 기법을 통해, 녹산산업국가단지에서 2002년 9월부터 2007년 4월 동안에 발생된 지반침하를 관측하였다. 그 결과 연구지역의 동쪽 중앙, 서쪽 중앙, 서쪽, 해안가와 닿아있는 남단에서 최대 10 cm/yr, 평균 6 cm/yr의 속도로 지반침하가 발생되고 있음을 확인하였다. 또한 RADARSAT-1 SAR 영상을 이용한 평균지표변위도는 2001년부터 2002년까지 침하계로 관측된 현장관측자료와 비교 분석되었다. 시간에 따른 지표변위 양상이 거의 선형에 가깝게 나타나므로, 연구지역의 지반침하가 안정권에 접어들 때까지 지속적인 모니터링이 필요할 것으로 사료된다.