• 한국정보통신학회:학술대회논문집
• /
• 한국해양정보통신학회 2001년도 추계종합학술대회
• /
• pp.300-303
• /
• 2001

The first 7 years of altimeter data from the TOPEX/POSEIDON (T/P) were analyzed to study the surface circulation and its variability in the East Asian Marginal Seas. Long term averaged T/P sea level time series data where compared with in situ sea level measurements from a float-operated type tide gauge around of south Korea and Japan. T/P data are a large contaminated by 60-day tidal aliasing effect, very near the alias periods of M2 and S2. When this 60-day effect is removed, the data agree well with the tide gauge data with 4.6 cm averaged RMS difference. The T/P derived sea level variability reveals clearly the well-known, strong current-topography such as Kuroshio. The T/P mean sea level of North Pacific (NP) was higher than Yellow Sea (YS) and East Sea (ES). The T/P sea level valibility, with strong eddy and meandaring, was the largest in eastern part of Japan and this variability was mainly due to the influence of bottom topography in Kuroshio Extention area.

• 한국해양학회지:바다
• /
• 제23권3호
• /
• pp.125-151
• /
• 2018

지난 20년간(1998-2017년) 한국해양학회지(바다)와 한국수산과학회지에 실린 한글 논문 중 우리나라 주변 바다 이름을 지도에 표기한 논문들을 대상으로 그 표기 방법을 살펴보았다. 지도에 표기된 바다 명칭들의 형태는 크게 세 가지 - 'East Sea(동해)와 Yellow Sea(황해)', 'East Sea(동해), Yellow Sea(황해), South Sea(남해)', 'East Sea(동해), West Sea(서해), South Sea(남해)' - 가 있다. 'East Sea'는 모든 논문에서 'East Sea'로 표기된 반면, 'Yellow Sea'는 'West Sea'와 혼용해서 사용되고 있었다. 'Korea Strait(대한해협)' 대신 'South Sea'의 사용 빈도도 높았다. 이 결과는 연구자들이 해안선으로부터 가까운 연안해역을 우리나라를 기준으로 지리적 방위에 근간하여 부를 때 사용하는 바다 명칭과 주변해에 대한 국제적인 바다 명칭을 혼용하여 사용하고 있음을 보여 준다. 따라서 우리나라 해양 수산 연구자들이 바다 이름표기에 관한 기준을 세우고 일관성 있게 표기하는 것이 시급하다. 이와 관련하여 이 연구에서는 연구논문 작성 시에 주변해와 우리나라 연안해역에 대한 바다 명칭을 서로 구분하여 사용할 것을 제안하였다. 즉, 주변해는 국제적으로 통용되고 있는 'East Sea(동해)', 'Yellow Sea(황해)', 'Korea Strait(대한해협)', 'East China Sea(동중국해)'로 사용하고, 이들 주변 바다에 포함되어 있는 연안해역은 우리나라를 기준으로 상대적 방위에 근거한 'Coastal Sea off the East Coast of Korea(한국 동쪽 연안 바다)', 'Coastal Sea off the West Coast of Korea(한국 서쪽 연안 바다)', 'Coastal Sea off the South Coast of Korea(한국 남쪽 연안 바다)' 등으로 표현할 수 있다. 다른 표현으로는 'East Korea Coastal Zone', 'South Coastal Zone of Korea', 'West Korea Coastal Zone'으로도 표현할 수 있다. 작은 규모의 특정 해역의 경우 해양지명(해상지명과 해저지명)을 사용하여 연구해역을 표기할 수 있다.

• Ocean and Polar Research
• /
• 제28권2호
• /
• pp.175-186
• /
• 2006

There are disputes for oil and gas development between China and Japan in the East China Sea. These involve the area where China is already carrying out activities of oil and gas development and where Japan is proclaiming its EEZ. China insists that the Chinese activities on oil and gas development area are being carried out within the Chinese jurisdictional waters even if the median line principle of Japanese proclamation is applied in delimitation. Indeed, the permit for Japanese development is causing disputes between China and Japan because its permit allows development in the waters adjacent to Chinese development area. h the event, the core of this dispute around the oil and gas field in the East China Sea relates to issues of maritime boundary delimitation and issues of resources acquisition with both states. Chinese policy on oil and gas development is to first consider development issues in accordance with a median line principle where waters toward to China from the median line should be developed by China and the area toward Japan from the median line within the Chinese continental shelf should be jointly developed. However, the Japanese position is that the East China Sea should be jointly developed, and Japan hopes to eventually convince China to accept its median line delimitation. With on-going development of such issues, Korea should establish a strategy of negotiation based on analyses of resource distributional conditions and other strategic factors in the Korean delimitation area. In particular, Korea should prepare and make the best use of joint development zone established in an agreement between the ROK and Japan concerning the development of the southern part of continental shelf adjacent to both states.

• Ocean and Polar Research
• /
• 제23권1호
• /
• pp.35-49
• /
• 2001

An ichthyofauna analysis of the East Sea using quantitative investigation procedures for latitudinal variations of the species richness and clustering of the species list is presented to illustrate the application of the adopted geographical scaling (less than 1:10,000,000) which provides a principal opportunity for common benthic and pelagic biogeographical zonation. The distribution of both pelagic and benthic marine fish biota at a scale of biosphere (or its major sections) was highly influenced by spatial nonuniformity of hydrological structure associated with the various water circulations and frontal zones. Following zoogeographical zonations were established for the East Sea: Osaka, East Korea, Primorye, North Primorye, Northern East Sea, Uetsu, Tsugaru, Soya and West Sakhalin.

• Fisheries and Aquatic Sciences
• /
• 제9권3호
• /
• pp.129-133
• /
• 2006

We examined the distribution and biology of cephalopods collected during joint Korean-Russian surveys of the East/Japan Sea in 1993 and 1994. A total of six species of cephalopods belonging to five families were collected during the surveys: one sepiid squid, four teuthid squids, and one octopus.

• 한국수산과학회지
• /
• 제18권4호
• /
• pp.374-380
• /
• 1985

12년간($1958{\sim}1969$) 동해의 경위도 2도 간격 격자상의 자료에 대한 조화분석을 통하여 동해의 표면수온, 기온 및 해면온도차의 계절적인 변화를 분석한 결과에 의하면, 동해에서 수온과 기온은 복사에너지 뿐만 아니라 해류와 계절풍에 의한 열이류의 영향을 크게 받고 있다. 동해에서 쓰시마난류가 흐르는 남동해역은 같은 위도상의 북서해역에 비하여 표면수온과 기온의 연평균이 높고 연교차의 폭이 작다. 이는 쓰시마난류에 의한 열이류 변화의 위상이 복사에너지 변화의 위상과 반대여서 계절적인 온도의 변화폭을 줄이기 때문이다. 동해에서 연평균 수온은 연평균 기온보다 $2{\sim}4^{\circ}C$ 높으며, 수온과 기온간의 차이는 계절에 따라 크게 변한다. 즉 여름에는 표면수온과 기온간에 차이가 거의 없지만, 겨울에는 수온이 기온보다 $6{\sim}10^{\circ}C$ 높으며, 겨울에 헌혈과 증발열을 통하여 해면으로부터 대기로 공급되는 에너지는 태양복사에너지의 2배에 달한다.

• 한국지역지리학회지
• /
• 제22권4호
• /
• pp.745-760
• /
• 2016

지명은 특정 물리적 공간을 나타낼 뿐만 아니라, 사회적이고 정치적인 권력 관계를 표상하고 있다. 특히 동해는 우리나라 영역을 나타내는 대표적인 지명일 뿐만 아니라, 해외에서는 일본해와 경쟁관계에 있는 지명이다. 우리나라는 국제사회에서 동해 지명 확산을 위해 다방면으로 노력하고 있으며, 점차 그 권력을 확대하고 있다. 본 연구는 프랑스를 제외한 주요 불어권 국가의 방송사 신문사의 실제 기사와 방송 내용 분석을 통해 동해 관련 표기 명칭의 현 상황을 도출하고, 프랑스에서 생산된 표기 명칭이 불어권 각 국가로 확산되는 과정과 영향력을 지명의 권력 관계 측면에서 밝히고자 하였다. 불어권 국가 중 북아프리카의 알제리, 서유럽의 벨기에, 룩셈부르크, 캐나다 퀘벡을 주요 연구 지역으로 선정하였다. 연구 결과, 북아프리카 알제리와 룩셈부르크 언론 매체는 동해 표기에 비호의적인 경향을 보인 반면, 벨기에와 퀘벡은 비교적 호의적이었다. 대체로 불어권 국가들은 프랑스의 AFP 통신으로부터 보도 자료를 제공 받고 있었는데, 동일한 기사라 하더라도 각 국가나 언론사에 따라 일본해 단독 표기를 고수하려는 매체가 있기도 하고, 경우에 따라 동해를 병기 표기하려는 의지를 보이는 곳도 있었다. 이를 통해 지명 확산과 전파의 사회적 정치적 이해 관계와 지명에서 나타난 권력관계, 대중적 지정학의 중요성을 강조하고자 하였다.

• Ocean and Polar Research
• /
• 제31권2호
• /
• pp.177-187
• /
• 2009

This study examined the multi-scale variabilities of sea surface temperature (SST) and salinity in the Japan/East Sea (JES) based on statistical analyses of observational data, with a focus on the northwestern part of the sea. The regionality of JES SST variability was estimated for different frequency ranges on semimonthly (11-17 days), monthly to seasonal (30-90 days), quasi-semiannual (157-220 days), and quasi-biennial (1.5-3 years) time scales using cluster analyses of daily gridded SST data for 1996 to 2007 from the Japan Meteorological Agency (JMA). Several significant peaks and regional cores were found in each frequency range of the SST anomaly (SSTA) oscillations. Quasi-semiannual SSTA oscillations with high amplitude were found in the south-southwestern part of the Japan Basin ($41-43^{\circ}N$) and were amplified in the area adjacent to Peter the Great Bay. Oscillations with periods of 79 and 55 days also prevailed over the southwest Japan Basin between the Yamato Rise and the continental slope. A similar method was applied to classify SST and the annual cycle of surface salinity using Generalized Digital Environmental Model (GDEM) gridded data. The Tatarskii Strait and adjacent area showed the most specific annual cycles and variability in salinity on interannual to interdecadal time scales. The most significant inverse relationship between surface salinity in the Tatarskii Strait and southern JES areas was found on the interdecadal time scale. Linkages of sea water salinity in the Tatarskii Strait with Amur River discharge and wind velocity over Amurskii Liman were also revealed.

• Ocean and Polar Research
• /
• 제30권1호
• /
• pp.119-128
• /
• 2008

Japan's new Basic Ocean Law took effect in 20 July 2007. This law contains that 1) calls for the consolidation of eight government offices that previously worked separately on maritime issues; 2) establishes a basic plan for maritime matters, and; 3) creates a comprehensive maritime policy headquarters, run by the Prime Minister. The result is a structure for the integrated promotion of maritime policy. The Minister of Land, Infrastructure and Transport has been appointed to the newly established position of maritime minister. Japan has been in conflict with Korea and China over EEZ and territory, which has caused the country to turn to ocean. If Japan puts more emphasis on sea, it will be on a collision course with neighboring countries such as Korea, China, Russia, and Taiwan. Japan has been at odds with these countries; with Korea over Dokdo islets, with China over the Senkaku Islands and the East China Sea, where gas fields lie, with Taiwan over fishery rights in the East China Sea, with Russia over the Kuril Islands. Korea's position about the establishment of Japan's new Basic Ocean Law is followed: 1) expression of Korea's position in maritime resourcces of east china sea, 2) understand of strategy for maritime resources development and maritime delimitation in China and Japan, 3) a caution for extention of EEZ and maritime activities, 4)effective and comprehensive policy establishment, and strength in R&D, 5) construction of active and responsive system for maritime issues in neighbor country.

• Journal of the korean society of oceanography
• /
• 제31권4호
• /
• pp.164-172
• /
• 1996

CREAMS (Circulation Research of the East Asian Marginal Seas) Expeditions have provided a rare opportunity to carry out precise measurements of salinity, temperature and chemical tracers extensively in all major basins of the East Sea (Japan Sea) in 1993-1996 for the first time in more than 60 years since Uda's investigation (Uda, 1934). Studies revealed unequivocal evidence that the East Sea Proper Water (ESPW), previously known as a single homogeneous water mass, is indeed made of several distinct water masses. CREAMS data further confirmed the earlier observations of Gamo et al. (1986) that properties in Deep Waters in the East Sea have been changing during at least the last 25 years. There is evidence, especially from the analysis of the DO profile, that these changes may result from a major change in the mode of deep water formation: from bottom water formation in the past to intermediate/deep water formation in recent years. The causes for these changes are not clear at the present time, but nay include natural variation and may also reflect recent global changes in regional scale. A moving-boundary box model is presented to describe current observations, predicting the turnover time of the total deep and bottom waters to the cold surface waters to be ${\sim}$80 years in 1996.