• 대한한의학원전학회지
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• 제33권2호
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• pp.91-108
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• 2020

Objectives : To study the shu points selection of the Four Seas in the 「Hailun」 chapter of 『Lingshu』. Methods : The effects and main indications of each shu point, their anatomical position, characteristics along with similarities of disease patterns according to excessiveness and deficiency of the Four Seas were examined. Results : The selection of shu points of the Four Seas were deeply related to the effects and main indications, and the common similarity among conditions due to excessiveness and deficiency was the presence of psychological aspects. Also, when the Four Seas are connected to the Jing-Qi-Shen and Blood, marrow sea[髓海] is connected to Jing & Shen, qi sea[氣海] is connected to Qi, blood sea[血海] is connected to Blood, and sea of water and grain[水穀之海] replenishes Jing-Qi-Shen and Blood. When connected to the Four Qi Intersections, the marrow sea is connected to 'head qi with intersection', qi sea is connected to 'chest qi with intersection', sea of water and grain or blood sea is connected to 'stomach qi with intersection', otherwise sea of water and grain is connected to 'shin qi with intersection'. Conclusions : The Four Seas are designated to the shu points due to their accumulation of Qi when the main elements of Jing-Qi-Shen and Blood are deficient or excessive, allowing for the most convenient management and manipulation of the condition of these main elements. In clinical practice, the shu points of the Four Seas will likely increase treatment efficacy for conditions that include psychological aspects.

• 대한지리학회지
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• 제48권6호
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• pp.914-928
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• 2013

바다를 이용한 항로의 발달과 바다를 터전으로 하는 어업활동의 증가에 따라 안전한 항해를 위한 바다의 경계와 그 공간을 지칭하는 지명의 제정은 필수적이다. 바다의 경계를 획정하는데 있어 국내 외적인 기준이 존재하지는 않지만, 국제수로기구에서 출판한 "해양과 바다의 경계; S-23"에 대한 보고서는 공식적인 문서로써 바다의 경계에 대한 기준을 제시해 줄 수 있다. 이에 본 연구는 S-23 보고서를 기초로 하여 바다경계 변화에 대해 살펴보고, 2002년 제4판 draft를 분석하여 바다의 속성지명 및 바다경계를 획정하는데 사용된 자연지리적 대상을 찾아 경계획정의 근거를 분석하는데 목적이 있다. 분석 결과 S-23(2002)에 나타난 바다는 9개의 속성지명, 즉 Ocean, Sea, Channel, Passage, Strait, Sound, Gulf, Bay, Bight로 분류되었다. 각각의 속성지명은 계층관계를 보이며 하부 계층의 바다는 배타적 또는 포함관계로 표현되었다. IHO의 용어사전에서 정의하는 속성지명의 특성과 현실에서의 바다특성이 상이하게 사용된 예도 발견되었다. 바다의 경계획정기준은 조약에서 제시한 경 위도, 대륙의 최외곽에 있는 곶 또는 갑, 하천하구와 사주 등으로 나타났다. 해저지형의 경우 대륙붕, 해구, 해곡, 해저융기부, 해저퇴, 암초가 경계로 이용되었는데, 특히 남극과 북극지역의 바다 경계는 대륙붕 또는 해저융기부의 경계가 이용되는 사례가 많았다. 해저지형에 의한 경계획정은 S-23 1953년 3판까지 제시된 것과는 달리 2002년 초안에서 주로 발견되는데, 이는 해저탐사기술이 발달하면서 해저지형에 대한 이해가 개선되고, 이러한 지식이 해양경계획정에 사용된 것으로 유추해볼 수 있다.

• 대한조선학회지
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• 제26권1호
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• pp.1-10
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• 1989

본 연구에서는 추파중에 항행하는 선박의 전복현상과 관련된 횡복원성 문제를 다루었다. 추파중에서 항행하는 선박의 복원력 변동량을 이론적으로 규명하기 위해서 Froude-Krylov 가설과 파랑중에서의 정적 평형조건 등을 이용한 이론계산법을 정식화하였다. 그리고 본 이론계산법에 따라서 고속화물선 선형과 어선 선형에 대해서 복원력 변동량을 계산하였으며, 동일한 파랑조건하에서 실시된 Hamamoto의 모형실험 결과와 비교하였다. 상기 이론계산 결과 및 모형실험 결과로부터 추파의 파정에서 선체중심이 위치하였을 때 복원력이 평수중에 비해서 절반이하로 감소되며, 이때 전복의 위험이 있다는 것을 확인할 수 있었다.

• 대한조선학회지
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• 제21권3호
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• pp.27-34
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• 1984

When a ship is travelling in following seas, the encounter frequency is reduced to be very low. In that case broaching phenomenon is most likely to occur, and it may be due to wave exciting forces acting on ships. It is thought that the wave exciting forces acting on ships in following seas almost consist of two components. One is hydrostatic force due to Froude-Krylov hypothesis, and the other is hydrodynamic lift force due to orbital motion of water particles below the wave surface. In the present paper, the emphasis is laid upon wave exciting sway force, yaw moment and roll moment acting on ships in following seas. The authers take the case that the component of ship speed in the direction of wave propagation is equal to the wave celerity, i.e., the encounter frequency is zero. Hydrostatic force components are calculated by line integral method on Lewis form plane, and hydrodynamic lift components are calculated by lifting surface theory. Furthermore captive model tests are carried out in regular following waves generated by means of a wave making board. Through the comparison between calculated and measured values, it is confirmed that the wave exciting forces acting on ships in following seas can be predicted in terms of present method to a certain extent.

• International Journal of Naval Architecture and Ocean Engineering
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• 제3권1호
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• pp.9-19
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• 2011

The paper describes the validation of two time domain methods to simulate the behaviour of a destroyer operating in steep, stern-quartering seas. The significance of deck-edge immersion and water on deck on the capsize risk is shown as well as the necessity to account for the wave disturbances caused by the ship. A method is described to reconstruct experimental wave trains and finally two deterministic validation cases are shown.

• 한국항해학회지
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• 제11권2호
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• pp.61-72
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• 1987

When a ship is running in following seas, the encounter frequency is reduced to a very low one. In that case broaching, surfiding and capsizing phenomena are most likely to occur due to wave exciting forces acting on a ship in following seas. In this paper, the emphasis is mainly laid upon transverse stability of ships following seas, which is related to capszing phenomenon. The authors take the case that ship speed is equal to the wave celerity, i.e., the encounter frequency is zero. Hydrostatic force and moment due to Froude-Krylov hypothesis are calculated by line intergral method. Transverse stability is evaluated from hydrostatic force and moment. Through the application of present calculation method to box-shaped vessel, it is confirmed that the transversestability of a vessel can be reduced to critical level at wave crest.

• 한국항해학회지
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• 제23권2호
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• pp.23-27
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• 1999

When a ship is running in following and quartering seas and on a crest with the ship′s length being nearly the same as the wave length, ship′s stability will be lost most; "T" shape crests with highly concentrated energy will appear during the process of transformation from irregular waves to regular ones, and the ship may be under continuous impact of large waves for a long period of time; Synchronism will also appear when the ship′s natural period of rolling and period of encounter are close to each other. For safe navigation, proper stability should be well ensured, proper speed and course chosen with speed under 1.8L1/2 kn (L is the ship′s length), initial listing avoided, special attention paid to steering.

• Ocean and Polar Research
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• 제42권3호
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• pp.211-223
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• 2020

With the increasing demand for improved marine environments and safety, greater ability to minimize damages to coastal areas from harmful organisms, ship accidents, oil spills, etc. is required. In this regard, an accurate assessment and understanding of current systems is a crucial step to improve forecasting ability. In this study, we examine spatial and temporal characteristics of current systems in the adjacent seas of Jeju Island using a high-resolution regional ocean circulation model. Our model successfully captures the features of tides and tidal currents observed around Jeju Island. The tide form number calculated from the model result ranges between 0.3 and 0.45 in the adjacent seas of Jeju Island, indicating that the dominant type of tides is a combination of diurnal and semidiurnal, but predominantly semidiurnal. The spatial pattern of tidal current ellipses show that the tidal currents oscillate in a northwest-southeast direction and the rotating direction is clockwise in the adjacent seas of Jeju Island and counterclockwise in the Jeju Strait. Compared to the mean kinetic energy, the contribution of tidal current energy prevails the most parts of the region, but largely decreases in the eastern seas of Jeju Island where the Tsushima Warm Current is dominant. In addition, a Lagrangian particle-tracking experiment conducted suggests that particle trajectories in tidal currents flowing along the coast may differ substantially from the mean current direction. Thus, improving our understanding of tidal currents is essential to forecast the transport of marine pollution and harmful organisms in the adjacent seas of Jeju Island.

• 한국항해항만학회지
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• 제41권3호
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• pp.103-108
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• 2017

이 연구에서는 최근 5년(2010~2014년) 동안의 데이터를 이용하여 우리나라의 풍랑특보 분포 특성에 대하여 분석하였다. 풍랑특보는 우리나라 주변 해역을 항해하는 선박 및 해양 구조물 등의 안전에 큰 영향을 미치므로 중요한 의미를 가진다. 풍랑특보는 한반도의 동측 즉, 동해남부 및 동해중부 해역, 남해동부 해역에서 많이 나타난다. 이 결과는 온대저기압의 이동과 발달, 계절풍의 세기 등과 밀접히 관련되어 있다. 그리고 풍랑특보는 12월에 가장 많고, 1월과 3~4월에도 높은 빈도수를 보인다. 계절로 구분해 보면, 겨울 > 봄 > 가을 > 여름의 관계를 확인할 수 있는데, 이들 결과는 온대저기압의 발생 및 발달, 계절풍의 세기 차이 등에 의한 것이다. 앞바다와 먼바다의 월별 풍랑특보 분포에 대하여 통계 분석한 결과, 양자는 강한 양의 상관관계가 있음을 확인하였다.

• 한국지구과학회지
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• 제39권1호
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• pp.1-22
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• 2018

Eight different data sets are examined in order to gain insight into the surface heat flux traits of the East Asian marginal seas. In the case of solar radiation of the East Sea (Japan Sea), Coordinated Ocean-ice Reference Experiments ver. 2 (CORE2) and the Objectively Analyzed Air-Sea Fluxes (OAFlux) are similar to the observed data at meteorological stations. A combination is sought by averaging these as well as the Climate Forecast System Reanalysis (CFSR) and the National Centers for Environmental Prediction (NCEP)-1 data to acquire more accurate surface heat flux for the East Asian marginal seas. According to the Combination Data, the annual averages of net heat flux of the East Sea, Yellow Sea, and East China Sea are -61.84, -22.42, and $-97.54Wm^{-2}$, respectively. The Kuroshio area to the south of Japan and the southern East Sea were found to have the largest upward annual mean net heat flux during winter, at -460- -300 and at $-370--300Wm^{-2}$, respectively. The long-term fluctuation (1984-2004) of the net heat flux shows a trend of increasing transport of heat from the ocean into the atmosphere throughout the study area.