• 한국해양학회지
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• 제2권1_2호
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• pp.1-12
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• 1967

바다의 플랭크톤은 장소와 시기에 따라 출현종류와 수량에 많은 변동이 있고, 이것들의 종적조성, 출현수량 또는 그 분포는 바다의 생태계를 구명하고, 해역의 생산성을 계측하는데 극히 중요한 기초적지식이 될뿐아니라 어업과 바다의 양 증식 에도 직접적인 관련을 갖는 중요한 자료가 된다.

• 해양환경안전학회지
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• 제16권2호
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• pp.153-159
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• 2010

본 연구는 1969~2007년간 한국 전체의 어업생산통계자료에서 멸치 및 미역 생산량 중 1990~2007년간 동해남부해역의 변동 양상을 파악하다. 이를 위하여 국립수산과학원의 같은 기간의 207선 수온자료를 이용하였다. 표층수온의 저온화 시기가 4월이면 미역 생장에 호영향을 주어 미역의 생산량이 많고, 그 시기가 6월이면 멸치에 악영향을 주어 멸치의 생산량이 적게 나타났다. 반대로 표층수온의 고온화 시기가 4월이면 미역 생장에 악영향을 주어 미역의 생산량은 적었고, 그 시기가 6월이면 멸치에 호영향을 주어 멸치의 생산량이 많았다. 표층 수온이 고온화 되면 멸치 생산량은 증가하고, 표층수온이 저온화 되면 미역 생산량은 증가하는 것으로 나타났다.

• 한국해양학회지:바다
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• 제18권3호
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• pp.131-141
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• 2013

본 연구는 2011년 9월에서 12월까지 동해(북부, 중부, 남부), 서해, 동중국해의 해구에서 각각 채집된 살오징어의 계군을 형태 및 유전학 차이를 이용하여 구분하였다. 형태학적 차이에 따른 계군분석은 평균성숙외투장(20-22 cm)을 기준으로 하여 발생시기를 구분하였고, 유전학적 특성에 따른 계군은 mtDNA COI 영역의 염기변이에 의한 유전자 다양성을 이용하여 확인하였다. 본 연구 결과 평균성숙외투장을 기준으로 동해 북부는 발생시기가 하계군, 나머지 집단(동해 중부, 동해 남부, 동중국해 북부, 서해 북부)은 추계군으로 크게 2개의 계군으로 추정되었다. 유전자 분석결과 살오징어 mtDNA COI 영역에서 총 49개의 haplotype을 확인하였다. TCS 분석결과 haplotype 유전자형 네트워크가 star-like형태이며, 모든 집단에서 유전적 다양성(haplotype diversity, h)이 높고(h=0.661~0.841), 반면에 염기 다양도(nucleotide diversity, ${\pi}$)가 낮게 나타난 점으로 미루어보아 국내 서식 살오징어의 경우 최근에 급속한 집단의 분화가 이루어진 것으로 판단된다. Pairwise Fst를 이용한 집단분석결과 비록 모든 집단간의 유전적 차이가 낮게 나타났지만(Fst = 0.001~0.043) 평균성숙외투장 기준으로 같은 추계군으로 분류된 집단(동해 중부, 동해남부, 서해 북부)간에는 유전적 차이를 확인할 수 있었다(P<0.05).

• 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.

• 한국환경과학회지
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• 제20권11호
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• pp.1425-1435
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• 2011

Time-series change in Gyeongpo beach shoreline was illustrated using DGPS(Differential Global Positioning System, resolution < 0.6m) observation from April, 2009 to April, 2010. The shoreline was subdivided into 12 areas, and westward and eastward movement of shoreline position at each area was calculated. In general, the shoreline moved toward sea during summer, and it moved toward land during winter. The southern and northern part of the shoreline had different pattern in time-series. The shoreline in the southern part moved toward sea during summer and moved toward land during winter, but time-series pattern of the shoreline in the northern part was more complicated than that in the southern part. Pattern of time-series change in the northern part was made up of three different types; the first is that the shoreline moves continuously toward land, and the second thing is that the shoreline's movement is the opposite to the southern part, and the third thing is that the shoreline maintains a state of equilibrium without any great fluctuation. The total length of the shoreline was the largest during winter and the smallest during summer. In general, time-series change in the shoreline had positive(+) relationship with sea surface pressure and wind speed.

• 해양환경안전학회지
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• 제22권1호
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• pp.145-151
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• 2016

수온과 기후 지수 자료를 이용하여 한국주변해 상층부의 수온변동과 북태평양 기후체제와의 관계를 분석하였다. 1970, 1980 그리고 1990년대 후반에 발생한 기후체제전환은 해양생태계의 구조 변화에 중요한 영향을 끼쳤다. 북서태평양 대륙주변부에 위치한 우리나라 주변해역 또한, 10년 이상의 장주기적인 변화의 영향을 받지만, 해역별 반응은 다르다. 동해, 서해, 남해 상층부(10 m)의 경우 1988년의 기후체제전환은 3개 해역의 상층부 수온변화에서 동시에 나타난다. 반면, 1998년은 동해남부해역과 서해, 1976년의 기후체제전환은 전 해역의 겨울철 수온변화에서만 그 영향이 나타난다. 1998년 기후체제전환 이후, 서해, 동중국해, 동해 남부의 수온은 점차 감소하지만, 동해 북부해역은 1988년 기후체제전환 이후 증가하는 형태이다.

• Fisheries and Aquatic Sciences
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• 제10권3호
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• pp.150-158
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• 2007

Data on squid catches, water temperature, and climatic factors collected for the Northwest and subtropical North Pacific were analyzed to examine the influence of oceanic and climatic conditions in spawning grounds on catches of Japanese common squid, Todarodes pacificus, in the East (Japan) Sea. The main spawning ground was divided into four sub-areas: the South Sea of Korea (R1), the southern waters off Jeju, Korea (R2), the southwestern part of Kyushu, Japan (R3), and the northern part of Okinawa, Japan (R4). Interannual and decadal fluctuations in water temperatures correlated well with squid catches in the East/Japan Sea. In particular, water temperatures at a depth of 50 to 100 m in sub-areas R3 and R4 showed higher correlation coefficients (0.54 to 0.59, p<0.01) in relation to squid catches in the East/Japan Sea than for R1 and R2, which had correlation coefficients of 0.40 or less (p>0.05). Air temperature and wind velocity fluctuations in each sub-area are correlated with water temperature fluctuations and were closely connected with variations in the surface mixed layers. Water, air temperatures and wind velocities at the main spawning grounds are linked to the Southern Oscillation Index (SOI) with higher signals in the ca. 2-4-year band. Strong changes in a specific band and phase occurred around 1976/77 and 1986/87, coincident with changes in squid catches.

• Journal of the korean society of oceanography
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• 제32권3호
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• pp.128-137
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• 1997

This study presents results from a detailed sedimentological investigation of surface sediments obtained from the Korea Strait region, the southern part of the East Sea (Sea of Japan). The distribution of different types of bottom sediments is controlled by the recent fine-grained sediment transport and deposition combined with the lowerings of sea level during the last glacial period, forming a diverse mixture of organic-rich fine-grained and shelly coarse-grained sediments. In comparison to high organic concentration of fine-grained sediments in the inner continental shelf and slope areas, the shell-rich coarse-grained sediments on the outer shelf are discernible being further modified. These coarse-grained sediments are confirmed as relict resulting from the sediment dynamics during the lower sea levels of the last glacial period. Clay mineral distribution of the fine-grained sediments gives information about the transport mechanism. Presence of present-day current system (the Tsushima Warm Current) is most probable source for the fine-grained particles into the open East Sea from the East China Sea, indicating that Holocene sediment dynamics may be used to explain the observed distribution of surface coarse-grained shell-rich sediments.

• Ocean and Polar Research
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• 제40권3호
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• pp.127-143
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• 2018

This study analyzed the influence of climate change on the spawning ground area of the common squid, Todarodes pacificus. To estimate long term changes in the area of the spawning ground of the common squid, water temperature at 50 m deep that can be inferred from sea surface temperature (SST) based on both NOAA/AVHRR (1981.07-2002.12) and MODIS/AQUA (2003.01-2009.12) ocean color data was analyzed. In addition, five climate indices, Arctic Oscillation Index (AO), Siberian High Index (SH), Aleutian Low Pressure Index (ALP), East Asia Winter Monsoon Index (EAWM) and Pacific Decadal Oscillation (PDO) which are the main indicators of climate changes in the northwestern Pacific were used to study the relationship between the magnitude of the estimated spawning ground and climate indices. The area of the estimated spawning ground was highly correlated with the total catch of common squid throughout four decades. The area of the estimated spawning ground was negatively correlated with SH and EAWM. Especially, PDO was negatively correlated with the area of the spawning ground in the northwestern Pacific (r = -0.39) and in the southern part of the East Sea (r = -0.38). There was a positive relationship between the AO and the area of the spawning ground in the northwestern Pacific (r = 0.46) as well as in the southern part of the East Sea (r = 0.32). Temporally, the area of the winter spawning ground in the southern part of the East Sea in the 1980s was smaller than those areas in the 1990s and 2000s, because the area was disconnected with the western coastal spawning ground of Japan in the 1980s, while the area had been made wider and more continuous from the Korea strait to the western coastal water of Honshu in the 1990s and 2000s.

• 해양환경안전학회:학술대회논문집
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• 해양환경안전학회 2003년도 추계학술발표회
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• pp.167-174
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• 2003

Oceanic conditions of the Tsushirm Wann Current (1WC) region in the southern area if the East Sea (the Japan Sea) are examined using data obtained from a CREAMS (Circulation Research if the East Asian Marginal Seas) cruise in June 1996. In 1990s, a lower temperature appears in $19\%$ and in this period, two branch of the TWC exist and the first branch of the TWC flows inshore if the Japanese coastal region compared to tfr1t in the other years, especially in the sfr1llower water layer at less th:1n about 2mm. The TWC cored with the higher salinity (>34.6 psu) is clearly observed over the continental shelf zone in the Japanese coastal region and offshore and identified by geostrophic calculation Intrusion if the TWC into the East Sea through the Korea Strait (the Tsushima Strait) makes the density structure in the water column change and the water mass in the TWC region is unstable based on Brunt- Vaisala frequency.