• Title/Summary/Keyword: shoreline

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Shoreline Change Model in Haeundae Beach (해운대 해빈의 해안선변형 예측 모형)

  • 박일흠;이종섭
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.1 no.1
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    • pp.50-62
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    • 1989
  • Shoreline change of Haeundae beach was predicted by one-line model considering interaction of seawalls and longshore variation of wave height . Wave deformation was calculated by combined wave refraction-diffraction model . In this shoreline change model, empirical constants and offshore sediment transport rate are treated as calibration parameters, and the calculated results are in good agreement with the observed data.

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Extraction of Coast Topographic Information Using Mobile Laser Scanning and Airborne LiDAR (지상레이저스캐너와 항공라이다를 이용한 해안 지형정보 추출)

  • Lee, In-Su;Tcha, Dek-Kee;Kim, Su-Jeong
    • Proceedings of the Korean Society of Surveying, Geodesy, Photogrammetry, and Cartography Conference
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    • 2009.04a
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    • pp.115-117
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    • 2009
  • Terrestrial Laser Scanner and Airborne Laser Scanning is one of the state of art surveying equipments. So This study deals with the combined use of mobile TLS(Terrestrial Laser Scanner) with ALS(Airborne Laser Scanning) to extract shoreline's topography information. These two systems have their own pros and cons. Mobile TLS can capture the facades of a low story building along the shoreline fast and quickly. Meanwhile, Due to viewpoint restrictions of ALS data collection, the amount of detail, which is available for the building facades is very limited. Therefore, it is recommended that the co-registration and geo-referencing methods of both two should be developed and the application of both system for shoreline mapping also should be investigated.

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An Approximate Solution for Diffraction-Induced Shoreline in a Double Headland and Comparison with Field Measurement

  • Shoaib, Muhammad;Kim, Dong Hee;Lee, Jung Lyul
    • Proceedings of the Korea Water Resources Association Conference
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    • 2016.05a
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    • pp.193-193
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    • 2016
  • In past decades beach erosion has been remarkably severe along coasts of different parts of the world, so that distinct types of coastal protective measures have been implemented; seawalls, wave-dissipating breakwaters, groins, artificial headlands or detached breakwaters have been constructed. In recent years, at Bongpeong beach, South Korea, an artificial headland was constructed to stop the beach erosion. The structure resulted in severe beach erosion of the adjoining places. In order to stop the consequences, another headland was constructed at some distance, but the construction of double headland did not prevent the erosion significantly. This paper focuses on the accurate design of the artificial double headland construction. The study presents the application of equilibrium shoreline empirical formula of parabolic type to estimate the equilibrium stages of the artificial double headland beaches and an analytic solution is presented in the present study. The research has solved the empirical formula of parabolic type to find the optimum result by considering the essential parameters that influence the erosion after the construction of double headland.

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An Accuracy Evaluation of Algorithm for Shoreline Change by using RTK-GPS (RTK-GPS를 이용한 해안선 변화 자동추출 알고리즘의 정확도 평가)

  • Lee, Jae One;Kim, Yong Suk;Lee, In Su
    • KSCE Journal of Civil and Environmental Engineering Research
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    • v.32 no.1D
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    • pp.81-88
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    • 2012
  • This present research was carried out by dividing two parts; field surveying and data processing, in order to analyze changed patterns of a shoreline. Firstly, the shoreline information measured by the precise GPS positioning during long duration was collected. Secondly, the algorithm for detecting an auto boundary with regards to the changed shoreline with multi-image data was developed. Then, a comparative research was conducted. Haeundae beach which is one of the most famous ones in Korea was selected as a test site. RTK-GPS surveying had been performed overall eight times from September 2005 to September 2009. The filed test by aerial Lidar was conducted twice on December 2006 and March 2009 respectively. As a result estimated from both sensors, there is a slight difference. The average length of shoreline analyzed by RTK-GPS is approximately 1,364.6 m, while one from aerial Lidar is about 1,402.5 m. In this investigation, the specific algorithm for detecting the shoreline detection was developed by Visual C++ MFC (Microsoft Foundation Class). The analysis result estimated by aerial photo and satellite image was 1,391.0 m. The level of reliability was 98.1% for auto boundary detection when it compared with real surveying data.

Shoreline Changes Caused by the Construction of Coastal Erosion Control Structure at the Youngrang Coast in Sockcho, East Korea (속초 영랑해안 해빈침식대책 인공구조물 건설에 기인하는 해안선 변화)

  • Kang, Yoon-Koo;Park, Hyo-Bong;Yoon, Han-Sam
    • Journal of the Korean Society for Marine Environment & Energy
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    • v.13 no.4
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    • pp.296-304
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    • 2010
  • The shoreline change caused by the construction of shore protection structures are discussed based on the example of Youngrang coast, Sokcho where the coastal erosion control system(CECS), three artificial headlands and two submerged breakwaters are being constructed. The study qualitatively analyzed the shoreline changes of Youngrang coast using available satellite/aerial photographs and camera photographs taken during the construction period of 6 years since 2002 for the artificial headlands construction. The main results from the study are as following. (1) Before the installation of the middle artificial headland, longshore drifts along Youngrang coast are transported in the NW-SE direction according to the seasonally different wave characteristics. (2) During the CECS construction the shoreline is continuously changed by altering the local longshore drift budget. Especially, the middle artificial headland induces considerable change of shoreline by blocking the sediment supply from the southern pocket beach to the northern pocket beach and by accelerating the sediment accretion at the wave shadow zone behind its head. It induces the asymmetry on the net longshore drift causing the significant erosion at the center of the southern pocket beach. (3) The study demonstrates that serious unintended erosion/accretion problem are possibly occurred due to local changes on the wave transformation and the sediment transport by the construction of coastal erosion control system.

Beach Nourishment Design for Minimum Beach Width Management at Gwangalli Beach (광안리 해수욕장의 최소 해빈폭 관리를 위한 양빈 설계)

  • Bae, Soen-Han;Lee, Jung-Lyul
    • Proceedings of the Korean Society of Disaster Information Conference
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    • 2015.11a
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    • pp.141-143
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    • 2015
  • 본 연구는 해변의 양측에서 퇴적되고 해변 중앙에서 침식이 일어나고 있는 광안리 해수욕장에 최소 해빈폭을 최대로 하는 최적의 양빈 설계를 하고자 실시하였다. 광안리 해수욕장에 3가지 case의 양빈안을 수치 모의 시나리오로 구성하여 OneLine Shoreline Model을 적용하여 해빈폭의 시간적 변화를 모의하였으며, Cross-shore Profile Model을 적용하여 연평균 파고에 따른 전진폭과 최고 파고에 따른 침식폭을 추정하였다.

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Seasonal Changes of Shorelines and Beaches on East Sea Coast, South Korea (동해안 해안선과 해빈의 계절적 변화)

  • Kim, Dae Sik;Lee, Gwang-Ryul
    • Journal of the Korean Geographical Society
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    • v.50 no.2
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    • pp.147-164
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    • 2015
  • This study analyzed characteristics and tendencies of seasonal change on shoreline and beach with 8 beaches at East Sea coast by topographical survey for 2 years from March 2012 to February 2013. The shorelines of East Sea coast appeared that amount of seasonal change was bigger than amount of annual change. The seasonal change tendencies between Gangwon-do and Gyeongsangbuk-do coast areas existed some regional differences. To synthesize seasonal changes on 8 beaches of East Sea coast, shoreline advance and beach deposit showed clearly in summer and shoreline retreat and beach erosion showed clearly in autumn. This result is different from tendencies of seasonal change in many mid-latitude coast areas of the world, but generally corresponds with reference studies in west coast and east coast. The major factor of beach erosion showing mostly in summer is storm wave caused by typhoon. The beach erosion by storm wave also occurred in late winter. And it assumes that the beach deposit showing mostly in autumn is result of equilibrium processes of coast area against strong erosion in summer.

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Quantitative Estimation of Shoreline Changes Using Multi-sensor Datasets: A Case Study for Bangamoeri Beaches (다중센서를 이용한 해안선의 정량적 변화 추정: 방아머리 해빈을 중심으로)

  • Yun, Kong-Hyun;Song, Yeong Sun
    • Korean Journal of Remote Sensing
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    • v.35 no.5_1
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    • pp.693-703
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    • 2019
  • Long-term coastal topographical data is critical for analyzing temporal and spatial changes in shorelines. Especially understanding the change trends is essential for future coastal management. For this research, in the data preparation, we obtained digital aerial images, terrestrial laser scanning data and UAV images in the year of 2009. 2018 and 2019 respectively. Also tidal observation data obtained by the Korea Hydrographic and Oceanographic Agency were used for Bangamoeri beach located in Ansan, Gyeonggi-do. In the process of it, we applied the photogrammetric technique to extract the coastline of 4.40 m from the stereo images of 2009 by stereoscopic viewing. In 2018, digital elevation model was generated by using the raw data obtained from the laser scanner and the corresponding shoreline was semi-automatically extracted. In 2019, a digital elevation model was generated from the drone images to extract the coastline. Finally the change rate of shorelines was calculated using Digital Shoreline Analysis System. Also qualitative analysis was presented.

Shoreline Changes and Erosion Protection Effects in Cotonou of Benin in the Gulf of Guinea

  • Yang, Chan-Su;Shin, Dae-Woon;Kim, Min-Jeong;Choi, Won-Jun;Jeon, Ho-Kun
    • Korean Journal of Remote Sensing
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    • v.37 no.4
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    • pp.803-813
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    • 2021
  • Coastal erosion has been a threat to coastal communities and emerged as an urgent problem. Among the coastal communities that are under perceived threat, Cotonou located in Benin, West Africa, is considered as one of the most dangerous area due to its high vulnerability. To address this problem, in 2013, the Benin authorities established seven groynes at east of Cotonou port, and two additional intermediate groynes have recently been integrated in April 2018. However, there is no quantitative analysis of groynes so far, so it is hard to know how effective they have been. To analyze effectiveness, we used optical satellite images from different time periods, especially 2004 and 2020, and then compared changes in length, width and area of shoreline in Cotonou. The study area is divided into two sectors based on the location of Cotonou port. The difference of two areas is that Sector 2 has groynes installed while Sector 1 hasn't. As result of this study, shoreline in Sector 1 showed accretion by recovering 1.20 km2 of area. In contrast, 3.67 km2 of Sector 2 disappeared due to coastal erosion, although it has groynes. This may imply that groynes helped to lessen the rate of average erosion, however, still could not perfectly stop the coastal erosion in the area. Therefore, for the next step, we assume it is recommended to study how to maximize effectiveness of groynes.

A Shoreline Change Model around Coastal Structures (해안구조물 주변에서 해안선변형 예측모형 실험)

  • 이종섭;박일현
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.2 no.2
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    • pp.67-74
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    • 1990
  • A numerical model is developed to predict the shoreline change by the coastal structures constructed. In order to describe the wave deformation at the shadow zone of the structure, the present model employs the mild-slope equation in steady state and the wave ray method using the coefficients of wave refraction, diffraction and shoaling. In the model results of shoreline changes for the various structures. it showed a qualitative agreement with the findings observed in the field such as tombolo, and the response of this model was found to be very sensitive to the longshore distribution of wave heights. It was also applied to a field area. From the results of the application this model is proved to be useful around the complex coastal structures and bottom topography.

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