• Title/Summary/Keyword: 해저면 영상

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Archeological methodology and technology for the sunken ship 'Dmitri Donskoi' exploration (침몰선 'Dmitri Donskoi' 호의 탐사 해역 설정 과정과 수중 유물 발굴의 방법론)

  • Kim, Su-Jeong;Yoo, Hai-Soo
    • 한국지구물리탐사학회:학술대회논문집
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    • 2004.08a
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    • pp.84-103
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    • 2004
  • Cruiser Dmitri Donskoi was constructed in 1895. During the Russo-Japanese War (1904-1905), she was damaged in an attack by Japanese destroyers at the battle of Tsushima, and scuttled in the east sea of Ulleungdo, Korea Peninsula on the 29th May 1905. In 2003, Dmitri Donskoi was found at the distance of 2 km off the east coast of Ulleung Island and at the depth of 400 m. Archival research was performed as the preliminary study for investigating the sunken ship.

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Comparison of the 2D/3D Acoustic Full-waveform Inversions of 3D Ocean-bottom Seismic Data (3차원 해저면 탄성파 탐사 자료에 대한 2차원/3차원 음향 전파형역산 비교)

  • Hee-Chan, Noh;Sea-Eun, Park;Hyeong-Geun, Ji;Seok-Han, Kim;Xiangyue, Li;Ju-Won, Oh
    • Geophysics and Geophysical Exploration
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    • v.25 no.4
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    • pp.203-213
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    • 2022
  • To understand an underlying geological structure via seismic imaging, the velocity information of the subsurface medium is crucial. Although the full-waveform inversion (FWI) method is considered useful for estimating subsurface velocity models, 3D FWI needs a lot-of computing power and time. Herein, we compare the calculation efficiency and accuracy of frequency-domain 2D and 3D acoustic FWIs. Thereafter, we demonstrate that the artifacts from 2D approximation can be partially suppressed via frequency-domain 2D FWI by employing diffraction angle filtering (DAF). By applying DAF, which employs only big reflection angle components, the impact of noise and out-of-plane reflections can be reduced. Additionally, it is anticipated that the DAF can create long-wavelength velocity structures for 3D FWI and migration.

Estimation of Bathymetry Changes using Hyperspectral Measurements -Focused on Haeundae beach- (초미세분광 측정치를 이용한 해저지형 변화산정 - 해운대를 중심으로 -)

  • Yang, Intae;Jo, Young-Heon
    • KSCE Journal of Civil and Environmental Engineering Research
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    • v.34 no.4
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    • pp.1335-1342
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    • 2014
  • Shallow water depths were estimated using Compact Airborne Spectrographic Imager (CASI)-1500 and mapped to analyze the bottom bathymetry changes due to the rip currents in Haeundae beach, South Korea for the first time. The depths were estimated empirically using the maximum reflectances from 420nm to 597nm wavelength of CASI and 47 in situ water depth measurements, which were compared with ground-truth bathymetry measurements. The comparisons showed that the RMSE was 1.1m with a correlation coefficient of 0.76. In addition, CASI imagery showed remarkably detailed bottom features, especially those resulting from the rip currents within the beach. Two different channels carved by the rip current were analyzed and characterized with respect to the width and slope compared to surrounding regions. While the west side of the channel showed a wide and gentle slope, the east side of the channel showed a narrow and steep slope. The estimated bathymetry map revealed that the uneven offshore bottom features were related to the transport and accumulation of sediments by the rip current, which reaches hundreds of meters offshore. Accordingly, the accumulated sediments were estimated by adding topography changes compared to the depths of the non-rip current regions. The sediments were accumulated in off channels as much as almost twice the amount of annual sand supplements along the Haeundae beach.

Remote Sensing을 이용한 태화강 하구 수심정보 획득 - Landsat 7 ETM 다중분광영상을 사용

  • Oh, Chang-Seok;Cho, Hong-Je;Song, Yeong-Min
    • Proceedings of the Korea Water Resources Association Conference
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    • 2006.05a
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    • pp.1530-1534
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    • 2006
  • 원격탐사 기법을 이용한 수심측정은 하나 혹은 그 이상의 파장대에서 수심과 반사되는 에너지 사이의 관계를 찾아내는데 달려 있다. 수심 정보를 획득하기 위한 스펙트럼의 최적 파장길이는 다중분광영상(Landsat 7 ETM)의 blue band에 해당하는 약 $0.48{\mu}m$이며, 이 band를 이용하여 연안의 수심을 측량하기도 한다. 하지만 단일밴드에 의해서 측정된 값을 이용한 수심측정은 해저표면에 의한 반사에 심각한 영향을 받을 수 있기 때문에 신뢰할 만한 결과를 얻을 수 없다. 따라서 본 연구에서는 해수와 관련한 여러 가지 변수들을 결정하기 위하여 다량의 실측 데이터를 필요로 하지 않는 선형다중밴드방식을 이용하여 2개의 Landsat 영상으로 태화강 하구의 수심정보를 추출하고 태화강 본류에 대한 수심정보획득과 하상변동에 대한 분석 가능성을 파악하였다. 그 결과 임의로 선정한 표본 50개 지점에 대한 영상분석에 의한 수심값과 해도의 수심값의 잔차 평균이 각각 2.29m, 2.43m로 비교적 큰 잔차를 보였다. 하지만 20m 미만의 수심대의 표본만을 확인한 결과 각각 1.73m, 1.88m로 잔차 평균이 크게 감소하였다. 2000년, 2003년 영상을 비교한 결과, 1번 2번 3번 지역에서 평균적으로 약 1.838m정도 2003년 수심이 감소한 것으로 나타났다. 본 연구에서 20m 미만의 수심 측량은 낮은 해상도의 위성영상이라도 실제 수심과 근접하고 있는 것으로 판단 할 수 있었다. 이것으로 넓은 지역을 경제적으로 수심자료를 획득할 수 있는 위성영상분석을 이용한 수심측정은 활용성이 있는 것으로 나타났다. 하지만 해저표면의 형태와 해수면의 상태 등 수심측정에 미치는 영향에 관한 실측데이터에 대한 자료수집과 분석이 선행된다면 더욱 좋은 결과를 도출할 수 있을 것으로 판단된다.A}$는 최대암모니아 섭취률을 이용하여 구한 결과 $0.65d^{-1}$로 나타났다.EX>$60%{\sim}87%$가 수심 10m 이내에 분포하였고, 녹조강과 남조강이 우점하는 하절기에는 5m 이내에 주로 분포하였다. 취수탑 지점의 수심이 연중 $25{\sim}35m$를 유지하는 H호의 경우 간헐식 폭기장치를 가동하는 기간은 물론 그 외 기간에도 취수구의 심도를 표층 10m 이하로 유지 할 경우 전체 조류 유입량을 60% 이상 저감할 수 있을 것으로 조사되었다.심볼 및 색채 디자인 등의 작업이 수반되어야 하며, 이들을 고려한 인터넷용 GIS기본도를 신규 제작한다. 상습침수지구와 관련된 각종 GIS데이타와 각 기관이 보유하고 있는 공공정보 가운데 공간정보와 연계되어야 하는 자료를 인터넷 GIS를 이용하여 효율적으로 관리하기 위해서는 단계별 구축전략이 필요하다. 따라서 본 논문에서는 인터넷 GIS를 이용하여 상습침수구역관련 정보를 검색, 처리 및 분석할 수 있는 상습침수 구역 종합정보화 시스템을 구축토록 하였다.N, 항목에서 보 상류가 높게 나타났으나, 철거되지 않은 검전보나 안양대교보에 비해 그 차이가 크지 않은 것으로 나타났다.의 기상변화가 자발성 기흉 발생에 영향을 미친다고 추론할 수 있었다. 향후 본 연구에서 추론된 기상변화와 기흉 발생과의 인과관계를 확인하고 좀 더 구체화하기 위한 연구가 필요할 것이다.게 이루어질 수 있을 것으로 기대된다.는 초과수익률이 상승하지만, 이후로는 감소하므로, 반전거래전략을 활용하는 경우 주식투자기간은 24개월이하의 중단기가 적합함을 발견하였다. 이상의 행태적 측면과 투자성과측면의 실증결과를 통하여 한국주식시장에 있어서 시장수익률을 평균적으로 초과할 수 있는 거래전략은 존재하므로 이러한 전략을 개발 및 활용할 수

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Sea Level Valiability and Eddy in the South Indian Ocean by Multi-satellite Data (Topex/Poseidon, ERS1) (복합위성자료(Topex/Poseidon, ERS1)를 이용한 남인도양의 해수면 변화와 와동류 연구)

  • 윤홍주;서영상
    • Korean Journal of Remote Sensing
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    • v.19 no.4
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    • pp.271-276
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    • 2003
  • Sea level variability and eddy in the Amsterdam-Crozet-Kerguelen region of the South Indian Ocean were studied during 1 year (October 15, 1992~October 15, 1993) using multi-satellite data (Topex/Poseidon, ERS1) produced by signal treatment. We found that sea level variabilities (>10cm) generally exist along the Antarctic Circumpolar Current in the area of 35$^{\circ}$~46$^{\circ}$S and strong sea level variabilities (20~30cm) were especially occurred from the effects of eddy due to bottom topography in two small area: 49$^{\circ}$~57$^{\circ}$E and 38$^{\circ}$~42$^{\circ}$S, and 58$^{\circ}$~64$^{\circ}$E and 42$^{\circ}$~44$^{\circ}$S.

Seismic reflection imaging of a Warm Core Ring south of Hokkaido (훗카이도 남부 Warm Core Ring의 탄성파 반사법 영상화)

  • Yamashita, Mikiya;Yokota, Kanako;Fukao, Yoshio;Kodaira, Shuichi;Miura, Seiichi;Katsumata, Katsuro
    • Geophysics and Geophysical Exploration
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    • v.14 no.1
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    • pp.18-24
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    • 2011
  • A multi-channel seismic reflection (MCS) survey was conducted in 2009 to explore the deep crustal structure of the Pacific Plate south of Hokkaido. The survey line happened to traverse a 250-km-wide Warm Core Ring (WCR), a current eddy that had been generated by the Kuroshio Extension. We attempted to use these MCS data to delineate the WCR fine structure. The survey line consists of two profiles: one with a shot interval of 200m and the other with a shot interval of 50 m. Records from the denser shot point line show much higher background noise than the records from the sparser shot point line. We identified the origin of this noise as acoustic reverberations between the sea surface, seafloor and subsurface discontinuities, from previous shots. Results showed that a prestack migration technique could enhance the signal buried in this background noise efficiently, if the sound speed information acquired from concurrent temperature measurements is available. The WCR is acoustically an assemblage of concave reflectors dipping inward, with steeper slopes (${\sim}2^{\circ}$) on th ocean side and gentler slopes (${\sim}1^{\circ}$) on the coastal side. Within the WCR, we recognised a 30-km-wide lens-shaped structure with reflectors on the perimeter.

Deep-sea floor exploration in the East Sea using ROV HEMIRE (무인잠수정 해미래 활용 동해 저서환경 심해탐사)

  • Min, Won-Gi;Kim, Jonguk;Kim, Woong-Seo;Kim, Dong-Sung;Lee, Pan-Mook;Kang, Jung-Hoon
    • Journal of the Korea Academia-Industrial cooperation Society
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    • v.17 no.4
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    • pp.222-230
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    • 2016
  • HEMIRE is a 6,000-meter-class remotely operated vehicle (ROV) that has been developed for observation and sampling of objects of interest on the deep seabed. We first carried out deep-seabed exploration around the slopes of the Hupo Bank and the Ulleung Basin in the East Sea in June 2015. Over two weeks, a total of 10 dives were made from a support ship, the R/V Onnuri, at eight stations with water depth ranging between 194 and 2,080 m. The dive times ranged from 1 to 6 hours, depending on the operating conditions. We obtained the following results: 1) video images of the deep seafloor; 2) red snow crab density data (a major fishery resource) and inventories of deep-sea fauna, including an unrecorded organism; 3) specific topographies such as canyons slopes; 4) an undisturbed sediment core obtained using a push corer; and 5) observations of the seabed surface covered with discarded anthropogenic waste material.

Subsidence Characteristics of Artificial Reefs using Sediment Grain Size and Shear Strength (퇴적물의 입도 및 전단강도를 이용한 인공어초 침하특성)

  • Kim, Ho-Sang;Kim, Chang-Gil;Seo, Young-Kyo;Kim, Gil-Young
    • Journal of the Korean Society of Fisheries and Ocean Technology
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    • v.41 no.1
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    • pp.46-53
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    • 2005
  • This paper describes the mean grain size and shear strength properties related to subsidence characteristics using sediment samples and acoustic images obtained from artificial reef areas in Tongyoung and Jangsungpo offshore. The acoustic images collected from chirp sonar and side scan sonar show well the attitude/orientation, the distribution pattern, and the degree of subsidence of artificial reefs, suggesting the possibility of suitable site investigation and the management of the reefs using acoustic sonar. The sediments were largely composed of clayey silt and silty clay. The mean grain sizes in Tongyoung and Jangsungpo offshore show the ranges of 5${\sim}$9${\Phi}$ and 8${\sim}$9${\Phi}$, respectively. The shear strength was significantly increased at the depths of 20cm in Tongyoung offshore and 80cm in Jangsungpo offshore, corresponding to the subsidence depth of artificial reefs. The relationship between mean grain size and shear strength did not show a correlation, suggesting the shear strength does not totally depend on mean grain size. Provided subsidence characteristics with respect to various artificial reefs and seabed condition are investigated in more details, the constructing area of the reef can be more extended.

A Study on Sea Water and Ocean Current in the Sea Adjacent to Korea Peninsula - Expansion of Coastal Waters and Its Effect on Temperature Variations in The South Sea of Korea - (한반도 근해의 해류와 해수 특성 -남해연안수 확장과 수온변화-)

  • NA Jung-Yul;HAN Sang-Kyu;CHO Kyu-Dae
    • Korean Journal of Fisheries and Aquatic Sciences
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    • v.23 no.4
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    • pp.267-279
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    • 1990
  • The temporal and spatial distribution of the coastal cold waters which was formed due to winter colling in the South Sea of Korea was analyzed by IR images from satellite and in situ data from shipboard observations. The coastal waters are known to be consisted of the Yellow Sea Coastal Waters(YSCW) and the South Korean Coastal Waters(SKCW). The former is driven around the Chuja-do and drifted into the Cheju Strait by residual currents, while the latter expands toward offsea by southward wind forcing. The expansion patterns of the SKCW were observed as sinking expansion or drifting expansion such that both were strongly dependent on the surface heat flux conditions. Under the condition of positive heat flux(warmer sea surface) or when the sea surface heat is lost to the atmosphere, the surface water started sinking and eventually expanded toward the open sea causing the cooling of the water column. For the negative heat flux the surface water was just drifted horizontally and expanded seaward and in this case only the surface layer of water was cooled.

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Improving target recognition of active sonar multi-layer processor through deep learning of a small amounts of imbalanced data (소수 불균형 데이터의 심층학습을 통한 능동소나 다층처리기의 표적 인식성 개선)

  • Young-Woo Ryu;Jeong-Goo Kim
    • The Journal of the Acoustical Society of Korea
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    • v.43 no.2
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    • pp.225-233
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    • 2024
  • Active sonar transmits sound waves to detect covertly maneuvering underwater objects and detects the signals reflected back from the target. However, in addition to the target's echo, the active sonar's received signal is mixed with seafloor, sea surface reverberation, biological noise, and other noise, making target recognition difficult. Conventional techniques for detecting signals above a threshold not only cause false detections or miss targets depending on the set threshold, but also have the problem of having to set an appropriate threshold for various underwater environments. To overcome this, research has been conducted on automatic calculation of threshold values through techniques such as Constant False Alarm Rate (CFAR) and application of advanced tracking filters and association techniques, but there are limitations in environments where a significant number of detections occur. As deep learning technology has recently developed, efforts have been made to apply it in the field of underwater target detection, but it is very difficult to acquire active sonar data for discriminator learning, so not only is the data rare, but there are only a very small number of targets and a relatively large number of non-targets. There are difficulties due to the imbalance of data. In this paper, the image of the energy distribution of the detection signal is used, and a classifier is learned in a way that takes into account the imbalance of the data to distinguish between targets and non-targets and added to the existing technique. Through the proposed technique, target misclassification was minimized and non-targets were eliminated, making target recognition easier for active sonar operators. And the effectiveness of the proposed technique was verified through sea experiment data obtained in the East Sea.