• Title/Summary/Keyword: the Sea of Japan/East Sea

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A Tidal Model of the East Sea (동해의 조석수치모형)

  • 최병호;이호준
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.5 no.3
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    • pp.250-262
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    • 1993
  • With the use of the two-dimensional tidal model including the tide generating potential tend tidal charts of four major tidal constituents (M$_2$, S$_2$, $K_1$, $O_1$) are presented in the East Sea (Japan Sea). Model results showed that the inclusion of tide generating force does influence the position of semi-diwrual amphidrumes in the Korean east coast but computed results are generally in .good agreements with coastal observations and also empirically drawn existing charts of this region.

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A New Species, Caprella multituberculum (Amphipoda, Caprellidae) from the East Sea in Korea (한국산 바다대벌레속(단각목, 바다대벌레과)의 1신종, Caprella multituberculum)

  • 이창목;이경숙
    • Animal Systematics, Evolution and Diversity
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    • v.12 no.4
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    • pp.281-287
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    • 1996
  • A new species of Caprellidae, Ca;rella multitberculum collected from 3 localities in the coast of the East Sea in Korea, is described and illustrated. This new species is very close to Caprella soyo Arimoto, 1934 from Japan, but is distinguished from it by having the more numerous small tubercles on body surface, the shorter flagellum of antenna 1 and the smaller appendages of abdomen. Moreover, the shape of propodus of gnathopod 2 reveals several prominent differences between the two.

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Creating a High-Definition Animation of Tsunami Propagation (지진해일 수치실험 결과의 고해상도 에니메이션 생성)

  • Kim, Kyeong-Ok;Yuk, Jin-Hee;Min, Byung-Il;Choi, Byung-Ho
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.23 no.5
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    • pp.327-334
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    • 2011
  • Simulation of the trans-oceanic or trans-basin propagation of a tsunami is a computer-intensive task. This study demonstrates an effective and detailed visualization technique to deal with the vast amount of surface-elevation and velocity-field output. This high-definition visualization technique is used to present simulations of the 1960 and 2010 Chilean earthquake tsunamis and the 1983 Central East (Japan) Sea earthquake tsunami. This tsunami-visualization method using high-definition graphic animation is an appropriate tool to show detailed tsunami-propagation behavior over an ocean or coastal sea, as exemplified by the Pacific Ocean and East (Japan) Sea tsunami events.

The Use of National Names for International Bodies of Water: Critical Perspective (공해(公海)에 대한 국가지명 사용: 비판적 관점)

  • 알렉산더B.머피
    • Journal of the Korean Geographical Society
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    • v.34 no.5
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    • pp.507-516
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    • 1999
  • More than twenty-five major international bodies of water bear the names of particular nations or states. Many of these are not names are widely accepted, but considerable disagreement has developed in some cases. A systematic examination of the level of conflict over the use of national names for international bodies of water indicates that conflict is most likely to develop where shifting power relations among interested states produce concern about the hegemonic ambitions of the state after which the body of water is named. This is the case in the three situations where considerable contention exists over the use of a national name for an international body of water: the Persian Gulf/Arabian Sea, the Sea of Japan/East Sea, and the South China SealBien Dong. Cases evidencing little contention are those where either no state has a significant interest in the naming issue, or where the name that is attached to the body of water is that of a state that has not been a historic threat to others in the region. Naming international bodies of water after nations or states is potentially problematic because such appellations can connote ownership or control by a single people or political entity. An understanding of the controversies surrounding these place names requires consideration of the geopolitical context in which they are embedded.

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A Study on the Status of Chinese Fishing in the East Sea off North Korea and Directions for Countermeasures (중국 어선의 북한 동해수역 입어동향과 대응방향)

  • Lee, Jung-Sam;Ryu, Jeong-Gon;Kee, Hae-Kyung
    • The Journal of Fisheries Business Administration
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    • v.48 no.3
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    • pp.61-74
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    • 2017
  • This study is aimed to analyze the change of chinese fishing vessels' entry into the East Sea off North Korea and suggest directions for countermeasures. Based on the real landing data in China, Chinese fishing vessels' squid catch volume and value in the East Sea off North Korea are estimated. Results show that at least 205 thousand tons of squid was caught by Chinese fishing vessels in 2014. If the catch amount is calculated by the unit price per kilogram at the same year in Korea, it would be 556.3 billion KRW. As the UN sanctions become stricter with the recent resolution 2371 passed, Chinese fishing vessels' entry may increase in the future to compensate decreased seafood supply from North Korea. Even though there are not many options left for Korea to decrease the impact of Chinese depletive fishing, the study suggests countermeasures such as strengthening cooperative crack down on the Chinese illegal fishing vessels in Korean waters; increasing cooperation with UN member countries to incorporate banning the trade of fishing rights in the next UN sanctions; establishing regional fisheries management organization and managing migratory species with China and Japan cooperatively in the long term.

The Cases of International Standardization of Sea Names and Their Implications for Justifying the Name East Sea (바다 이름의 국제적 표준화 사례와 동해 표기 정당화에의 시사점)

  • Choo, Sung-Jae
    • Journal of the Korean Geographical Society
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    • v.42 no.5
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    • pp.745-760
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    • 2007
  • This study aims to categorize and analyze internationally standardized sea names based on their origins. Especially noting the cases of sea names using country names and dual naming of seas, it draws some implications for complementing logics for restoring the name East Sea. Of the 110 names for 98 bodies of water listed in the book titled Limits of Oceans and Seas, the most prevalent cases are named after adjacent geographical features; followed by commemorative names after persons, directions, and characteristics of seas. These international practices of naming seas are contrary to Japan's argument for the principle of using the name of archipelago or peninsula. There are several cases of using a single name of country in naming a sea bordering more than two countries, with no serious disputes. This implies that a specific focus should be given to peculiar situation that the name East Sea contains, rather than the negative side of using single country name. In order to strengthen the logic for justifying dual naming, it is suggested, an appropriate reference should be made to the three newly adopted cases of dual names, in the respects of the history of the surrounding region and the names, people's perception, power structure of the relevant countries, and the process of the standardization of dual names. In order to endow East Sea with the meaning of the east of the Eurasian continent, westerners' perception on the Far East should be elaborated in more detail.

Numerical Analyses of 2011 East Japan Tsunami Propagation towards Korean Peninsula (2011년 동일본 지진해일의 한반도 전파 수치해석)

  • Bae, Jae-Seok;Cho, Young-Joon;Kwon, Seok-Jae;Yoon, Sung-Bum
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.24 no.1
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    • pp.66-76
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    • 2012
  • The effect of bathymetry near the south sea area of Korea on the propagation of 2011 East Japan Tsunami is analyzed based on the numerical simulation using the finite difference dispersion-correction model. It is found that the bathymetry from the source to Korean Peninsula, such as Nankai Trough, Ryukyu Islands and the topographical lens in the East China Sea, plays an important role to reduce the tsunami height along the south coast of Korea. The mechanism involved in the transformation of tsunamis over those topographies is discussed.

CHARACTERISTICS AND ORIGIN OF THE COLD WATER MASS ALONG THE EAST COAST OF KOREA (한국 동해안에 출현하는 냉수괴의 특성과 기원)

  • Kim, Cheol Ho;Kim, Kuh
    • 한국해양학회지
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    • v.18 no.1
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    • pp.73-83
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    • 1983
  • To serch the origin of the cold water mass along the east coast of Korea its characteristics are inrestigated based upon Cooperative Study of Kuroahio and Fisheries Research and Development Agency data. In the southwestern part of the Japan Sea the North Korean Cold Water sinks at the front and flows southwards on top of the Japan Sea Proper Water. it is found that the sunken North Korean Cold Water il high in the content of dissolved oxygen and less saline compared with the Japan Sea Proper Water. It is highly likely that the cold water mass off the Jugbyeon-Chuksan coast in summer il the North Koreah Cold Water and not upwelled Japan Sea Proper Water. It os shown that the Notth Korean cold Water Flows strongly in summer and its scuthern limit is generally off Chuksan-Janggigab and occasionally off Gampo as observed in 1973.

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Strengthening Trend of Coast Guards in Northeast Asia (동북아 해양경찰 증강 동향)

  • Yoon, Sungsoon
    • Strategy21
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    • s.43
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    • pp.175-199
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    • 2018
  • Recent marine territorial disputes in the East China Sea and the South China Sea have come to us as a great threat. China, which has recently established the China Coast Guard and has rapidly developed maritime security forces, is trying to overcome the various conflict countries with its power. Japan is also strengthening intensively its maritime security forces. Since Korea, China, and Japan are geographically neighboring and sharing maritime space in Northeast Asia, there is no conflict between maritime jurisdiction and territorial rights among the countries. The struggle for initiative in the ocean is fierce among the three coastal nations in Northeast Asia. therefore, Korea needs more thorough preparation and response to protect the marine sovereignty. As the superpowers of China and Japan are confronted and the United States is involved in the balance of power in strategic purposes, the East Asian sea area is a place where tension and conflict environment exist. China's illegal fishing boats are constantly invading our waters, and they even threaten the lives of our police officers. The issue of delimiting maritime boundaries between Korea and China has yet to be solved, and is underway in both countries, and there is a possibility that the exploration activities of the continental shelf resources may collide as the agreement on the continental shelf will expire between Korea and Japan. On the other hand, conflicts in the maritime jurisdictions of the three countries in Korea, China and Japan are leading to the enhancement of maritime security forces to secure deterrence rather than military confrontation. In the situation where the unresolved sovereignty and jurisdiction conflicts of Korea, China and Japan continue, and the competition for the strengthening of the maritime powers of China and Japan becomes fierce, there is a urgent need for stabilization and enhancement of the maritime forces in our country. It is necessary to establish a new long-term strategy for enhancing the maritime security force and to carry out it. It is expected that the Korean Coast Guard, which once said that it was a model for the establishment of China's Coast Guard as a powerful force for the enforcement of the maritime law, firmly establishes itself as a key force to protect our oceans with the Navy and keeps our maritime sovereignty firmly.

On the Characteristics of the Oceanic Condition in the Surface Layer of the Northwestern East Sea (Japan Sea) (동해 북서해역의 표층해황 특성)

  • 김철호
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.8 no.2
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    • pp.215-220
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    • 1996
  • Seasonal and interannual variations of the oceanic condition in the surface layer of the northwestern East Sea are described. The seasonal variation shows two types in the water circulation. In the first type the East Korean Warm Current (EUC) Water are dominant in the East Korean Bay in spring, while in summer the cold water region develops as the North Korean Cold Current (NKCC) becomes strong. In the second type the cold water appears in the East Korean Bay from spring, but in summer the EKWC comes close to the coast, thus influencing the coastal cold water region. The characteristics of the interannual variation can be classified into 4 types according to the relative strength between the EKWC and the NKCC, and the paths of these currents. In each case various sizes of cyclonic cold eddies and/or anti-cyclonic warm eddies are formed frequently in the East Korean Bay.

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