• 한국수산과학회지
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• 제25권6호
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• pp.495-500
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• 1992

1985년 한국 동해에서 격월로 수직채집된 어류 난$\cdot$자어와 동물부유생물, 그리고 동시에 관측된 수온과 염분자료를 이용하여 멸치난$\cdot$자어분포와 그 분포에 영향을 미치는 환경요인과의 관계를 연구하였다. 멸치난과 자어는 6월과 8월에 채집되었는데, 6월에는 고수온과 고염분역인 난수역에 분포하였다. 8월에는 난과 자어분포역이 외해역으로 이동하였다. 멸치난과 자어분포 및 수온, 염분, 동물부유생물 밀도의 관계를 분석한 결과 6월의 멸치 난과 자어의 분포밀도는 수온 및 염분의 분포와 정상관 관계에 있다고 분석되었다.

• Journal of the korean society of oceanography
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• 제37권4호
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• pp.212-223
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• 2002

Cochlodinium polykrikoides bloom in 1995 was studied with a focus on an unusual coastal environment in the South Sea of Korea. Data on temperature, salinity, and zooplankton biomass during 1965-1998 and nutrients during 1990-1998 and chlorophyll-a during 1995-1998 were used in this study. These data were obtained from the serial oceanographic observations in Korean waters carried out by the National Fisheries Research and Development Institute. In 1995 the C. polykrikoides bloom began in the coastal area around Narodo Island in August and consequently occurred to the whole coastal area of the South and East Seas of Korea. During June-October 1995, the coastal environment was unusual compared with the long-term means during 1965-1998. In June 1995, sea surface temperature was 1-2$^{\circ}C$ warmer than in other years in all coastal areas, while salinity was high only to the east of Jeju Island. In August 1995, a strong coastal front appeared inshore of a line between Jeju and Tsushima Islands. In particular, a strong coastal front which showed the characteristics of upwelling front occurred in the coastal area around Narodo and Sorido Islands, not only because of a strong intrusion of the Tsushima Warm Current but also because of the upwelling of cold bottom water. Salinity was low in the neighboring waters of western side of Jeju Island. Nutrients and chlorophyll-a were high in the inshore area between Narodo and Sorido Islands in 1995 in contrast with the other years and areas. Zooplankton showed an unusually high abundance in the coastal area in October 1995. We conclude that the Tsushima Warm Current strongly influenced the South Sea of Korea in 1995 and created strong upwelling front bordering cold upwelled water in the coastal area around Narodo and Sorido Islands. It leads us that these physical structures introduce the favorable environment for the development of C. polykrikoides blooms. We suggest that C. polykrikoides has a bio-physical tolerance of high shear and stress and prefers frontal and upwelling relaxed areas as its habitat. We also find that nutrients were not supplied to the coastal area from the offshore where a low salinity water mass with high nutrients appeared around Jeju Island. Because the strong upwelling front protect the reach of offshore low saline water mass. The main source of nutrients was the upwelled water mass in the coastal area of Wando-Narodo-Sorido.

• 수산해양기술연구
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• 제54권2호
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• pp.116-123
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• 2018

Pacific bluefin tuna (Thunnus orientalis) has been mostly caught by the Korean offshore large purse seine fishery in Korean waters. The annual catch of Pacific bluefin tuna caught by the offshore large purse seine fishery in Korean waters showed less than 1,000 mt until the 1990s except for 1997. The catch sharply increased to 2,401 mt in 2000 and recorded the highest of 2,601 mt in 2003, but the catch has generally decreased with a fluctuation thereafter. The main fishing ground of Pacific bluefin tuna of this fishery is formed around Jeju Island. However, it expanded to the Yellow Sea, the coastal of Busan, and the East Sea, which depends on the migration patterns of Pacific bluefin tuna by season. The CPUE standardization of Pacific bluefin tuna was conducted using Generalized Linear Model (GLM) to assess the proxy of the abundance index. The data used for the GLM were catch (weight), effort (number of hauls), catch ratio of Pacific bluefin tuna, moon phase by year, quarter and area. The standardized CPUE from 2004 to 2011, except for 2003 and 2010, showed a steady trend, and then increased until 2014. The CPUE in 2015 decreased, and in 2016 was higher than that in 2015. The result of GLM suggests that the effect of the catch ratio of Pacific bluefin tuna is the largest factor affecting the nominal CPUE.

• 한국수산과학회지
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• 제40권1호
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• pp.24-30
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• 2007

We developed an ecosystem indicator (EI) for the coastal and offshore areas of Korean waters. One of the major scientific challenges of this undertaking was to translate broad policy statements for ecosystem-based fisheries management (EBFM) into practical terms. Fish reproduction potential (FRP) was defined as an EI to describe the reproductive probability of adult fisheries resources in Korean waters. The FRP was estimated as the ratio of adult fish composition to total catch, catches (in metric tons) by species and by ecosystem, and fishery effort (in horse power per metric ton). The FRP indices of the East/japan Sea Ecosystem (EJSE), Yellow Sea Ecosystem (YSE), and East China Sea Ecosystem (ECSE) began to decrease after the mid-1980s, and the current indices have decreased further, at 0.63 (EJSE), 1.22 (YSE), and 0.68 (ECSE) index points compared to the indices of 1975, when similar catch amounts were recorded. Lower FRPs in the Korean marine ecosystems were the result of higher proportion of immature fisheries resources in the total catch. Because this kind of ecosystem-level indicator is thought to reflect scientific approaches to EBFM and to provide an important tool for assessing the current status of marine ecosystems with respect to both quantity and quality, more EIs should be developed for Korean waters.

• 한국해양학회지:바다
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• 제1권1호
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• pp.46-54
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• 1996

한반도 서해 태안반도 연근 해역에서 춘계동안 부유물 함량분포경향을 분석 하여, 부유물질의 운반 양상을 해석하였다. 특히 비파괴 방식의 SPECTREX 분석 기기를 이용하여 부유물의 입도분포를 정밀 분석하였다. 연구해역의 수괴 특성은 강한 조석전선이 형성되어, 수직적으로 균질한 수괴의 연안역과 수온약층이 뚜렷한 외양역으로 구분되었다. 부유물 함량은 대체로 10 mg/l 이하로 낮지만, 연안역의 저층수와 외양역의 중층수에서는 혼탁한 수괴가 관측되었다. 부유물은 평균입도가 각각 5-6$\mu\textrm{m}$와 8-10$\mu\textrm{m}$에 해당하는 세립질 부유물과 조립질 부유물로 구분되며, 주로 쇄설성 성분이 우세한 것으로 해석되었다. 전반적으로 태안반도 연근해역에서는 강 한 조류에 의해 해저 퇴적물의 재부유작용이 우세하며, 세립 퇴적물의 집적이 제한 되는 것으로 해석된다. 또한 경기만의 초입에 해당하는 북부역으로부터 공급되는 쇄설성 부유 퇴적물이 수온약층의 중층수역을 따라 남쪽 또는 남서쪽 방향으로 우 세하게 운반되는 것으로 해석된다.

• 한국수산과학회지
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• 제30권5호
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• pp.759-770
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• 1997

제주해협내에 설정한 3개의 남북 단면상에 배열한 13개의 관측정점과 기타 4개의 제주항 부근의 연안정점에서 $1986\~1989$년까지 실시한 해류계에 의한 해류조사결과와 $1981\~1987$년 사이에 실시된 해류판 추적조사, 일반해양관측 등에 의하여 얻어진 자료들을 종합적으로 분석하여 정리한 제주해협의 유황을 요약하면 다음과 같다. 1. 제주해협내에는 주로 동$\~$북동류의 항류가 있어, 해협 서쪽 입구의 전단면을 통하여 해협내로 유입된 해수가 동쪽 입구의 전단면을 통하여 유출되고 있으며, 이 항류의 유속은 10m층에서 $5.2cm/sec\~30cm/sec$이고, 중${\cdot}$저층은 $1.3\~24cm/sec$로 대체로 해협의 심소 및 제주도 북측에 강류대가 있고, 추자도 및 보길도 부근의 연안 천소에 악한 항류가 있다. 2. 제주해협 서쪽 입구의 전단면에서 실측한 항류의 하계 평균유속은 6.93cm/sec로, 이것을 기초로 계산한 이 단면의 해수수송량은 $0.384\times10^6\;m^3/sec(Sv)$이며, 단면의 항류분포와 지형류 유속 분포간에는 많은 차를 보였다. 3. 추자도 북서쪽의 전선역에서는 밀물 때는 북향류에 의해 고온${\cdot}$고염분의 외해수가 5mile정도 연안역으로 이동 하지만, 썰물 때는 북상 거리만큼 다시 남하하지 않고 동$\~$남동향류 때문에, 연안수와 혼합하면서 전선북쪽의 연안역으로 이동하므로, 결과적으로 추자도 북서해역은 제주도 서방해역으로 부터 북상해온 외해수가 한국남해연안수내로 유입하는 창구가 되며, 이것을 일으키는 주된 작용은 항류가 아닌 조류이다.

• 환경생물
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• 제36권3호
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• pp.260-270
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• 2018

A study describing unrecorded and taxonomically undescribed indigenous species is in progress since 2006. Samples were collected from many sites in coastal waters and offshore of Korea as well as from Jeju Island. Since 2008, we have found ten unrecorded species of four genera belonging to family Dinophysaceae, Gonyaulacaceae, Gymnodiniaceae, and Heterocapsaceae. The species are as follows, Dinophysis elongata (2016 winter), D. nasuta (2016 winter), Gonyaulax alaskensis (2016 winter), G. diegensis (2017), G. monospina (2008), Amphidinium flagellans(2017), Heterocapsa circularisquama (2017), H. horiguchii (2017), H. lanceolata (2017), and H. pygmaea (2017) (note; The numbers in the parenthesis refer to the year in which the species was reported as unrecorded indigenous species by National Institute of Biological Resources, NIBR hereafter). Among them, seven species were described as newly recorded species in Korean waters, and three have been re-described in this study.

• 환경생물
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• 제35권3호
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• pp.251-264
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• 2017

A study searching for unrecorded and taxonomically undescribed indigenous species has been conducted since 2006. Samples were collected from many sites in coastal waters and offshore in Korea as well as around Jeju Island. Since 2008 we have found 13 unrecorded species belonging to family Diplopsaliaceae, Heterocapsaceae, Kolkwitziellaceae, Protoperidiniaceae and Thoracosphaeraceae. The species are as follows, Preperidinium meunieri (2014), Heterocapsa ovata (2015), H. pseudotriquetra (2015), Diplopsalis lenticula (2008), Protoperidinium abei (2009), P. diabolus var. longipes (2010), P. depressum (synonym: P. parallelum (2008)), P. latispinum (2016), P. punctulatum (2010), P. solidicorne (synonym: P. spinosum (2010)), P. subpyriforme (2010), P. pacificum (2013), Scrippsiella hexapraecingula (2009) (note; The numbers in parenthesis refer to the year that the species was reported as unrecorded indigenous species by National Institute of Biological Resources, NIBR hereafter). Among these, 5 species were described as newly recorded species in Korean waters, and 8 were re-described in this study.

• 환경생물
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• 제35권3호
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• pp.273-288
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• 2017

An investigation focusing on the unrecorded and taxonomically undescribed indigenous has been done since 2006. Samples were collected from various sites in the coastal and offshore waters of Korea as well as around Jeju Island. Since 2008, 16 unrecorded species belonging to the family Gymnodiniaceae have been found. The species were as follows: Amphidinium thermaeum (2015), Cochlodinium convolutum (2015), C. strangulatum (2015), Gymnodinium abbreviatum (valid name: G. gracile), G. arenicola (2015), G. gracile (2015), G. dorsalisulcum (2015), G. microreticulatum (2014), G. micrum (2016) (valid name: Karlodinium micrum), G. pyrenoidosum (2016), G. simplex (2015), G. veneficum (2016) (valid name: Karlodinium veneficum), Gyrodinium aureum (2015), G. fusiforme (2015), G. dominans (2014), and Nusuttodinium latum (2016) (valid name: Amphidinium latum). (The numbers in parentheses refer to the year that the species was found). These species were newly recorded in Korean waters in this study.

• 해양환경안전학회지
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• 제9권2호
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• pp.59-64
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• 2003

국립수산과학원에서 장기간 관측한 정선해양관측자료와 연안정지관측자료를 이용하여 한국주변해역의 수온과 염분의 장기변화경향과 수층별 상관성을 보고자 하였다. 장기변화의 분석결과 한국연안수온은 하계냉수역이 발생하는 한국남서연안을 제외하고 상승하는 것으로 나타났다. 근해수온은 동해의 경우 표층은 상승하는 경향을 보인 반면 50m 와 l00m 수층은 하강하는 경향을 보였다. 남해의 경우 전 수층에서 상승하는 것으로 나타났으며, 서해의 경우 표층에서는 상승하나 50m 수층은 하강하는 것으로 나타났다. 근해염분은 동해의 경우 표층에서 하강하는 경향을 보인 반면, 50m 수층에서는 상승하는 경향을 보였으며, 100ml 수층 하강정도가 미미하게 나타났다. 남해의 경우 표층에서는 하강하는 경향을 보였으며, 50m 와 l00m 수층에서는 상승하는 경향을 보였다. 서해의 경우 표층과 50m 수층 모두 하강하는 경향을 보였다. 수층별 상관성을 보면 수온의 경우 동해와 남해에서 50m 수층과 100m 수층이 높은 상관도를 보였으나 서해의 경우 표층과 50m 수층 사이에는 상관성이 없는 것으로 나타났다. 염분의 경우 동해에서는 표층과 50m 수층이, 남해에서는 50m 와 l00m 수층이, 서해에서는 표층과 50m 수층이 높은 상관도를 보였다.