• 제목/요약/키워드: Coast Topography

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양빈 후 지형변화에 따른 해운대 이안류 수치모의 (A numerical study on rip currents at the Haeundae coast changed after the beach nourishment)

  • 최준우
    • 한국수자원학회논문집
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    • 제55권9호
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    • pp.669-678
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    • 2022
  • 연안정비사업으로 추진된 해운대 해수욕장의 대규모 양빈(2013~2015)으로 해운대 해변의 해안선 및 수심지형에 급한 인위적 변동이 있었다. 기존 연구에서는 양빈 직, 전후의 수심지형을 입력 조건으로 Boussinesq 방정식 모형인 FUNWAVE를 이용하여 수치모의를 수행, 수심지형 변화에 따른 이안류 발생 특성을 분석하였다. 양빈 직후 쇄파대 폭의 감소로 이안류의 강도 및 발생정도가 감소하였다. 본 연구에서는 대규모 양빈 후 수년이 지난 2017년 및 2020년에 다시 측량된 수심지형을 이용하여 동일한 조건으로 수치모의를 수행하여 결과를 제시하였다. 그리고 양빈 전 및 직후, 그리고 수년이 지난 후의 해운대 이안류를 비교하였다. 시간이 지남에 따라 단면경사가 완만해 지고 쇄패대 폭이 증가되어 이안류의 강도와 발생정도가 다시 증가하고 있다고 판단된다.

상대적으로 수심이 낮고 급한 전면 경사를 갖는 직립식 호안에서의 월파량 산정에 관한 수리 및 수치 실험 (Hydraulic and Numerical Tests on Wave Overtopping for Vertical Seawall with Relatively Shallow and Steep Sloped Water Depth)

  • 김영택;최혁진;이황기
    • 한국해안·해양공학회논문집
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    • 제34권6호
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    • pp.258-265
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    • 2022
  • 국내에서 수행된 대부분의 항만구조물에 대한 월파량 산정 실험은 구조물 전면 바닥 경사가 일정한 조건 또는 전면경사면이 설치되지 않은 상태에서 수행되었다. 금번 실험에서는 직립식 호안도로 전면의 수심을 단면수로에 재현하고 외해에서 파랑 내습시 월파량을 계측하였다. 월파량의 계측은 수리실험이외에 OLAFoam을 적용하였다. 계측결과는 기존 연구성과인 EurOtop과 비교하였다. 실험 결과비교를 통하여 직립식 구조물의 경우 전면 경사면의 영향이 매우 큰 것을 알 수 있었으며, 향후 EurOtop 등의 적용시 이에 대한 검토가 필요할 것이다. 또한 OLAFoam을 활용하여 복잡한 지형을 갖는 구조물에 대해서도 월파량 예측이 가능할 것을 알 수 있었다.

Comparison of vegetation recovery according to the forest restoration technique using the satellite imagery: focus on the Goseong (1996) and East Coast (2000) forest fire

  • Yeongin Hwang;Hyeongkeun Kweon;Wonseok Kang;Joon-Woo Lee;Semyung Kwon;Yugyeong Jung;Jeonghyeon Bae;Kyeongcheol Lee;Yoonjin Sim
    • 농업과학연구
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    • 제50권3호
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    • pp.513-525
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    • 2023
  • This study was conducted to compare the level of vegetation recovery based on the forest restoration techniques (natural restoration and artificial restoration) determined using the satellite imagery that targeted forest fire damaged areas in Goseong-gun, Gangwon-do. The study site included the area affected by the Goseong forest fire (1996) and the East Coast forest fire (2000). We conducted a time-series analysis of satellite imagery on the natural restoration sites (19 sites) and artificial restoration sites (12 sites) that were created after the forest fire in 1996. In the analysis of satellite imagery, the difference normalized burn ratio (dNBR) and normalized difference vegetation index (NDVI) were calculated to compare the level of vegetation recovery between the two groups. We discovered that vegetation was restored at all of the study sites (31 locations). The satellite image-based analysis showed that the artificial restoration sites were relatively better than the natural restoration sites, but there was no statistically significant difference between the two groups (p > 0.05). Therefore, it is necessary to select a restoration technique that can achieve the goal of forest restoration, taking the topography and environment of the target site into account. We also believe that in the future, accurate diagnosis and analysis of the vegetation will be necessary through a field survey of the forest fire-damaged sites.

남해군 어촌지역 무인도 생태현황 기초연구 (The Basic Study of Ecology Status of the Uninhabited Islands of Fishing Village in Namhae-Gun)

  • 강현경;이수동;조현서
    • 농촌계획
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    • 제15권2호
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    • pp.81-96
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    • 2009
  • This study has found out the status of the environment ecology(topography structure. land-use, flora, plant community structure, wildbird) in 10 uninhabited islands(i.e. Kei island, Hadon island, Sangdon island, Daewa island, Hwanggang island, Naebi island, Oebi island, Prickly castor-oil tree island, Tongin island, Yuk island), Namhae-gun, Gyeongsangnam-do. Moreover, It has suggested ways of improving the environment ecology status by classifying the type of environment ecology about the degree of use and damage that based on the results of environment ecology survey. According to the results of topography structure survey, the survey site altitude was ranged within 1m$\sim$25m, otherwise, the radient was classified the rock area(.i.e. slope of less than $5^{\circ}$ the dead level) and the slope area where is steep slope. Moreover, there was showed evenly a variety of aspect. Land-use were divided the field(Kei island), dry native grasslands(Hadon island), naturalized grasslands(Sangdon island), Pinus thunbergii community(Dacwa island, Hwanggang island, Naebi island, Yuk island), the rock area(Oebi island, Prickly castor-oil tree island, Tongin island). As the results of flora survey, the number of plant species were 30$\sim$115 species and the naturalized species were found 2$\sim$12 species in each site. The results of plant community structure analysis, The dominant species were Pinus thunbergii and Pinus densiflora were in upper tree layer, furthermore, it were Pinus thunbergii, Eurya japonica, Prunus sargentii, Celtis sinensis, Morus bombycis, ect. in cannopy tree layer. In shrub layer, the dominant species were Rosa multiflora, Rubus crataegifolius, Parthenocissus tricuspidata, etc. The status of wildbird bird, had been found 42 species 938 individuals, especially, there were Bubo bubo kiautschensis(natural monument No. 324) and Haematopus ostralegus osculans(natural monument No. 326). According to these synthetic results, we are able to classify the 5 types of environment ecology such as the natural coast forest that composed of Pinus thunbergii and Pinus densiflora(Daewa island, Hwanggang island, Naebi island, Oebi island, Tongin island, Yuk island), the field in vegetation area(Kei island), vegetation succession area of fallow field type(Hadon island), vegetation damage area by the forest fire and disturbance elements(Prickly castor-oil tree island), dominant naturalized species grassland by grazing cattle(Sangdon island).

Seasonal Variation of Water Mass Distributions in the Eastern Yellow Sea and the Yellow Sea Warm Current

  • Pang, Ig-Chan;Hyun, Kyung-Hoon
    • Journal of the korean society of oceanography
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    • 제33권3호
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    • pp.41-52
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    • 1998
  • A seasonal circulation pattern in the eastern Yellow Sea (EYS) is suggested from the water mass analysis and geostrophic calculation using the hydrographic data collected by National Fisheries Research and Development Institute during the years of 1970 to 1990. This research focuses on the presence of inflow of warm (and saline) waters into EYS in summer. EYS is divided into two regions in this paper: the west coast of Korea (WCK) and the central Yellow Sea (CYS). In CYS, waters are linked with warm waters near Cheju Island in winter, but with cold waters from the north in summer (in the lower layer). It is not simple to say about WCK because of the influences of freshwater input and tidal mixing. Nevertheless, water mass analysis reveals that along WCK, waters have the major mixing ratios (40-60%) of warm waters in summer, while the dominant mixing ratios (50-90%) of cold waters in winter. Such a seasonal change of water mass distribution can be explained only by seasonal circulation. In winter, warm waters flow northward into CYS and cold waters flow southward along WCK. In summer, warm waters flow northward along WCK and cold waters flow southward into CYS. This circulation pattern is supported by both statistical analysis and dynamic depth topography. Accordingly, Yellow Sea Warm Current may be defined as the inflow of warm waters to CYS in winter and to WCK in summer.

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Influence of Seasonal Forcing on Habitat Use by Bottlenose Dolphins Tursiops truncatus in the Northern Adriatic Sea

  • Bearzi, Giovanni;Azzellino, Arianna;Politi, Elena;Costa, Marina;Bastianini, Mauro
    • Ocean Science Journal
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    • 제43권4호
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    • pp.175-182
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    • 2008
  • Bottlenose dolphins are the only cetaceans regularly observed in the northern Adriatic Sea, but they survive at low densities and are exposed to significant threats. This study investigates some of the factors that influence habitat use by the animals in a largely homogeneous environment by combining dolphin data with hydrological and physiographical variables sampled from oceanographic ships. Surveys were conducted year-round between 2003 and 2006, totalling 3,397 km of effort. Habitat modelling based on a binary stepwise logistic regression analysis predicted between 81% and 93% of the cells where animals were present. Seven environmental covariates were important predictors: oxygen saturation, water temperature, density anomaly, gradient of density anomaly, turbidity, distance from the nearest coast and bottom depth. The model selected consistent predictors in spring and summer. However, the relationship (inverse or direct) between each predictor and dolphin presence varied among seasons, and different predictors were selected in fall. This suggests that dolphin distribution changed depending on seasonal forcing. As the study area is relatively uniform in terms of bottom topography, habitat use by the animals seems to depend on complex interactions among hydrological variables, caused primarily by seasonal change and likely to determine shifts in prey distribution.

GSIS를 이용한 해안 지형의 시계열 변화량 추출 (Estimation of Coastal Terrain Differences by time-series using GSIS and The chart)

  • 양인태;한성만;최승필
    • 한국측량학회:학술대회논문집
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    • 한국측량학회 2002년도 창립 20주년기념 국제학술대회
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    • pp.219-228
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    • 2002
  • 서해 연안의 개발은 갯벌의 감소로 해양생태계를 위협하고 있으며 산업화에 따른 대형 매립공사는 주변의 기상변화와 해상변화를 일으켜 해저지형 및 해안선에 많은 변화를 발생시키고 있다. 또한 선박의 안전한 입, 출항을 위한 항로에 영향을 주고 있다. 따라서 본 연구는 해도에 나타난 기준선인 최저저조면의 해양 기준면을 기초 자료로 사용하여 육지부분의 해안선과 갯벌의 경계로 나타나는 0m경계선, 수심2m선을 수치화 하였으며, 수치화 된 도면을 4개의 구역으로 구분하여 분석함으로써 신공항건설과 신도시개발, 방조제공사 등의 서해 연안 개발에 따른 해안과 해저의 변화 정도를 알아보았다.

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Mean Flow and Variability in the Upper Portion of the East Sea Proper Water in the southwestern East Sea with APEX Floats

  • Lee, Homan;Kim, Tae-Hee;Kim, Ji-Ho;Seo, Jang-Won;Youn, Yong-Hoon
    • 한국환경과학회지
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    • 제13권2호
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    • pp.135-141
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    • 2004
  • Drift data from 17 Argo profiling floats in the East Sea are used to understand the mean flow and its variability in the upper portion of the East Sea Proper Water (UESPW) (around 800 m). The flow penetrates into the Ulleung basin (UB) through two paths: an extension of the southward flowing of the North Korean Cold Water along the east coast of Korea and between Ulleung Island and Dok island. Flows at 800 m are observed in the range of from 0.2 to 4.29 cms-1 and the variability in the north of the UB is larger than that in the south of the UB. In the UB, cyclonic flows from 0.3 to 1.6 cms-1 are observed with the bottom topography. We found that the mean kinetic energy (MKE) and the mean eddy kinetic energy (EKE) are 1.3 and 2.1 cm2s-2 respectively.

The Generative Mechanism of Cloud Streets

  • Kang Sung-Dae;Kimura Fujio
    • Environmental Sciences Bulletin of The Korean Environmental Sciences Society
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    • 제1권2호
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    • pp.119-124
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    • 1997
  • Cloud streets were successfully simulated by numerical model (RAMS) including an isolated mountain near the coast, large sensible heat flux from the sea surface, uniform stratification and wind velocity with low Froude number (0.25) in the inflow boundary. The well developed cloud streets between a pair of convective rolls are simulated at a level of 1 km over the sea. The following five results were obtained: 1) For the formation of the pair of convective rolls, both strong static instability and a topographically induced mechanical disturbance are strongly required at the same time. 2) Strong sensible heat flux from the sea surface is the main energy source of the pair of convective rolls, and the buoyancy caused by condensation in the cloud is negligibly small. 3) The pair of convective rolls is a complex of two sub-rolls. One is the outer roll, which has a large radius, but weak circulation, and the other is the inner roll, which has a small radius, but strong circulation. The outer roll gathers a large amount of moisture by convergence in the lower marine boundary, and the inner roll transfers the convergent moisture to the upper boundary layer by strong upward motion between them. 4) The pair of inner rolls form the line-shaped cloud streets, and keep them narrow along the center-line of the domain. 5) Both by non-hydrostatic and by hydrostatic assumptions, cloud streets can be simulated. In our case, non-hydrostatic processes enhanced somewhat the formation of cloud streets. The horizontal size of the topography does not seem to be restricted to within the small scale where non-hydrostatic effects are important.

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DRAGON-KORUS-AQ 기간 중 서해안 지역 에어로졸 광학 두께 고도별 PSCF 분석 (Assessing the Altitudinal Potential Source Contribution Function of Aerosol Optical Depth in the West Coast of Korean Peninsula during the DRAGON-KORUS-AQ Campaign)

  • 오세호;김준;손장호;배민석
    • 한국대기환경학회지
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    • 제33권1호
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    • pp.19-30
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    • 2017
  • The altitudinal potential source contribution function (PSCFa) method was developed by considering topography and height of back trajectories. The PSCFa calculated on the contributions of trans-boundary transport to the hourly mean concentrations of aerosol optical depth (AOD) of the Aerosol Robotic Network (AERONET) in the Distributed Regional Aerosol Gridded Observation Networks (DRAGON) KORea-US Air Quality (KORUS-AQ) campaign from March 31 to July 1 in 2016. Eastern China ($33^{\circ}N{\sim}35^{\circ}N$ and $119^{\circ}E{\sim}121^{\circ}E$) can be the major source of trans-boundary pollution to the western area in South Korea resulted from PSCFa (0~700 m). In this study, AOD by Moderate Resolution Imaging Spectroradiometer (MODIS) was compared to verify the source regions. Regionally, the effects of the long-range transport of pollutants from the eastern China on air quality in south Korea have become more significant over this period.