• Ocean and Polar Research
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• 제23권3호
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• pp.245-253
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• 2001

To investigate the community structures and the their seasonal variation of phytoplankton and zooplankton, a study was conducted at 6 selected stations during the period from April 1999 to October 2000 in the marine ranching ground off Tongyeong. One hundred ninety species of phytoplankton were identified, including 146 diatoms, 38 dinoflagellates, 4 silicoflagellates and 2 euglenophytes. Phytoplankton standing crops varied extensively by months and stations, ranging from $3.0{\times}10^4\;cells/l\;to\;1.0{\times}10^6\;cells/l.$. The dominant species varied from the vertical distribution as well as seasonal changes. In April and July 1999, Skeletonema costatum and Ceratium fusus were predominant in both the surface and the bottom water columns. Leptocylindrus danicus was the dominant species in April and June 2000, and Thalassiosira spp. were also predominant in bottom waters in June 2000. Pseudonitzschia pungens and Chaetoceros spp. were the dominant species at both surface and near bottom waters in August and October 2000, respectively. Zooplankton abundance was comparatively high in April and July in 1999, and April, June, and October in 2000, but extremely low in November 1999. The density of dominant zooplankton was higher in 2000 than in 1999. Copepods were the most predominant group except for July 1999 when the bivalve larvae showed extremely high abundance. Acartia omorii and Oithona similis were the dominant or subdominant copepod species mainly in April 2000, and June/July, while O. davisae and O. plumifera had peaks in August and October 2000. Corycaeus affinis and Paracalanus sp. also showed higher peaks in April and June (or July), even though they occurred in all sampling time. Centropages abdominalis occurred abundantly only in April 1999. Oikopleura dioica, a gelatinous zooplankton, was another important zooplankton, showing high density in all samples except in July 1999.

• Fisheries and Aquatic Sciences
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• 제7권3호
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• pp.148-162
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• 2004

The monitoring activities at the National Fisheries Research and Development Institute (NFRDI) in Korea have been extended to include all the coastal waters of Korea after the outbreak of Cochlodinium polykrikoides blooms in 1995. We used several alternative methods including climatological analysis, spectral and optical methods which may offer potential detection of the major species of red tide in Korean waters. In the climatological analysis, NOAA, SeaWiFS, OCM satellite data was chosen using the known C. polykrikoides red tide bloom data and the area was mapped by helicopter reconnaissance and ground observation. The relationship between the distribution of sea surface temperature to C. polykrikoides bloom areas was studied. The anomalies of SeaWiFS chlorophyll a imageries against the imageries of non-occurring red tide for August, 2001 showed where the C. polykrikoides occurred. The anomalies of chlorophyll a concentrations from the satellite data during red tide outbreaks showed a similar distribution of C. polykrikoides in the red tide in August, 2001. The distribution between differences in sea surface temperatures during the day and at night also showed a possibility for red tide detection. We used a corrected vegetation index (CVI) to detect floating vegetation and submerged vegetation containing algal blooms. The results of from the optical absorption of C. polykrikoides in the ultraviolet band (340 nm) showed that if we use the optical characteristics from each red tide, we will be able to establish the feasibility of red tide detection.

• 한국해양학회지
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• 제30권3호
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• pp.163-169
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• 1995

동해 남부해역에서 1988년 5월과 1989년 7월 및 1991년 11월에 관찰된 식물 플랑크톤 집은 총 190종의 출현종을 기록하였고 규조류가 우점하고 있었다. 춘계 에는 Leptocylindrus danicus, Nitzschia pungens, Bacteriastrum delicatulum 등이 우점종으로 나타났고 하계에는 Skeletonema costatum이 전반적인 우점현상을 보였 으며 Chaetoceros socialis, Rhizosolenia alata f. gracillima 등이 수역에 따라 우점 하였다. 추계에는 Chaetoceros socialis, Nitzschia delicatissima, Nitzschia sp., Gymnodinium sp.. 등이 우점하였다. 종다양성 지수의 평균은 춘계에 1.24, 하계에 1.69, 추계에 2.12로 다소 낮게 측정되었다. 식물플랑크톤 군집의 집괴분석 결과 하 계에는 표층에서 대마난류의 영향을 받는 외양적 특성의 수계와 동해 연안의 수계 및 울릉도 주변수등 크게 3개의 수역으로 구분할 수 있는 것으로 나타났다. 한편 하계의 40m 수층 집괴분석 결과는 연구해역의 중앙부에서 표층 자료의 수역 구분 과는 별개의 또다른 식물수문학적 수역이 인지되었는데 이곳은 표층 주변의 대마 난류의 영향과 50m 이심의 수층에 존재하는 수온 1$0^{\circ}C$ 수괴의 양면적 영향을 받는 것으로 사료된다.

• 수산해양기술연구
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• 제51권4호
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• pp.520-526
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• 2015

A tragic disaster happened by capsizing O-Ryong 501 trawler at Western Bering Sea in 1st, Dec. 2014. The disaster was caused by the severe weather and the long deferred escape from the storm in fully developed high sea. Lots of sea water from poop deck rushed into the fish ponder with fishes all together after hauling net and then remove the fishes from codend. The vessel became to incline to the one side caused by the weight and the free surface effect of flood sea waters and fishes at initial stage. In spite of crews all effort to discharge the waters, but the work was not achieved successfully. For the worse thing, the order of abandon ship was issued too late. After all, the ship capsized and sank, then almost crews became to the victims of the casualty including captain. In this paper, author carried out restrictively the calculation of dynamic factors influenced on the disaster including the weather condition and effects of the flood sea waters, and found out that the most important causes of the disaster were the decrease of stabilities, GM was decreased from 0.9m to 0.08 m, and the high waves which led to the vessel disaster.

• 한국해양학회지:바다
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• 제3권1호
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• pp.25-33
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• 1998

황해 중동부 해역에서 영양염 원소들의 시, 공간적 변화를 살펴보기 위해 1995년 5월과 1995년 11월, 1996년 6월의 세 차례에 걸쳐 현장조사를 실시하고, 표층수에 대해 염분, 온도, 부유물질 및 입자태 유기탄소와 암모니아, 질산염, 아질산염, 인산염, 규산염 등의 영양염 원소를 분석하였다. 세차례의 현장 조사에서 표층수의 영양염 농도 분포는 암모니아를 제외하면 일반적으로 6월이 가장 낮고 11월이 가장 높은 값을 보이는 한편, 암모니아는 5월에 가장 낮은 농도 분포를 보이고 11월에 가장 높은 값을 보였다. 봄에는 5월에 식물 플랑크톤의 1차 생산 활동으로 영양염이 고갈된 외해역의 표층수는 6월로 되면서 수온약층과 조석전선의 발달로 저층과 강으로부터의 영양염 공급이 더욱 제한되고, 봄철 식물 플랑크톤 대번식기에 증식된 동물 플랑크톤 또는 그 배설물 등이 박테리아에 의해 분해되는 과정에서 암모니아가 수층으로 공급되는 것으로 보인다. 한편, 11월에는 늦가을로 접어들면서 봄-여름철에 형성된 성층이 깨지고 수층의 수직 혼합이 활발해지면서 성층기간 동안 저층수에 축적되었던 영양염 원소들이 표층으로 공급되는 것으로 보인다.

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

• 한국환경과학회:학술대회논문집
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• 한국환경과학회 2005년도 봄 학술발표회지 제14권(제1호)
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• pp.241-244
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• 2005

The aim of this study was to determine the first outbreaks of nontoxic Gonyaulax polygramma Stein in Yeosu waters in place of harmful Cochlodinium polykrikoides Margalef, which has occurred annually in the same coastal region since 1995. The observation of cellular arrangement and structure by electron microscopy showed that G. polygramma isolated from Yeosu waters had a few spines connecting with mem-branes and prominent longitudinal ridges on the cell surface, with a cingular dis-placement 1.5 times their cell width. Furthermore, the location of the nucleus wasposterior of large oval formation according to electron microscopy. On 6 August, 2004,the first bloom of G. pozygramma occurred, the date of own its disappearance was with a maximum cell density of 8,000 cells ml$^{-1}$ on 21 August, 2004. During the period of this study, the horizontal distribution of sea water temperature and salinity showed a strong coastal front, whereas the front of DIN (Dissolved Inoganic Nitrogen) was significantly different between the occurrence and disappearance of G. polygramma blooms. These results suggested that the process of the breakdown of stratification by wind and a low level of inorganic nitrogen play important roles in the rapid growth of G. polygrmma, which is associated with a greater robustness in growth against DIN than that of C.polykrikoides in nature.

• 한국해안해양공학회지
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• 제2권4호
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• pp.200-207
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• 1990

본 연구는 해양에서의 염료 플럼축의 사행에 관한 것이다. 농도 확산장에서의 이러한 과정은 산단 염료 확산장의 무게 중심의 분석에 대하여 속도장의 여러 주기 성분이 원점으로부터의 거리의 함수로서 차별적으로 기여하기 때문에 일어나는 것으로 이해된다. 제시된 진단 모델은 과동장을 보여줄 뿐만 아니라 플럼축이 증폭되어 사행하는 현상까지도 설명할 수 있다. 염표 플럼의 항공사진을 이용한 자료로부터 사행 과동의 파장을 추정한 바 연안 표층수에서 5.5에서 60.3 미터까지 분포하였다. 또한 수치 시뮬레이션을 통하여 사행 플럼 농도장을 예측하였다.

• 한국환경과학회지
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• 제14권7호
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• pp.639-647
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• 2005

The aim of this study is to determine the outbreaks of nontoxic Gonyaulax polygramma Stein in Yeosu waters in place of harmful Cochlodinium polykrikoides Margalef, which has occurred annually in the same region since 1995. The observation of cellular arrangement and structure by electron microscopy showed that G. polygramma isolated from Yeosu waters had a few spines connecting with membranes and prominent longitudinal ridges on the cell surface, with a cingular displacement 1.5 times their cell width. Furthermore, the location of the nucleus was posterior of large oval formation according to electron microscopy. On 6 August, 2004, the first bloom of G. polygramma occurred, the date of its disappearance was with a maximum cell density of 8,000 cells $ml^{-1}$ on 21 August, 2004. During the period of this study, the horizontal distribution of sea water temperature and salinity showed a strong coastal front, whereas the front of DIN (Dissolved Inorganic Nitrogen) was significantly different between the occurrence and disappearance of G. polygramma blooms. These results suggested that the process of the breakdown of stratification by wind and a low level of inorganic nitrogen play important roles in the rapid growth of G. polygramma, which is associated with a greater robustness in growth against DIN than that of C. polykrikoides in nature.

• 수산해양교육연구
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• 제28권5호
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• pp.1417-1434
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• 2016

Starting from the February 2008 till the end of November 2014, abundance of phytoplankton and their composition living in the coastal waters of Kyoungju city were investigated. Environmental and biological properties were also observed at 10 different stations on a seasonal basis. Due to the environmental variables, fluctuating pattern was appeared during the entire period of observation with different degree, as compared to those found in other costal waters in the East Sea. The concentration of phosphate was turned out to be very low which was even less than threshold level in the study area. Phytoplankton community structure was dominated by diatoms (both micro- and nanoplankton fractions) for several years and seasonal succession was also relied on the diatoms. The importance of dinoflagellates in the community was relatively low. Abundance of phytoplankton was heavily affected by physical factors in the surface water, however, affected more by chemical factors including nutrients in the deep water. For periods of this study, the phosphate concentrations was observed in an extremely low, which indicates that the main limiting factor affecting phytoplankton growth could be phosphate.