• 한국해양공학회:학술대회논문집
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• 한국해양공학회 2004년도 학술대회지
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• pp.279-284
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• 2004

Red tide(harmful algae) in the Korean Coastal Waters has a given a great damage to the fishery every year. However, the aim of our study understands the influence of meteorological factors (air and water tempaerature, precipitation, sunshine, solar radiation, winds) relating to the mechanism of red tide occurrence and monitors red tide by satellite remote sensing, and analyzes the potential area for red tide occurrence by GIS. The meteorological factors have directly influenced on red tide formation. Thus, We want to predict and apply to red tide formation from statistical analyses on the relationships between red tide formation and meteorological factors. In future, it should be realized the near real time monitoring for red tide by the development of remote sensing technique and the construction of integrated model by the red tide information management system (the data base of red tide - meteorological informations).

• 한국정보통신학회논문지
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• 제15권9호
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• pp.1881-1888
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• 2011

적조란 유해조류의 일시적인 대 번식인 자연현상으로 어패류를 집단 폐사 시킨다. 적조에 의한 양식어업의 피해는 매년 발생하고 있다. 이 때문에 적조 발생을 미리 예측할 수 있으면 적조에 대한 피해를 최소화 시킬 수 있다. 적조발생 예측시 나이브베이스 분류자를 이용하면 좋은 예측결과를 얻을 수 있다. 그러나 나이브베이스를 이용한 결과는 단순한 발생 여부 만을 판별 할뿐 발생하는 적조가 어느 정도 증가 할지는 알 수 없다. 본 논문은 퍼지 추론과 나이브베이스 분류자를 이용한 새로운 적조발생 예측 방법을 제안한다. 제안방법은 적조 발생 예측의 정확률을 향상시키면서 적조생물 밀도의 증가율을 예측할 수 있다.

• Spatial Information Research
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• 제12권3호
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• pp.263-274
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• 2004

본 연구의 목적은 GIS 분석기법에 의해 적조의 발생시기와 생물학적, 해양학적인 인자를 통해 적조의 발생 가능한 시-공간적인 분포를 분석하는 적조정보시스템의 개발이다. 적조의 발생은 1994년까지 남해안에서 산발적으로 일어났다. 그러나 1995년 이후로 남해안과 동해안 전 해역에 걸쳐서 빈번히 광역적인 범위로 적조가 발생하고 있다. 따라서 적조 연구 분야도 최근 중요한 변화가 이루어졌다. 적조 모니터링을 위한 원격탐사, GIS, 퍼지 모델 시스템 등과 같은 다양한 기술 분야가 수행되었다. 본 연구에서는 국내 연안에서 발생한 적조의 발생 범위와 적조 생물, 그리고 해양환경 요소 등을 하나의 지리정보시스템 기반에 의한 적조정보시스템으로 구축하기 위해 각각의 자료를 데이터베이스화하고 적조발생의 공간적 분포를 분석하는데 필요한 자료의 구축 방안을 제시하였다.

• 수산해양기술연구
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• 제57권1호
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• pp.45-56
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• 2021

In order to understand the tide and current around the sea route of Jinhae and Masan passages, tide measurement and 2D numerical model experiments of tidal current and residual flow were carried out. Tide is composed of 84% of semi-diurnal tide, 11% of diurnal tide and 4% of shallow water tide, respectively. Phase lags of the major components for the tide around the study area have little differences. The flows are reversing on the whole, but have rotational form around Jamdo Island, south of Masan passage in spring tide and Ungdo Island, north of Masan passage in middle and neap tide. Current flows the speed of 50 cm/s in the sea areas near small islands, 5 cm/s in Jinhae harbor, Hangam bay and near Jinhae industrial complex and 20-30 cm/s in Jinhae passage, Budo channel and Masan passage. Tide-induced topographical eddies are formed near small islands, but few eddies exist and the flow rate of less than 5 cm/s tidal residual current formed in Jinhae and Masan passages. The flows in Jinhae and Masan passage give a good condition for a passage into Jinhae and Masan harbor.

• 수산해양기술연구
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• 제41권2호
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• pp.140-146
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• 2005

The aim of our study understands the influence of meteorological factors relating to the formation of the red tide, and monitors the red tide by satellite remote sensing. The meteorological factors have directly influenced on red tide formation. Thus, it was possible to predict and apply to red tide formation from statistical analyses on the realtionships between red tide formation and meteorological factors, and also to realize the near real time monitoring for red tide by satellite remote sensing.

• 대한전자공학회논문지SP
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• 제48권5호
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• pp.39-45
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• 2011

적조에 의한 양식어업의 피해가 증가함에 따라서 적조에 대한 많은 연구가 이루어지고 있다. 현재 적조에 대한 대부분의 연구는 화학적 특성이나 생물학적 원인 규명에 초점이 맞춰 연구되고 있다. 적조 발생을 미리 예측할 수 있으면 적조에 대한 피해를 최소화 시킬 수 있다. 그러나 국내의 적조 현상 예측에 대한 연구는 단순히 적조발생 판별에 그치는 등 미흡한 실정에 있다. 본 논문은 신경망과 SVM을 이용한 새로운 적조발생 예측 방법을 제안한다.

• Ocean and Polar Research
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• 제30권1호
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• pp.1-10
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• 2008

In order to find the effect of intertidal sediments on nutrient cycle in coastal environment, we measured ammonia, nitrate, phosphate, and silicate concentrations every hour during at least 12 hours in the entrance of Keunso Bay during four seasons. The content of ammonia and silicate do not change considerably with season, but nitrate shows large seasonal variation. In summer, nitrate concentration was much lower than in other seasons, which resulted from large biological uptake and active denitrification in intertidal sediments during summer. Phosphate also exhibit seasonal variations, but not that large like nitrate. N/P and N/Si ratios were lower in summer than in other seasons, which was due to active denitrification in the intertidal sediments during summer. For all seasons, ammonia concentrations were higher at low tide than at high tide, but nitrate concentrations were higher at high tide. Dissolved inorganic nitrogen concentrations measured in spring, summer, and winter were higher at high tide than at low tide, but in fall, they were higher at low tide than at high tide. For spring and winter, phosphate and silicate concentrations were higher at low tide than at high tide, while in summer and fall, they were higher at high tide than at low tide. In Keunso Bay, intertidal sediments affect significantly the nutrient cycle around the coastal areas. The intertidal sediments act as a source for ammonia and silicate, but as a sink for nitrate. However, phosphate is not considerably influenced by intertidal sediments.

• 수산해양기술연구
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• 제30권3호
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• pp.142-149
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• 1994

In order to investigate the environmental properties of set net grounds located in the coastal waters of Yeosu. The current in the vicinity of set net grounds was observed by drogue and current meter in 1990 and 1992. The results obtained are summarized as follows: The direction of tidal current at the north enterance of Yeosu bay was southerly in ebb and northwesterly in flood without the distiction of the neap tide and the spring tide. In spring tide the maximum Velocity of the tidal current was 68 cm/sec in ebb and 66 cm/sec in flood. In neap tide the maximum velocity of the tidal current was 37 cm/sec in ebb and 35 cm/sec in flood. And so the direction of residual current was the south ward mainly and 21 cm/sec. The direction of tidal current at set net fishing grounds was southwesterly in ebb and westerly or northwesterly in flood. Regardless of the distinction of neap and spring. The maximum velocity of the current in spring tide was 50 cm/sec in ebb and 40 cm/sec in flood and that in neap was 28 cm/sec in ebb and 25 cm/sec in flood. In spring tide the speed vector along the major axis of semidiurnal tide component was three times as large as diurnal tide. In neap tide, however, the speed vector was about 50% less then that in spring tide, and the semidiurnal tide and diurnal tide were equal in the size of current ellipse and the direction of major axis. The sea area had a southwesterly residual current. 11 cm/sec in spring tide and 7 cm/sec in neap tide. According to the result of drogue tracking, the vicinity of set net fishing ground had a southerly residual current which formed in Yeosu Bay and a weak westerly residual current toward Dolsando from Namhedo. Therefore, set net fishing ground in coastal water of Yeosu was distributed in boundary of inner water which formed from Seamjin river and offshore water supplied from the vicinity of Sorido and Yochido.

• 대한공간정보학회지
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• 제15권2호통권40호
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• pp.51-57
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• 2007

기존 유해성 적조의 발생해역에 대한 공간결정 연구는 미비하였으며, 적조발생지와 소멸지에 대한 공간을 정확하게 판단하기 어려웠다. 따라서 좀 더 객관적이며, 과학적인 방법으로서 적조의 발생과 이동에 따른 시 공간적인 방법으로의 분석 필요성이 대두 되고 있다. 본 연구에서는 매년 발생되는 유해성 적조 발생지에 대한 공간을 파악하기위해 수치지형도를 이용한 GSIS기법을 적용 해안선을 추출하였으며, 수년간 발생된 적조발생 자료를 근거로 발생지의 공간위치를 결정하여 분석한 결과 연구지 중 여자만 일대에서는 적조의 발생이 거의 없었음을 알 수 있었고 남해 돌산도와 남해도 앵강만 해역일대에서 최고의 발생빈도를 나타냄을 알 수 있었다. 이를 근거로 매년 반복적으로 발생되는 해역에 대한 적조의 분포상황을 시공간적으로 판단하여 이동경로 해역의 예측과 피해의 사전예방이 가능하리라 판단된다.

• 수산해양기술연구
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• 제47권4호
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• pp.338-343
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• 2011

To obtain the effective sampling estuarine fauna by a passive net in the West Sea of Korea occurring strong tide, catch were collected by bag nets with various sampling trials off Ganghwa Island in November 2009. We compared the difference of community structures (on spring tide vs. neap tide, total sample vs. subsample and 4 nets vs. 1 net) with each species composition as a sampling unit by the Pearson chi-square test. Number of individual at the spring tide was more abundant than that at the neap tide (p<0.0001) although number of species at the spring tide was not significantly different with that at the neap tide (p=0.174). Both number of species (p=0.138) and number of individual (p=0.096) were not significantly different between total sample and random subsample. Number of species was not significantly different between the subsample by 1 net and the subsample by 4 nets (p=0.515), but number of individual was a little different on both samples (p=0.024). In conclusion, we suggest the subsample by 1 net at spring tide as the effective sampling estuarine fauna by a passive net in the West Sea occurring strong tide.