• Title/Summary/Keyword: 실측 파랑자료

Search Result 22, Processing Time 0.029 seconds

Seepage Flow Model for Analysis of the Flow Field within the Beach (해빈내의 흐름장 해석을 위한 침투류 모형)

  • 김규한;박창근;한상대;편종근
    • Journal of Korean Society of Coastal and Ocean Engineers
    • /
    • v.9 no.3
    • /
    • pp.125-131
    • /
    • 1997
  • In order to analyze the feasibility of the drain layer construction method, which is one of the beach protection methods, a hybrid model is constructed by combining the wave model and the seepage flow model. The used wave model is the analytic solution given by Shuto (1972). and the seepage flow model is used by Richards equation which governs the saturated-unsaturated flow in the porous media. It is concluded by the sensitivity analysis of the hybrid model that the most sensitive parameter in the flow field within the beach is the saturated hydraulic conductivity. The developed hybrid model will be efficiently used in the analysis of the parameter when the drain layers are constructed in the beach, if the field datas are obtained more.

  • PDF

Dynamic Responses of Offshore Meteorological Tower Under Wind and Wave (바람과 파랑을 받는 해상 풍력 기상탑의 동적 응답)

  • Kwon, Soon-Duck
    • Journal of the wind engineering institute of Korea
    • /
    • v.22 no.4
    • /
    • pp.171-177
    • /
    • 2018
  • In order to investigate the cause of damage of the offshore meteorological tower, the measured wind speed data were analyzed, the dynamic displacement due to fluctuating wind load and wave load was calculated, and the fatigue was examined for vortex-induced vibration. It was confirmed from the results that the vibration lasting for four hours occurred in the meteorological tower when the maximum wind speeds for 10 minutes were compared for both the vane anemometer and ultrasonic anemometer. The effect of the gust wind on the dynamic response of the meteorological tower was greater than the wave. However, the combined forces acting on the meteorological tower was much lower than the design force even though the wind and wave loads were simultaneously applied. The vortex-induced vibration seemed to be cause of the fatigue failure in the connecting bolts. The destruction of the offshore meteorological tower was considered to be a vortex-induced vibration, not a fluctuating fluid flows.

Improvement of the Accuracy of Short Baseline Acoustic Positioning System (단기선 (SBL) 음향위치 시스템의 정도 개선)

  • 박해훈;윤갑동
    • Journal of the Korean Institute of Navigation
    • /
    • v.17 no.1
    • /
    • pp.99-105
    • /
    • 1993
  • Underwater acoustic positioning systems have been extensively used not only in surface position fixing but also in underwater position fixing. Recently, these systems have been applied in the field of installation and underwater inspection offshore platforms etc. But in these systems are included the fixing errors as results of a signal with noise and irregular motion of vessel by ocean waves. In this paper to improve the accuracy of the position fixing a Kalman filter is applied to the short baseline(SBL) acoustic positioning system. The optimal position obtained by the Kalman filter is compared with the raw position and it is confirmed that the former is more accurate than the latter.

  • PDF

Current Status and Future Plans for Surface Current Observation by HF Radar in the Southern Jeju (제주 남부 HF Radar 표층해류 관측 현황 및 향후계획)

  • Dawoon, Jung;Jae Yeob, Kim;Jae-il, Kwon;Kyu-Min, Song
    • Journal of Korean Society of Coastal and Ocean Engineers
    • /
    • v.34 no.6
    • /
    • pp.198-210
    • /
    • 2022
  • The southern strait of Jeju is a divergence point of the Tsushima Warm Current (TWC), and it is the starting point of the thermohaline circulation in the waters of the Korean Peninsula, affecting the size and frequency of marine disasters such as typhoons and tsunamis, and has a very important oceanographic impact, such as becoming a source of harmful organisms and radioactively contaminated water. Therefore, for an immediate response to these maritime disasters, real-time ocean observation is required. However, compared to other straits, in the case of southern Jeju, such wide area marine observations are insufficient. Therefore, in this study, surface current field of the southern strait of Jeju was calculated using High-Frequency radar (HF radar). the large surface current field is calculated, and post-processing and data improvement are carried out through APM (Antenna Pattern Measurement) and FOL (First Order Line), and comparative analysis is conducted using actual data. As a result, the correlation shows improvement of 0.4~0.7 and RMSE of about 1~19 cm/s. These high-frequency radar observation results will help solve domestic issues such as response to typhoons, verification of numerical models, utilization of wide area wave data, and ocean search and rescue in the future through the establishment of an open data network.

Surface Current Measurement by Tracking a Buoy Drifted from Mara-do (마라도에서 표류된 부이의 위치추적을 이용한 표층류의 실측정보)

  • Ryu Hwangjin;Song Museok;Jung Jinyoung;Ahn Yongho
    • Journal of the Korean Society for Marine Environment & Energy
    • /
    • v.5 no.4
    • /
    • pp.41-47
    • /
    • 2002
  • The surface current in the region from Mara-do to mid of the Pacific has been measured by tracking the position of a buoy. The buoy was accidentally released from its original location, near Mara-do, and it has been drifting following the surface current. The tracking started on 27 December 2001 and continued until 29 June 2002. We combined the trace oi the buoy with the wind data available.

  • PDF

Beach Deformation Mechanisms in Haeundae Beach (해운대(海雲臺) 해수욕장(海水浴場)의 해빈변형기구(海濱變形機構))

  • Lee, Jong Sup;Park, II Heum;Kim, Cha Kyum
    • KSCE Journal of Civil and Environmental Engineering Research
    • /
    • v.14 no.3
    • /
    • pp.595-605
    • /
    • 1994
  • The field observations. data analyses and numerical experiments are performed to investigate the short and long term beach deformation mechanisms in Haeundae beach. The schematic diagrams of deposition and erosion mechanism due to the attack of typhoons are described from the analysis on the beach widths and profiles. The short term beach deformation depends strongly on the characteristics of incident waves and wave-induced currents. The main incident wave and the calibration parameters of the shoreline change model are determined using the beach width data. Beacause the main incident wave approaches obliquly from the SE direction, the net westward longshore sediment transport occurs. Therefore the unbalance of longshore sediment budget in the east of the beach where the sediment source dose not exist causes a beach erosion. On the other hand, the deposited sand in the west is lost offshore by the storm wave action.

  • PDF

Grand Circulation Process of Beach Cusp and its Seasonal Variation at the Mang-Bang Beach from the Perspective of Trapped Mode Edge Waves as the Driving Mechanism of Beach Cusp Formation (맹방해안에서 관측되는 Beach Cusp의 일 년에 걸친 대순환 과정과 계절별 특성 - 여러 생성기작 중 포획모드 Edge Waves를 중심으로)

  • Cho, Yong Jun
    • Journal of Korean Society of Coastal and Ocean Engineers
    • /
    • v.31 no.5
    • /
    • pp.265-277
    • /
    • 2019
  • Using the measured data of waves and shore-line, we reviewed the grand circulation process and seasonal variation of beach cusp at the Mang-Bang beach from the perspective of trapped mode Edge waves known as the driving mechanism of beach cusp. In order to track the temporal and spatial variation trends of beach cusp, we quantify the beach cusp in terms of its wave length and amplitude detected by threshold crossing method. In doing so, we also utilize the spectral analysis method and its associated spectral mean sand wave number. From repeated period of convergence and ensuing splitting of sand waves detected from the yearly time series of spectral mean sand wave number of beach cusp, it is shown that the grand circulation process of beach cusp at Mang-Bang beach are occurring twice from 2017. 4. 26 to 2018. 4. 20. For the case of beach area, it increased by $14,142m^2$ during this period, and the shore-line advanced by 18 m at the northen and southern parts of the Mang-Bang beach whereas the shore-line advanced by 2.4 m at the central parts of Mang-Bang beach. It is also worthy of note that the beach area rapidly increased by $30,345m^2$ from 2017.11.26. to 2017.12.22. which can be attributed to the nature of coming waves. During this period, mild swells of long period were prevailing, and their angle of attack were next to zero. These characteristics of waves imply that the main transport mode of sediment would be the cross-shore. Considering the facts that self-healing capacity of natural beaches is realized via the cross-shore sediment once temporarily eroded. it can be easily deduced that the sediment carried by the boundary layer streaming toward the shore under mild swells which normally incident toward the Mang-Bang beach makes the beach area rapidly increase from 2017.11.26. to 2017.12.22.

Numerical study on cohesive sediment flux by tidal asymmetry (조류 비대칭성에 의한 점착성 유사의 이동량 수치연구)

  • Son, Min-Woo;Kim, Sang-Ug;Kim, Jae-Hyun;Byun, Ji-Sun
    • Proceedings of the Korea Water Resources Association Conference
    • /
    • 2012.05a
    • /
    • pp.500-504
    • /
    • 2012
  • 하구부에서의 점착성 유사의 이동량(유사량)은 조류의 비대칭성, 파랑, 하천 흐름, 조류 유속과 수위의 불일치성, 유사특성, 응집현상, 하상 침식율, 바닥지형 등 많은 인자의 영향을 받는다. 본 연구는 이들 인자들이 어떻게 영향을 주는지 살펴보기 위해 점착성 유사의 이동을 모의하는 1DV 모형을 이용하여 수치실험을 실시하고 그 결과를 분석하는 것이 목적이다. 점착성 유사의 실측자료가 부족한 실정과 현상에 대한 원인을 체계적으로 연구하는 방법을 참고하여 이상적인 조류조건을 가정하고 수치모형을 적용하였다. 점착성 유사의 특성을 고려하기 위해 응집현상이 고려되었고 가변적인 한계소류력이 적용되었다. 모의 결과를 통해서 조류의 한 주기 동안 이동하는 점착성 유사량은 가는 비점착성 유사의 이동량에 비해 조류 유속의 왜곡도에 영향을 덜 받을 수 있다는 결론이 도출되었다. 이러한 점은 가변적인 한계소류력에 기인하는 것으로 고려되며, 점착성 유사의 이동량을 연구하는 경우 가변적인 한계소류력이 고려되어야 한다는 점을 알 수 있다. 조류의 유속이 왜곡된 경우 하천으로부터 유하하는 유량이 크지 않은 경우 유사량의 방향이 조류 1 주기의 평균방향과 다를 수 있다는 결론 역시 도출된다. 조류의 수위와 유속 사이의 위상차가 유사량에 큰 영향을 주는 것으로 나타났다. 위상차가 무시되는 진행파 형태의 조류의 경우 큰 유사량을 나타내지만 약 $90^{\circ}$의 위상차를 나타내는 정상파의 경우는 무시할 정도의 유사량이 계산되었다. 위상차가 하구부의 형태에 따라서 결정된다는 점을 생각할 때 자연적 변화, 인위적 공사 등에 따라 하구부의 형태적 변화가 발생하는 경우는 유사량의 변화 역시 고려되어야 한다는 점을 알 수 있다. 이상적인 조건에서 수행된 본 연구의 보다 객관적인 검증을 위해 Ems/Dollard 하구부에서 측정된 수위, 유속, 부유사 농도 자료와 비교하였다. 그 결과 본 연구의 이상적인 조건과 유사한 특성을 나타낸다는 점을 알 수 있었고 본 연구의 결과가 자연에서 나타나는 현상의 특성을 대변할 수 있을 것으로 유추된다.

  • PDF

Validation of Sea Surface Wind Estimated from KOMPSAT-5 Backscattering Coefficient Data (KOMPSAT-5 후방산란계수 자료로 산출된 해상풍 검증)

  • Jang, Jae-Cheol;Park, Kyung-Ae;Yang, Dochul
    • Korean Journal of Remote Sensing
    • /
    • v.34 no.6_3
    • /
    • pp.1383-1398
    • /
    • 2018
  • Sea surface wind is one of the most fundamental variables for understanding diverse marine phenomena. Although scatterometers have produced global wind field data since the early 1990's, the data has been used limitedly in oceanic applications due to it slow spatial resolution, especially at coastal regions. Synthetic Aperture Radar (SAR) is capable to produce high resolution wind field data. KOMPSAT-5 is the first Korean satellite equipped with X-band SAR instrument and is able to retrieve the sea surface wind. This study presents the validation results of sea surface wind derived from the KOMPSAT-5 backscattering coefficient data for the first time. We collected 18 KOMPSAT-5 ES mode data to produce a matchup database collocated with buoy stations. In order to calculate the accurate wind speed, we preprocessed the SAR data, including land masking, speckle noise reduction, and ship detection, and converted the in-situ wind to 10-m neutral wind as reference wind data using Liu-Katsaros-Businger (LKB) model. The sea surface winds based on XMOD2 show root-mean-square errors of about $2.41-2.74m\;s^{-1}$ depending on backscattering coefficient conversion equations. In-depth analyses on the wind speed errors derived from KOMPSAT-5 backscattering coefficient data reveal the existence of diverse potential error factors such as image quality related to range ambiguity, discrete and discontinuous distribution of incidence angle, change in marine atmospheric environment, impacts on atmospheric gravity waves, ocean wave spectrum, and internal wave.

A Qualitative Analysis on the Deformation of HAEUNDE Beach Profiles (해운대사빈(海雲臺砂濱)의 단면천이특성(斷面遷移特性)에 관한 해석적(解析的) 연구(硏究))

  • Yang, Yun Mo;Ham, Gye Un
    • KSCE Journal of Civil and Environmental Engineering Research
    • /
    • v.3 no.3
    • /
    • pp.9-18
    • /
    • 1983
  • In many geological investigation, a data sequence may be created which consisted of a succession of mutually exclusive state. However, now our interest lie in the nature of transition from one state to another, rather than in the position of states in the sequence. In this paper, authors studied for the deformation of HAEUNDAE beach by transition matrices and empirical eigenfunction method. In this paper, 5-yr. set of profile data from HAEUNDAE beach measured at several monthly or yearly intervals are analyzed by using the transition matrices and empirical eigen-function. Results of this study indicate that the transition matrices and empirical eigenfunctions are useful in the analysis of beach profile data and provide objective insight in the nature of profile configuration.

  • PDF