• Journal of the Korean Association of Geographic Information Studies
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• v.6 no.3
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• pp.139-150
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• 2003

There was a close relationship between spatio-temporal distribution of Cochlodinium polykrikoides red tide and meso-scale variation of oceanographic environment around the Korean waters. Oceanographic conditions of Narodo island, where red tide usually first occurred during summer seasons were formation of the thermohaline frontal zone from 1995 to 2001. Huge C. polykrikoides red tides were observed in every uneven year during the past 7 years (1995~2001) and quasi-biennial oscillation also occurred in the oceanographic variations of sea surface temperature and salinity in the northern part of the East China Sea during the same years. The distribution area and moving pattern of C. polykrikoides red tides were definitely depended on the temporal and spatial variation of upwelling cold water originated form the southeastern coast of the Korean peninsula in summer season.

• Journal of the Korea Institute of Information and Communication Engineering
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• v.7 no.4
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• pp.845-852
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• 2003

This study deals with the relationship between the red tide occurrence and the meteorological and marine factors, the prediction of areas where the red tide is likely to occur based on the information, and the satellite monitoring for the red tide in mid-South Sea of Korea. From 1990 to 2001, the red tide was observed every year and the number of occurrences increased as well. The red tide mostly occurred in July, August, and September. The most important meteorological factor governing the mechanisms of the increase in the number of red tide occurrences is found to be a heavy precipitation. It was found that the favorable marine environmental conditions for the red tide formation are some of marine factors such as the warm water temperature, the low salinity, the high suspended solid, the low phosphorus, and the low nitrogen. The necessary conditions for the red tide occurrence are found to be the heavy precipitation (23.4-54.5 mm) for 2∼4 days, the warm temperature $(24.6∼25.9^{\circ}C)$, proper sunshine (2∼10.3 h), and light winds (2∼4.6 m/s & SW) for the day in red tide occurrence. It was possible to monitor the spatial distributions and concentration of the red tide using the satellite images. It was found that the likely areas for red tide occurrence in August 2000 were Yosu - Dolsan coast, Gamak bay, Namhae coast, Marado coast, Goheung coast, and Deukryang bay.

• Proceedings of the Korean Institute of Information and Commucation Sciences Conference
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• 2003.05a
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• pp.323-328
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• 2003

This study deals with the relationship between the red tide occurrence and the meteorological and marine factors, the prediction of areas where the red tide is likely to occur based on the information, and the satellite monitoring for the red tide in mid-South Sea of Korea. From 1990 to 2001, the red tide was observed every year and the number of occurrences increased as well. The red tide mostly occurred in July, August, and September. The most important meteorological factor governing the mechanisms of the increase in the number of red tide occurrences is found to be a heavy precipitation. It was found that the favorable marine environmental conditions for the red tide formation are some of marine factors such as the warm water temperature, the low salinity, the high suspended solid, the low phosphorus, and the low nitrogen. The necessary conditions for the red tide occurrence are found to be the heavy precipitation (23.4∼54.5 mm) for 2∼4 days, the warm temperature (24.64-25.85 $^{\circ}C$), proper sunshine (2∼10.3 h), and light winds (2∼4.6 m/s & SW) for the day in red tide occurrence. It was possible to monitor the spatial distributions and concentration of the red tide using the satellite images. It was found from this study that the likely areas for red tide occurrence in August 2000 were Yosu ∼ Dolsan coast, Gamak bay, Namhae coast, Marado coast, Goheung coast, and Deukryang bay.

• Proceedings of the Korean Society of Fisheries Technology Conference
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• 2002.10a
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• pp.80-81
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• 2002

근년 Cochlodinium polykrikoides 적조는 막대한 경제적 피해를 입히고 있으며, 이의 방제를 위하여 우리나라에서는 황토살포와 살조세균 등에 관한 연구가 진행되어 왔으나 이 적조 발생시 양식어 폐사 등 수산업의 피해는 여전히 반복되고 있다. 우리나라에서 C. polykrikodes 적조로 인하여 양식어가 폐사하였을 때에는 전량 폐기하고 있어 수산자원의 효율적 이용이라는 측면에서 큰 손실이라 아니할 수 없다. (중략)

• Proceedings of the Korean Society of Fisheries Technology Conference
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• 2001.10a
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• pp.202-203
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• 2001

거의 매년 우리나라 연안해역에서 푸른 바닷물이 갑자기 붉은색이나 황록색으로 변하는 적조 현상을 쉽게 관찰할 수 있다. 특히, 부영양화된 폐쇄성 및 반폐쇄성 내만 해역에서부터 해수유동이 원활한 외해역까지 광범위하게 매년 상습적으로 적조가 발생하여 어장환경과 수산생물에 막대한 피해를 일으키므로서 심각한사회ㆍ경제적인 문제를 야기시키고 있다(남해안 피조발생현황, 1995, 1996.; 한국연안의 적조발생 상황, 1997, 1998, 1999, 2000). (중략)

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.21 no.1
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• pp.44-47
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• 2016

Real-time PCR was applied to early warning of red tide. For early warning of red tide at $10cells\;mL^{-1}$, Cochlodinium polykrikoides specific real-time PCR was used as a complement of microscopy that has a lower detection sensitivity. C. polykrikoides appeared extensively in Tongyeong, Namhae waters at low densities in the end of June, and early warning of C. polyrkrikoides blooms was issued on 2 August 2015.

• Journal of the Korean Society of Marine Environment & Safety
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• v.26 no.5
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• pp.523-530
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• 2020

Based on the results of harmful algal blooms (HABs) monitoring by the National Institute of Fisheries Science and local governments, the effects of changes in the marine environment on HABs are described. Since the beginning of HABs monitoring in 1972, they continued to increase from the 1980s to the 1990s. After the largest number of HAB incidents (109) in 1998; the trend declined until the 2010s. Most HABs in the 1970s were caused by diatoms. In the 1980s, coastal dinoflagellates caused HABs; Cochlodinium polykrikoides blooms have been occurring continuously since 1993. There are three HAB species that cause damage to fisheries in Korea. The high-density bloom of Karenia mikimotoi caused mass mortality in shellfish in Jinhae Bay in 1981. Karenia sp. blooms occurring around Tongyeong in 1992 killed aquaculture fish. Since the occurrence of the largest fisheries damage of KRW 76.6 billion in 1995 caused by C. polykrikoides blooms, they have been occurring continuously. The concentration of nutrients in coastal waters was the highest in the 1980s and has declined since the mid-1990s. This reduction in nutrient concentration is a good explanation for the decreasing number of HABs. Since 2016, a summer high water temperature of 30℃ or more has appeared, and the range and scale of C. polykrikoides blooms have been greatly reduced. In 2016, K. mikimotoi blooms occurred around Wando, Jangheung and Goheung and small scale blooms of C. polykrikoides occurred around Yeosu. There were no C. polykrikoides blooms in 2017; however, Alexandrium affine blooms occurred from Yeosu to Tongyeong. There was a small-scale blooms of C. polykrikoides in 2018 compared to those in the previous years. Our results show that reduction in nutrients and the high water temperature owing to climate change are a good explanation for variation in HABs in Korean coastal waters.

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.26 no.4
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• pp.217-224
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• 2014

Cochlodinium polykrikoides is a typical harmful algal species which generates the red-tide in the coastal zone, southern Korea. Accurate algal growth model can be established and then the prediction of the red-tide occurrence using this model is possible if the information on the optimal growth model parameters are available because it is directly related between the red-tide occurrence and the rapid algal bloom. However, the limitation factors on the algal growth, such as light intensity, water temperature, salinity, and nutrient concentrations, are so diverse and also the limitation function types are diverse. Thus, the study on the algal growth model development using the available laboratory data set on the growth rate change due to the limitation factors are relatively very poor in the perspective of the model. In this study, the growth model on the C. polykrikoides are developed and suggested as the optimal model which can be used as the element model in the red-tide or ecological models. The optimal parameter estimation and an error analysis are carried out using the available previous research results and data sets. This model can be used for the difference analysis between the lab. condition and in-situ state because it is an optimal model for the lab. condition. The parameter values and ranges also can be used for the model calibration and validation using the in-situ monitoring environmental and algal bloom data sets.

• Journal of the Korean Society for Marine Environment & Energy
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• v.14 no.1
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• pp.19-31
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• 2011

This study has examined the water quality environment of six areas in the mid-southern coastal waters of Korea in order to find the significance between water quality and algal blooms of the area, based on the last 17 years of data offered by the National Fisheries Research and Development Institute. Water temperature in these areas fluctuated with a three to five year of period, and revealed little yearly variations at the surface layer while slowly decreasing at the bottom layer. On the other hand, salinity tended to increase both the surface and bottom layers. Algal blooms had a tendency to decrease in their outbreaks and causative species, with a peak of the middle of 1990s. C. polykrikoides prevailed in the entire areas, and in particular, almost annually appeared in Goheung coastal area since 1995. C. polykrikoides blooms occurred when a mean water temperature was approximately $26^{\circ}C$, and salinities were between 31.00 and 31.50 but exceptionally 28.68 in Yeosu Coast. However, the concentrations of DIN, DIP, TN, TP, including DO, turned out not to be such significant factors for the outbreaks of C. polykrikoides blooms. Therefore, water temperature was judged as the most controlling factor for the outbreak of C. polykrikoides blooms.

• Proceedings of the Korean Society of Fisheries Technology Conference
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• 2000.05a
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• pp.402-403
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• 2000

적조의 원인생물에는 분류학적으로 다양한 종류가 속하며, 이 중 와편모조류는 대표적이라 할 수 있다 (박 등, 1988). 일부 와편모조류는 생활사 중 휴면포자로 해양퇴적토의 표층에서 일정기간 생존하다가 외부환경이 좋아지면 유영세포로 발아하여 다시 번무를 일으킴으로써 적조의 발생 분포 지역의 확대와 발생빈도를 더욱 증가시킨다 (Steidinger and Haddad, 1981; Hallegraeff, 1993; Ishikawa and Taniguchi, 1994; Nehring, 1995). (중략)