• 한국해양학회지
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• 제8권1호
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• pp.4-8
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• 1973

Recent dynamic computations of zonal flow and analysis of oceanographic data of CSK in winter indicate year-to year variations in the location and dynmic structure of the Subtropic Countercurrent in the western North Pacific. In January 1966, the Subtropical Countercurrent migrated southward to 21$^{\circ}$- 22$^{\circ}$N Lat in association with the subsurface Subtropical Convergence. At the area of 25$^{\circ}$- 26$^{\circ}$N Lat, another surface thermal front was formed along which a stronger eastward flow of approximately 0.4kt is seen. On the section of 142$^{\circ}$E Long in January 1967, eastward flow appears at every interval of 2$^{\circ}$latitude in the northern waters of 20$^{\circ}$N Lat.

• 한국수산과학회지
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• 제23권5호
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• pp.407-415
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• 1990

We studied the spatio-temporal characteristics of the Ullung Warm Lens (UWL) using the historical oceanographic data of the National Fisheries Research and Development Agency of Korea in the East Sea from 1967 to 1983. The UWL is basically a subsurface phenomenin found in 100 to 300m depths, and its existence is not well posed in the distribution of the sea surface temperature. The UWL has a typical size of 100 km diameter, and its center migrates within the region of 150 by 150 km south of the Ullung Island. The UWL is almost a permanent feature, and the probability of its occurence within our study area ($129\~132^{\circ}E,\;36\~38^{\circ}N)\;was\;86\%$.

• 한국항해학회지
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• 제21권4호
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• pp.39-47
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• 1997

We researched the mechanism on th flucturain of Bottom Cold Water in the western channel of Korea Strait, using 13 years(1981~1933) oceanographic data of FRDA. The bottom cold water in the western channel appears more often in summer and fall than in winter and spring, and its year-to-year variation of temperature is very large. Such variation seems to be closely related with the variations of cold waters in the subsurface layer of the southwestern East Sea. According to the longitudinal temperature distribution along the korean southeastern coast, a density difference occurs all the time at the still deepth between the western channel and the southwestern East Sea. Thus, it is inferred that the cold waters would intrude into the western channle form the subsurface layer in the southwestern East Sea as a density-driven current, and it intensity depends upon the density difference.

• 한국해양학회지
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• 제22권2호
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• pp.63-70
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• 1987

기존 해양조사 자료에 의하면 황해 동부는 일반적으로 한국연안을 따라 형성되는 조석전선으로 특징지어 진다. 황해서부에서는 이러한 조석전선이 약하게 나타나는 듯하다. 이러한 현상은 장소에 따라 그 강도가 다른 조석혼합에 기인된다 하겠다. 측정된 밀도구조에 기존 지혈調整모델을 적용한 결과연안의 혼합수는 북향, 외양의 성층수(표층 및 저층)는 남향함이 밝혀졌다. 이들 각 수괴의 수송량은 약 $10^{4}$m$^{3}$/sec로 나타났다.

• 한국항해항만학회:학술대회논문집
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• 한국항해항만학회 2022년도 추계학술대회
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• pp.323-324
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• 2022

본 눈문은 X-밴드 레이더 이미지를 이용한 표층해류 계측 비교 결과를 분석한다. 속초해수욕장에 설치된 선박용 X-밴드 레이더를 이용해 2022년 2월 기간 동안 표층해류 계측을 진행하였다. 국립해양조사원 해양 관측 부이의 자료를 기준으로 하여 계측 데이터 비교 및 분석을 통해 표층해류(유속) 계측 정확도를 입증했다.

• 한국해안·해양공학회논문집
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• 제20권1호
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• pp.110-120
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• 2008

한국 주변해역$(30^{\circ}N{\sim}44^{\circ}N,\;117^{\circ}E{\sim}143^{\circ}E)$에 대한 30초 간격의 격자수심을 산출하였다 자료 생산을 위해 공개된 1분 수심 최신자료와 2007년 간행된 국립해양조사원의 모든 수치해도를 이용하였다. 격자수심의 기준면은 약 최저저조면이며 경위도는 WGS84 좌표계를 사용하였다. 특히 수치해도에서 측심자료를 추출하고 이를 WGS84 좌표로 변환하는 프로그램을 개발하여 자료의 정확성을 꾀하였고 보간법을 이용한 산출된 자료를 기존 자료와 비교 분석하였다. 본 수심자료에서는 기존 격자수심과 달리 보다 상세하고 정확한 지형을 볼 수 있다.

• 한국해양학회지:바다
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• 제26권3호
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• pp.201-219
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• 2021

최근에 기후변화와 같은 전 지구적인 문제에 대한 해양의 역할을 이해하기 위해 다양한 연구자들이 지난 반세기 동안 전 세계 해양에서 수집한 자료를 통합하여 체계적으로 관리하기 위한 노력을 수행하였다. 국내에서도 우리나라 주변 해역에서 해양 환경변화를 지속해서 감시하기 위한 노력을 공공기관, 연구소, 대학에서 수행하고 있다. 이렇게 생산된 다양한 형태의 해양화학 자료들은 기관별 목적에 따라 자체적으로 관리해 왔다. 최근 국가 주도로 다양한 자료를 통합하는 노력을 수행하고 있다. 본 연구에서는 해외 여러 기관에서 생산된 다양한 형태의 자료를 통합하여 체계적으로 관리에 사용된 자료 품질관리 방법에 관해 설명하였다. 본 연구에서는, 이러한 방법을 적용하여 국내 여러 기관에서 생산된 자료의 형식을 통일, 해양학적인 특성에 따라 자료의 일차적인 품질관리, 신뢰할 만한 자료와 비교 또는 표준물질 등을 활용한 이차적인 품질관리를 수행하기 위한 기초정보를 제공하고, 궁극적으로는 국내에서 다양한 목적으로 수집된 자료가 생산자의 숙련도와 상관없이 상호비교 가능한 자료로 통합하는데 기여하고자 한다.

• 한국지구과학회지
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• 제41권4호
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• pp.323-343
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• 2020

Observation data measured at Ieodo Ocean Research Station (IORS) have been utilized in oceanographic and atmospheric studies since 2003. Sea level data observed at the IORS have not been paid attention as compared with many other variables such as aerosol, radiation, turbulent flux, wind, wave, fog, temperature, and salinity. Total sea level rises at the IORS (5.6 mm yr^-1) from both satellite and tide-gauge observations were higher than those in the northeast Asian marginal seas (5.4 mm yr^-1) and the world (4.6 mm yr^-1) from satellite observation from 2009 to 2018. The rates of thermosteric, halosteric, and steric sea level rises were 2.7-4.8, -0.7-2.6, 2.3-7.4 mm yr^-1 from four different calculating methods using observations. The rising rate of the steric sea level was higher than that of the total sea level in the case with additional data quality control. Calculating the non-steric sea level was not found to yield meaningful results, despite the ability to calculate non-steric sea level by simply subtracting the steric sea level from total sea level. This uncertainty did not arise from the data analysis but from a lack of good data, even though tide, temperature, and salinity data were quality controlled two times by Korea Hydrographic and Oceanography Agency. The status of the IORS data suggests that the maintenance management of observation systems, equipment, and data quality control should be improved to facilitate data use from the IORS.

• Fisheries and Aquatic Sciences
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• 제15권4호
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• pp.345-352
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• 2012

To predict catches of Pacific anchovy Engraulis japonicus larvae, anchovy eggs were collected in the coastal waters off Gunsan, Korea, in the Yellow Sea during the main spawning season (June to July) from 2003 to 2009. A ring net was repeatedly towed vertically at 10 stations during the daytime to sample eggs. Catch data estimated by auction sales were obtained from the Fisheries Cooperatives Union of Gunsan City and daily water temperature data in the outer harbor of Gunsan City during the survey periods were obtained from the National Oceanographic Research Institute. A significant relationship was found between anchovy egg density from June to July and larval catch from July to October in the same year. Catch of anchovy larvae in Gunsan were also high when optimal growth temperatures were recorded in the coastal waters off Gunsan in July. Although the recruitment success or failure of anchovy larvae can be predicted from variability in egg density, we suggest that mean daily water temperature is a more efficient indicator for predicting variability in catches of larval anchovy in the Yellow Sea.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume II
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• pp.529-532
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• 2006

The oceanic currents in the South China Sea (SCS) are strongly influenced by monsoon winds. A review on the SCS currents has indicated that previous studies have pointed out an anticyclonic circulation in the area between the southern Vietnam coast and the Spratly Islands. However, its detail is not understood because of less information of in situ observations. The physical-biological interaction is quite new research area, which has been established and promoted by means of the ocean color remote sensing. Temporal/spatial variability of the phytoplankton activities are well captured by ocean color (OC) -derived Chlorophyll-a images. Combining the OC-Chl-a and the other high-resolution satellite data (e.g., SST images), the biological aspects of oceanographic variation is well described. The blooming phenomena in the area between the southern Vietnam coast and the Spratly islands are further investigated. Change in the wind-system related to the El Nino generates upwelling/SST-cooling in the sea south of the Spratly Islands through the air-sea-land interaction was studied. The seasonal upwelling is also associated with the harmful algal bloom (HAB) off two side of Indochina Peninsula have investigated. The seasonal variation of SCS phytoplankton blooming and related oceanic conditions in Vietnam coast was observed. Ocean color satellite data has effective contribute to study the oceanic condition and phytoplankton blooming in South China Sea.