• 제목/요약/키워드: the East Sea

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Boussinesq 방정식을 이용한 동해지진해일 수치실험 연구 (A Study on the Numerical Simulation of the Seismic Sea Waves in the East Sea based on the Boussinesq Equation)

  • 김성대;정경태;박수영
    • Ocean and Polar Research
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    • 제29권1호
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    • pp.9-31
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    • 2007
  • Most seismic sea waves in the East Sea originate from earthquakes occurring near the Japanese west coast. While the waves propagate in the East Sea, they are deformed by refraction, diffraction and scattering. Though the Boussinesq equation is most applicable for such wave phenomena, it was not used in numerical modelling of seismic sea waves in the East Sea. To examine characteristics of seismic sea waves in the East Sea, numerical models based on the Boussinesq equation are established and used to simulate recent tsunamis. By considering Ursell parameter and Kajiura parameter, it is proved that Boussinesq equation is a proper equation for seismic sea waves in the East Sea. Two models based on the Boussinesq equation and linear wave equation are executed with the same initial conditions and grid size ($1min{\times}1min$), and the results are compared in various respects. The Boussinesq equation model produced better results than the linear model in respect to wave propagation and concentration of wave energy. It is also certified that the Boussinesq equation model can be used for operational purpose if it is optimized. Another Boussinesq equation model whose grid size is $40sec{\times}30sec$ is set up to simulate the 1983 and 1993 tsunamis. As the result of simulation, new propagation charts of 2 seismic sea waves focused on the Korean east coast are proposed. Even though the 1983 and 1993 tsunamis started at different areas, the propagation paths near the Korean east coast are similar and they can be distinguished into 4 paths. Among these, total energy and propagating time of the waves passing over North Korea Plateau(NKP) and South Korea Plateau(SKP) determine wave height at the Korean east coast. In case of the 1993 tsunami, the wave passing over NKP has more energy than the wave over SKP. In case of the 1983 tsunami, the huge energy of the wave passing over SKP brought about great maximum wave heights at Mukho and Imwon. The Boussinesq equation model established in this study is more useful for simulation of seismic sea waves near the Korean east coast than it is the Japanese coast. To improve understanding of seismic sea waves in shallow water, a coastal area model based on the Boussinesq equation is also required.

Estimated Advection Heat in the East/Japan Sea

  • Han, In-Seong;Kang, Yong-Q;Kim, Bok-Kee;Seong, Ki-Tack
    • 한국환경과학회:학술대회논문집
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    • 한국환경과학회 2003년도 International Symposium on Clean Environment
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    • pp.165-170
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    • 2003
  • A significant surface net heat loss appears around the Kuroshio and the Tsushima Warm Current regions. The area where the surface heat loss occurs should require heat to be supplied by the current to maintain the long-term annual heat balance. Oceanic heat advection in these regions plays an important role in the heat budget. The spatial distribution of the heat supply by the Tsushima Warm Current near the surface was examined by calculating the horizontal heat supply in the surface layer of the East/Japan Sea, directly from historical sea surface temperature and current data. We have also found a simple estimation of the effective vertical scale of heat supply by the current to compensate net heat loss using the heat supplied by the current in the surface 10m layer. The heat supplied by the current for the annual heat balance was large in the Korea/Tsushima Strait and along the Japanese Coast, and was small in the northwestern part of the East/Japan Sea. The amount of heat supplied by the current was large in the northwestern part and small in the southeastern part of the East/Japan Sea. These features suggest that the heat supplied by the Tsushima Warm Current is restricted to near the surface around the northeastern part and extends to a deeper layer around the southeastern part of the East/Japan Sea.

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A Report on the Mass Mortality of the Farmed Japanese Scallop, Patinopecten yessoensis on the Korean Coasts of the East Sea

  • Jo, Q-Tae;Kim, Su-Kyoung;Lee, Chu;Rahman, Mohammad M.;Lee, Chae-Sung;Oh, Bong-Se
    • 한국패류학회지
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    • 제25권2호
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    • pp.93-96
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    • 2009
  • Unexpected mass mortality has been one of the drawbacks in front of the stable production of Japanese scallop (Patinopecten yessoensis) on the Gangwon coasts of the East Sea. The preliminary data from our routine observation revealed that the mortality appeared to be related to variation of water temperature in the farming site and the degree of the mortality was dependent on scallop strain. The present study performed to verify the preliminary findings exhibited that the mortality was closely related to daily temperature variation rather than monthly variation. Daily temperature variation was particularly damageable to the scallop during the temperature elevation period. Scallops from hatchery seeds (Chinese strain) were more tolerant against the temperature variation over those from wild seeds. The hatchery scallop gain of the temperature tolerance was probably due to their larval experience to higher temperature in the hatchery as well as their maternal genetic acclimation to upper temperature extreme of the Chinese environment which was recently found.

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A Seasonal Circulation in the East China Sea and the Yellow Sea and its Possible Cause

  • Oh, Kyung-Hee;Pang, Ig-Chan
    • Journal of the korean society of oceanography
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    • 제35권4호
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    • pp.161-169
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    • 2000
  • A seasonal circulation in the East China Sea and the Yellow Sea and its possible cause have been studied with CSK data during 1965-1989. Water mass distributions are clear in winter, but not in summer because the upper layer waters are quite influenced by atmosphere. To solve the problem, a water mass analysis by mixing ratio is used for the lower layer waters. The results show that the distribution of Tsushima Warm Current Water expands to the Yellow Sea in winter and retreats to the East China Sea in summer. It means that there is a very slow seasonal circulation between the East China Sea and the Yellow Sea: Tsushima Warm Current Water flows into the Yellow Sea in winter and coastal water flows out of the Yellow Sea in summer. By the circulation, the front between Tsushima Warm Current Water and coastal water moves toward the shelf break in summer so that the flow is faster in the deeper region. The process eventually makes the transport in the Korea Strait increase. The Kuroshio does not seem to influence the process. A possible mechanism of the process is the seasonal change of sea surface slope due to different local effects of surface heating and diluting between the East China Sea and the Yellow Sea.

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한국 해산 히드라충류의 동물지리학적 분포 (Zoogeographical Distribution of Marine Hydroids(Cnidaria: Hydrozoa: Hydroida) in Korea)

  • 박정희
    • Animal Systematics, Evolution and Diversity
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    • 제8권2호
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    • pp.279-300
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    • 1992
  • 지금까지 밝혀진 한국 해산 히드라충류는 17과 55속 120종이다. 이 가운데 Abietinaria filicula (ellis and Solander, 1786)는 한국 미기록종으로 밝혀졌고 Sertularella miurensis Stechow, 1921는 96개 채집지 가운데 33개 지점에서 채집되어 한국해역의 히드라충류 가운데 우점종으로 나타났다. 한국 해역은 동해, 남해, 황해 그리고 제주도의 4개 해역으로 나뉜다. 각 해역에서 채집된 종수는 동해 43종, 남해 73종, 황해 52종 그리고 제주도 83종으로 나타났다. 따라서 제주도 해역은 한국 해산 히드라충류의 가장 높은 다양활르 나타낸다고 할 수 있다. 각 해역간의 군집계수는 동해-황해가 0.444, 동해-남해가 0.553, 동해-제주도가 0.519, 황해-남해가 0.682, 황해-제주도가 0.533 그리고 남해-제주도가 0.642이다. 그러므로 히드라충류의 분포에 따른 두 해역 사이의 연관은 황해-남해가 가장 높고 동해-황해가 가장 낮다.

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SEA LEVEL VARIATIONS IN THE LONG TERM IN THE EAST SEA OF KOREA

  • Cho, Keun-Han;Kim, Hee-Jong;Lee, Dong-In;Yoon, Hong-Joo
    • 대한원격탐사학회:학술대회논문집
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    • 대한원격탐사학회 2007년도 Proceedings of ISRS 2007
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    • pp.37-40
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    • 2007
  • Satellite altimetric data from 1993 to 2006 are used to study sea level variations in the long tenn in the East Sea. The trend of sea level in the East Sea is rising 4.16 mm/yr and indicate that it rose 5.82 cm in 2006 against to 1993. The South Ses is the fastest in the study areas (4.89 mm/yr, 6.84cm) and the Yellow Sea is 4.10 mm/yr and 5.75cm, respectively. The both of Mokho coast and Ulleung island are minimal sea level in March to May and maximal sea level in September to November. For periods above 20.9days, coherences are found to be higher than 95% confidence level, and the phase differences are near zero.

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A new free-living marine nematode species of the genus Phanoderma Bastian, 1865(Enoplida: Phanodermatidae) from the East Sea, Korea

  • Lee, Hyo Jin;Rho, Hyun Soo
    • 환경생물
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    • 제37권3호
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    • pp.396-405
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    • 2019
  • A new species of free-living marine nematode is described from intertidal sediments of the East Sea, Korea. Phanoderma koreense sp. nov. is characterized by the presence of well-developed pharyngeal and cephalic capsule, six inner labial sensilla present as minute papillae around with circular groove, long and slender spicules with 4-5 serrated distal end, located at the base of the precloacal supplement, a series of eight to nine stout and short setae on the ventral cloacal region and conico-cylindrical tail with two pairs of blunt setae. In this study, we provide taxonomic descriptions and illustrations of a new species by differential interference contrast microscope and a pictorial key to the valid species of Phanoderma Bastian, 1865. This is the first record of the genus Phanoderma in the East Sea, Korea.

지구환경 변화와 관련된 한국 연근해 해양 이상변동 (Anomalous Variation of the Oceanic Features around Korean Waters Related to the Global Change)

  • 서영상;장이현;황재동
    • 한국환경과학회지
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    • 제12권3호
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    • pp.257-263
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    • 2003
  • Oceanographic features around Korean waters related to the global change were studied by analysis of the longterm variation of water temperature, dissolved oxygen, sea level of the surface layer with 1$^{\circ}C$ temperature, spatial position of the subpolar front in the East Sea/Japan Sea (the East sea hereafter) and the Wolf Sunspot Number. With the global warming, the temperature of Korean waters has been increased 0.5∼1.0$^{\circ}C$ for 33years (1968∼2000). In case of the dissolved oxygen in the East Sea has been decreased 0.46$m\ell$/$\ell$. Year to year vertical fluctuations of the monthly anomalies of the surface layer with 1$^{\circ}C$water in the East Sea have predominant periods with 15years as the longterm variation of Arctic climate, 12 and 18years as the El Nino-Southern Oscillation. Spatial position of the subpolar front in the East Sea moved to northern part of the sea from the southern part of the sea with the increasing sea surface temperature. The relationship between the number of Wolf Sunspot and the anomalies of sea surface temperature was very closer after the late of 1980s than those before the early of 1980s in Korean waters.

황해 중앙부와 동중국해 북부 해역에서의 대형 독성 노무라입깃해파리의 개체군 특성 연구 (Population Characteristics of the Venomous Giant Jellyfish, Nemopilema nomurai, found in the Yellow and Northern East China Seas)

  • 장수정;기장서
    • 한국환경과학회지
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    • 제33권1호
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    • pp.87-95
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    • 2024
  • The giant jellyfish, Nemopilema nomurai, is an endemic species found in Northeast Asian waters and their population structures, such as size and genetics, and their environmental characteristics were investigated. N. nomurai was obtained from the Yellow and Northern East China Seas during the summers of 2006, 2007, and 2009. In the northern Yellow Sea, small-sized jellyfish were found to be dominant and towards the southern seas, the size of the jellyfish increased. In the northern East China Sea, only one mode of jellyfish was found in May, and the number of modes increased up-to five in July. However, at the center of the Yellow Sea, one or two modes were found in July, 2007. Thus, different jellyfish populations were present in the northern East China Sea and the Yellow Sea. However, based on first appearance and a cohort analysis using the bell diameter, the jellyfish population in the northern Yellow Sea might be recognized as a distinct group that differed from those found in the northern East China Sea. Furthermore, mitochondrial DNA sequences (cytochrome c oxidase subunit I) of N. nomurai were, determined and compared with genetic structures obtained from jellyfish in the Yellow Sea. The genetic diversity of N. nomurai was highest in the regions around the northern East China Sea and at the center of the Yellow Sea and was the lowest around the northern Yellow Sea. Thus, N. nomurai populations in the Yellow Sea and northern East China Sea might be different concerning their seeding places.