• 한국컴퓨터정보학회논문지
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• 제27권11호
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• pp.47-55
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• 2022

최근 우리나라에서도 인공지능 모델을 이용한 수온예측 관련 연구가 활발히 진행되고 있으나 한반도 주변 해역의 수온을 예측한 대부분의 연구는 주로 해수면 온도 예측에 중점을 두고 진행되었다. 반면 본 연구는 XBT(eXpendable Bathythermograph, 소모성 연직수온측정기) 데이터와 기계 학습 모델(RandomForest, XGBoost, LightGBM)을 사용하여 잠수함 작전 및 대잠전(Anti-Submarine Warfare)에 있어서 군사적으로 중요한 동해의 수직 수온분포를 예측하였다. 동해 특정해역의 해수면부터 수심 200m까지 측정된 XBT 데이터를 이용하여 모델을 학습시키고 절대 평균 오차(MAE, Mean Absolute Error)와 수직 수온분포 그래프를 통해 예측정확도를 평가하였다.

• Ocean and Polar Research
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• 제34권1호
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• pp.37-51
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• 2012

We investigated the distribution and species composition of zooplankton in relation to hydrographical characteristics in the Korea Strait during the winter (February) and summer (July) of 2009. Satellite images of sea surface temperatures and in situ CTD data showed that the southeastern water zone (St3-5) off Jeju Island was strongly influenced by the Tsushima Current during both the winter and summer, whereas the Changjiang Diluted Water, characterized as water with relatively low salinity, was evident in the coastal waters of Jeju Island during the summer. During winter, zooplankton abundance was significantly higher than in the summer, with dominance by copepods, ostracods, siphonophorans, appendicularians, and nauplii. In both seasons, copepods represented >70% of the total zooplankton population. Calanus sinicus, a large calanoid copepod, was dominant in near the coast, and that may be associated with the intrusion of low salinity water (i.e., the Changjiang Diluted Water) along the coast. The abundance of P. parvus s.l. and A. omorii, known as neritic copepods, was mainly associated with the Korea Southern Coastal Water. Foraminiferans, Ostracods, O. plumifera, and P. aculeatus were concentrated in the southeastern water off Jeju Island during both seasons; showing their association with the Tsushima Current, which is characterized warm, high salinity water. Our results suggest that the distribution, abundance, and species composition of zooplankton are highly influenced by different water masses in the Korea Strait.

• 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.

• 한국항해항만학회:학술대회논문집
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• 한국항해항만학회 2004년도 춘계학술대회 논문집
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• pp.255-261
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• 2004

본 논문에서는 진해만에서 수질환경에 대한 현장관측조사를 통하여 진해만 수질현황에 대한 해수유동 시뮬레이션을 실시하여 대상해역의 유통특성을 파악하고, 계산된 유통data를 이용하여 해양오염시뮬레이션을 행하였으며 해수유동시뮬레이션 결과를 해양조사원에서 실시한 조석 및 조류관측 자료를 이용하여 시뮬레이션 결과를 검증하였으며, 유통결과를 해양오염 시뮬레이션의 유통 입력 자료로 이용하였다. 해수유통 Data 및 해양관측 Data를 이용하여 수질확산시뮬레이션을 행하여 실측데이터와 비교분석하여 COD농도 분포를 계산하여서 진해만의 수질특성을 파악하고자 하였다.

• Elastomers and Composites
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• 제46권2호
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• pp.158-163
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• 2011

해수 하에서 경시 변화에 따른 경질 폴리우레탄 폼(PUF)의 물성 변화를 알아보기 위해 방향족 폴리에스테르 폴리올, 지방족 폴리에스테르 폴리올과 지방족 폴리에테르 폴리올 함량에 따라 경질 폴리우레탄 폼을 합성하였다. 해수 하에서 PUF의 물성변화를 고찰하기 위해 만능시험기, 시차 주사 열량계, 경도 측정기, 적외선 분광계를 이용하였다. 방향족 폴리에스테르 폴리올의 함량이 증가함에 따라 해수 하에서 경시 변화에 따라 PUF의 압축강도와 경도의 감소폭은 증가하였다. 해수 하에서 PUF의 유리전이온도는 증가하였는데 적외선 스펙트럼 분석 결과 우레탄과 우레아의 피크는 감소하고, 알로파네이트와 바이우렛의 피크는 증가한 것을 알 수 있었다. 해수 하에서 PUF는 가교도가 증가하여 폼이 brittle하게 형성됨에 따라 유리전이온도가 증가하였지만 가수 분해로 인하여 기계적 물성이 저하된 것으로 사료 된다.

• 한국수산과학회지
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• 제8권4호
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• pp.208-212
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• 1975

The study was conducted to determine the optimum conditions for keeping quality of shucked sea mussel, Mytilus edulis, during marketing under commercial handling. As quality factors, water holding capacity, pH, VBN and TMA content were measured. Water holding capacity was obviously affected by salt content of the sea mussel meat. Water was released at the salinity above $2.8\%$ and absorbed below the value. In case of distilled water added instead salt solution, $23.3\%$ weight was gained. Absorbing or releasing water of sea mussel meat was also influenced by temperature showing either water gain or loss was greater at, $3^{\circ}C\;than\;25^{\circ}C$. Osmotic quilibrium by salt between meat and liquor was held within 4 hours. The pH value of fresh sea mussle marked 6.0 which is somewhat lower when compared with that of other shellfishes, and it gradually decreased to 5.0 during storage. VBN contents of fresh muscle and shell liquor were $2.1mg\%$ and $1mg\%$ respectively. The sour odour began to be detectable with $5.0mg\%$ of VBN content. TMA in the sea mussel was not detected.

• 대한원격탐사학회지
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• 제20권3호
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• pp.153-162
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• 2004

In the summer of 1998-2001, a huge flood occurred in the Yangtze River in the eastern China. Low salinity water less than 28 psu from the river was detected around the southwestern part of the Jeju Island, which is located in the southern part of the Korean Peninsula. We studied how to detect low salinity water from the Yangtze River, that cause a terrible damage to the Korean fisheries. We established a relationships between low salinity at surface, turbid water from the Yangtze River and digital ocean color remotely sensed data of SeaWiFS sensor in the northern East China Sea, in the summer of 1998, 1999, 2000 and 2001. The salinity charts of the northern East China Sea were created by regeneration of the satellite ocean color data using the empirical formula from the relationships between in situ low salinity, in situ measured turbid water with transparency and SeaWiFS ocean color data (normalized water leaving radiance of 490 nm/555 nm).

• 한국해안해양공학회지
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• 제18권4호
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• pp.301-307
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• 2006

서해안과 같이 큰 조차를 가진 연안해역에서 항만건설과 매립사업이 널리 진행되고 있으며, 대부분의 사업은 방조제 건설을 필요로 한다. 대부분의 방조제는 내부와 외부사이에 해수가 교환되지 않으나, 사석만을 사용해서 축조된 방파제와 가호안의 투수성 제방에서는 해수가 교환된다. 내부의 수면은 외부 조위의 변화에 따라 시간에 따라 변화하나 그 조차는 해수교환시 제방에서의 큰 마찰로 인하여 외부보다는 작다. 지금까지의 연구에서는 제방을 통한 해수교환을 무시하는 것이 조석모델링에서 일반적이다. 이는 내부의 해수면 변화를 계산할 수 없을 뿐 아니라 물막이 공사와 같이 일부 개방구간이 존재하는 경우에 개방구간만을 통한 해수교환량만을 고려하고, 제체를 통한 해수교환량을 무시하여 내부의 조위와 실제 해수교환량을 부정확하게 계산한다. 본 연구에서는 지하수이론을 이용하여 해수유동모의시 투수성 제체를 통한 해수교환량을 정확히 고려할 수 있도록 하였다.

• 물과 미래
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• 제17권2호
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• pp.72-79
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• 1984

This investagation was carried out by analyzing water types and measuring the environmetal isotopes (tritium and deuterium) for development of water resources and protection of ground waters from sea water intrusion. The water sample were taken monthly from April to June, 1983 from sixteen sites in the Cheju metropolitan area; three sea, three spring, and ten ground waters. The ground water in the midwest area of the city contained 20 TU of tritium and-46 per mille of deuterium, classified as the $NaHCO_3$ type of ground water, generally deep seated. The spring water and ground water in the southern part of the city contained 15 to of tritium and-39 per mile of deuterium, and appeared to the $CaHCO_3$ type of shallow ground water, easily affected 표 precipitation. The results of tritium and deuterium analyses showed that the ground water in the coastal area were not affected by sea water intrusion, although they changed from $NaHCO_3$ or $CaHCO_3$ type to NaCl type in May and June. It is concluded that the high Na and Cl content in those ground waters might come from municipal sewage. The sea water in the Yong-duam area was influenced by sping water.

• 한국해양학회지
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• 제17권2호
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• pp.74-82
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• 1982

1968-1980年의 韓.日共同海洋調査點中 韓國側 63個定點의 海洋調査資料를 使用하여 月別 水溫 및 분의 變動係數를 分析 硏究한 缺課의 要約은 다음과 같다. 變動係數는 水溫과 분의 前線域이나 혹은 躍層形成海域에서 크게 나타났다. 水溫의 變動係數는 각 水塊의 勞力이 가장 强한 時期에 最大値를 나타냈다(對馬 暖流와 黃海暖流域의 夏季 中層에서, 南海岸沿岸水 및 西海南部域의 冬季의 全層 에서 最大). 鹽分의 變動係數는 東支那海 低鹽水의 影響을 많이 받는 夏季에 暖流系水의 表層水에서 크게 나타나며, 沿岸水 및 西海南部域에서는 暖流系水値의 1/2정도였다.