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홍철훈,최용규,HONG Chul-hoon,CHOI Yong-Kyu The Korean Society of Fisheries and Aquatic Scienc 1997 한국수산과학회지 Vol.30 No.4
[ $M_2$ ] 조에 의해 구동되는 원시방정시을 이용한 수치모델이 득량만에서 수온장 및 유속장에 미치는 조석의 효과를 조사하기 위해 이용된다. 모델결과는 관측된 수온장의 여러 가지 특징을 재현하였다. 즉 등온선이 만내의 연안선과 평행한 점, 냉수가 만의 우측에 나타나는 점 등이었다. 특히 실험결과로 볼 때 수평 수온장 및 유속장은 해저지형효과를 크게 받고 있으며 만내의 표층냉수는 고저시의 유입되는 흐름에 수반된다. 경압성을 조사하기 위한 부가적인 수치실험결과는 유속장내의 경압성이 매우 약함을 보여준다. 그러나 실험결과는 관측에서 보여준 밀도성층구조를 재현하지 못했다. 이를 재현하기 위해서는 $M_2$ 조 이외에 $S_2,\;O_2$ 또는 $K_2$ 조를 외력에 포함시켜야 할 것으로 예상된다. A primitive equation numerical model driven only by $M_2$ tide is used to examine role of tide in the temperature and velocity fields of Deukryang Bay. The numerical model reproduces several features of the observational temperature fields such that the isotherms tend to be parallel to the coast in the bay, and the colder water exists at the right hand side in the bay. The horizontal temperature and velocity fields in the model are dominantly influenced by bottom topography. The model also shows that the surface colder water in the bay is accompanied by strong-alongshore current during the flood tide. An investigation for baroclinicity in the bay by additional numerical experiment indicates that the baroclinirity in velocity field is very weak. The model, however, did not reproduce a stratification in the observation, implying that the model needs to add other semi-diurnal components such as $S_2,\;O_2\;or\;K_2$ tides to $M_2$ tide.
3차원 원시모델을 이용한 태풍통과시 일본 북부 연안역에서 발생한 연안용승 연구
홍철훈,HONG Chul-Hoon 한국수산과학회 2003 한국수산과학회지 Vol.36 No.6
A three-dimensional numerical model (POM) is implemented to examine coastal upwelling in the northern Japanese coastal region with the passage of Typhoon Oliwa in September 1997. Observed sea surface temperature (SST) decreased suddenly ranging from $-6\;to\;-7^{\circ}C$ in the coastal regions, and such a SST decrease state lasted for more than ten days after the typhoon passed. The model successfully reproduces the observation and gives a clear explanation, the sudden decrease of SST occurred in the process of coastal upwelling with Ekman dynamics. The model also describes the sea surface cooling in the open ocean with vertical velocity.
박성은,조규대,홍철훈,김동선,조광우,PARK Sung-Eun,CHO Kyu-Dae,HONG Chul-Hoon,KIM Dong-Sun,CHO Kwang-Woo 한국수산과학회 1999 한국수산과학회지 Vol.32 No.5
The effect of wind on the circulation in Kamak Bay in the southern sea of Korea was examined using a numerical shallow water model. The experiments were primarily focused on how the effect of wind influence the tidal residual current. According to wind directions, the residual currents were changed; the westerly wind created a strong anti-clockwise eddy in the northwestern area of the bay where the flow field is usually very weak; the easterly wind strengthened the flow field in the central area of the bay; the patterns of flow fields to the north and south winds were almost the same as one without the wind, although the flow field became slightly stronger, The model flirty reproduced features in the observed current field at Pyongsa.
우리나라 전문계열 고등학교 교과서의 해양관련 내용 분석
김삼곤(Sam-Kon KIM),홍철훈(Chul-Hoon HONG),차철표(Cheol-Pyo CHA) 한국수산해양교육학회 2008 水産海洋敎育硏究 Vol.20 No.2
The study analyzed 343 government-authorized and officially approved textbooks of the Seventh Curriculum's specialized subjects in high school from March to September, 2007. The textbooks were categorized into the area of agriculture, industry, commerce, household and business, science, foreign languages and physical exercise and analyzed in terms of the target and content areas of marine education. And the findings were as follows: First, among the textbooks in the seven groups serving as the focus of this study, 19.8% have oceanic-related information but pages including ocean contents occupy only 0.8%. Consequently ocean-related contents are scarcely included. The ocean-related contents are necessary to be treated goals. Second, the goals of school oceanic education are focused in vocational subjects. In order of commonality, information & knowledge are most frequent, then functionality, followed by activity & participation. There was no education provided focusing on value & attitude. Given that school oceanic educations were selected for promoting the importance of the ocean and highlighting the problems of the ocean, the lack of information & knowledge is of concern. The goals of oceanic education should be augmented to actively and positively participate in the solutions of the problems with knowledge, ocean-friendly value & attitude, and increased activity & participation. Third, the contents of school oceanic education commonly focuses on the relationships of oceans and humans, oceans and ecology, and artificial oceanic environments and facilities. Less common but still introduced are ocean resources, sea pollution, sea preservation and measures. Yet, in contrast there is a lack of education in the ethics of sea preservation.
최용규,양성기,홍철훈,조규대 한국환경과학회 1994 한국환경과학회지 Vol.3 No.4
Based on the Results of Marine Meteorological and Oceanographical Observations (1966∼1987), oceanographic conditions of the Japan Sea in winter was studied in relation to the Japan Sea Proper Water (JSPW). The mean and dispersion of the deep water above 1000m depth are O.26±0.2℃ in temperature and 5.1±0.25 ㎖/ℓ in oxygen. The mean and dispersion of the bottom water below 1000m depth are 0.07±0.04℃ in temperature and 5.1±0.15㎖/ℓ in oxygen. The distributions of the temperature and dissolved oxygen in the deep water above 1000m depth are ranged wider than those of the bottom water below 1000m depth in T-S and T-O_2 diagrams. The bottom water are showed more homogeneous and smaller variations than the deep water in the characteristics of water mass. The deep water above 1000m depth is active in contact with the atmosphere. The JSPW similar to the above characteristics is showed in the open ocean of the north of 40°30' N, west of 138°E. Therefore, the deep water is formed probably by the open-ocean convection.
동해고유수의 생성가능해역 : I.극전선에 의한 해역구분 I.Subareas by the Polar Front
최용규,양성기,조규대,이재철,홍철훈 한국환경과학회 1993 한국환경과학회지 Vol.2 No.1
Based on the Results of Marine Meteorological and Oceanographical Observations during 1966∼1987 and the Ten-day Marine Report during 1970∼1989 by Japan Meteorological Agency, the possible area where the Japan Sea Proper Water (JSPW) can be formed is investigated by analyzing the distribution of water types in the Japan Sea. The Japan Sea can be divided into three subareas of Northern Cold Water(NCW), Polar Front(PF) and Tsushima Warm Current (TWC) by the Polar Front identified by a 6℃ isothermal line at the sea surface in winter. Mean position of the Polar Front is approximately parallel to the latitude 39∼40°N. The standard deviation of the Polar Front from the mean position of about 130㎞ width is the smallest in the region between 136°E and 138°E where the Polar Front is very stable, because the branches of the Tsushima Current are converging in this region. However, standard deviations are about 180∼250㎞ near the Korean peninsula and the Tsugaru Strait due to greater variability of warm currents. In the NCW area north of 40°30'N and west of 138°E, the water types of the sea surface to the 100m depth are similar to those of the JSPW. This fact indicates that the surface layer of the NCW area is the possible region of the JSPW formation in winter.