• 한국컴퓨터정보학회논문지
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• 제24권4호
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• pp.57-63
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• 2019

In this paper, we propose a new framework to control VR(Virtual reality) contents in real time using user's mouth-wind and acceleration sensor of mobile device. In VR, user interaction technology is important, but various user interface methods is still lacking. Most of the interaction technologies are hand touch screen touch or motion recognition. We propose a new interface technology that can interact with VR contents in real time using user's mouth-wind method with acceleration sensor. The direction of the mouth-wind is determined using the angle and position between the user and the mobile device, and the control position is adjusted using the acceleration sensor of the mobile device. Noise included in the size of the mouth wind is refined using a simple average filter. In order to demonstrate the superiority of the proposed technology, we show the result of interacting with contents in game and simulation in real time by applying control position and mouth-wind external force to the game.

• 한국컴퓨터그래픽스학회논문지
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• 제24권4호
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• pp.21-27
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• 2018

본 논문은 모바일 디바이스에서 사용자의 입 바람을 통해 실시간으로 인터랙션 할 수 있는 기법을 제시한다. 모바일과 가상현실 분야에서 사용자의 인터랙션 기술이 중요함에도 불구하고 여전히 사용자 인터페이스 기술의 다양성이 부족하며 대부분 손을 이용한 스크린의 터치나 동작 인식이다. 본 연구에서는 사용자의 입 바람을 이용하여 실시간으로 상호작용할 수 있는 새로운 인터페이스 기술을 제안한다. 사용자와 모바일 디바이스 간의 각도와 위치를 이용하여 바람의 방향을 결정하며 사용자의 입 바람과 가중치 함수를 기반으로 바람의 크기를 계산한다. 제안하는 기술의 우수성을 보여주기 위해 입 바람 외력을 유체 방정식에 적용하여 실시간으로 벡터장의 흐름을 시각화하는 결과를 보여준다. 우리는 제안하는 방법의 결과를 모바일 디바이스 환경에서 보여주지만 인터페이스 기술을 요구하는 가상현실과 증강현실 분야에 응용할 수 있다.

• 한국환경과학회지
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• 제16권1호
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• pp.73-79
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• 2007

The purpose of this study is to clarify the effect of mountain-valley wind on heat island formed in urban area which is located around valley mouth. The meteorological observations were carried out over the Dalbi-valley under a clear summer pressure patterns, and some consideration were tried from the results. In order to make clear the climatological characteristics and air-mass modification process of the mountain-valley wind over the valley, the meteorological observations were done simultaneously at two points. The observational points were located at the breast and valley mouth parts, respectively. The results were as follows: First, it was found that the valley wind was observed through the daytime, and it was replaced by a mountain wind after sunset. Second, the heat budget is also investigated with observation data. The sensible heat flux over the breast of Dalbi-valley reached to about $200 W/m^2$ during daytime, which is a little more than one third of net radiation. On the other hand, the sensible heat flux represented negative values during nighttime. But the sensible heat flux over the valley mouth covered by asphalt showed plus value(about $20{\sim}30 W/m^2$) during the nighttime.

• Journal of the korean society of oceanography
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• 제39권2호
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• pp.119-135
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• 2004

A three-dimensional numerical model using POM (the Princeton Ocean Model) is established in order to understand the dispersion processes of the Yangtze River water in the Yellow and East China Seas. The circulation experiments for the seas are conducted first, and then on the bases of the results the dispersion experiments for the river water are executed. For the experiments, we focus on the tide effects and wind effects on the processes. Four cases of systematic experiments are conducted. They comprise the followings: a reference case with no tide and no wind, of tide only, of wind only, and of both tide and wind. Throughout this study, monthly mean values are used for the Kuroshio Current input in the southern boundary of the model domain, for the transport through the Korea Strait, for the river discharge, for the sea surface wind, and for the heat exchange rate across the air-sea interface. From the experiments, we obtained the following results. The circulation of the seas in winter is dependent on the very strong monsoon wind as several previous studies reported. The wintertime dispersion of the Yangtze River water follows the circulation pattern flowing southward along the east coast of China due to the strong monsoon wind. Some observed salinity distributions support these calculation results. In summertime, generally, low-salinity water from the river tends to spread southward and eastward as a result of energetic vertical mixing processes due to the strong tidal current, and to spread more eastward due to the southerly wind. The tide effect for the circulation and dispersion of the river water near the river mouth is a dominant factor, but the southerly wind is still also a considerable factor. Due to both effects, two major flow directions appear near the river mouth. One of them is a northern branch flow in the northeast area of the river mouth moving eastward mainly due to the weakened southerly wind. The other is a southern branch flow directed toward the southeastern area off the river mouth mostly caused by tide and wind effects. In this case, however, the tide effect is more dominant than the wind effect. The distribution of the low salinity water follows the circulation pattern fairly well.

• 한국해양공학회지
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• 제23권2호
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• pp.18-27
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• 2009

This study was conducted to examine the effect of wind on the circulation of seawater in Gamak Bay, which contains numerous farms for fish and shellfish but suffers a significant loss by fisheries nearly annually from harmful algal blooms. In numerical experiments with a simplified bathymetry for Gamak Bay, the wind in summer appeared to more strongly influence the east-westward flow than the south-northward flow. In winter, this trend was nearly similar to the summer but seemed to have a greater effect on the flow at the north-west of the bay than the flow at the south mouth of the bay. On the other hand, in numerical experiments with a realistic bathymetry for Gamak Bay, the wind in summer appeared to more strongly influence the east-westward flow than the south-northward flow. Furthermore, the effect of the wind was stronger at the south mouth of the bay than at the north-west of the bay. In contrast, the wind in winter affected the east-westward flow more strongly and its effect appeared stronger at the north-west of the bay than at the south mouth of the bay. In addition, the effect of the wind tended to increase with distance from the east to the west. Therefore, the tidal currents in Gamak Bay proved to be strongly influenced by the wind, in particular east-westward. However, some measures are urgently required to improve the water quality of the bay, since the south-northward flow turned out to be obstructed by an east-westward shoal located in the middle of the bay.

• 수산해양기술연구
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• 제28권4호
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• pp.385-397
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• 1992

Current measurements at 3 sections and numerical experiments were carried out in Masan Bay to understand the effect of the wind on the residual currents and pollutant transport. The vertical distribution of horizontal velocities were directly affected by the wind at the depths of 1m and 2m beneath the sea surface. Analysis of the velocity data suggested that changes in the vertical gravitational circulation contributed to the net circulation. The net transport of water through the northern part of the bay was observed to be landward, with wind-induced transport of about 100m super(3)/s. Hence, wind is concluded to be the dominant mechanism driving the net circulation in the northern area of Masan Bay. Numerical experiments are shown that when S wind with 5m/s blew, northern area of the bay was generated the horizontal circulation of clockwise and local gyre. On the contrary of those, N wind made her to the anti-clockwise. In the case of no wind, the tidal residual current(constant flow) is very small or neglected except the bay-mouth. The inflow or outflow pattern of the mouth is considered as the flows generated by tidal residual current only. The distance of wind-induced transport of pollutant was as long as 2 times of no wind during the one tidal period.

• Ocean and Polar Research
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• 제22권2호
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• pp.81-90
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• 2000

Supposed construction of a large port in the mouth of Tuman River requires careful examination of possible unfavorable ecological consequences for the Far Eastern Federal Marine Reserve. Since the Tuman River is the largest source of suspended material and possible contaminants flowing into the sea, and in order to understand how this material is allocated in the coastal zone, analyses are needed to check possible pathways of water transport and circulation system in the region. Linearized shallow water equations were used for numerical simulation of the wind-driven circulation to the north off the Tuman River mouth. The model results satisfactorily agreed with in situ data. The model circulation patterns are largely dependent on the wind direction and are conformed by the distribution of bottom sediments, and by the location of organic carbon and some pollutants accumulation zones. The most unfavorable situation for the Marine Reserve is the case of the southwesterly wind; even with quite moderate wind, the waters polluted by the run-off from the Tuman River can attain the south section of the Marine Reserve during the diurnal period.

• 한국컴퓨터정보학회:학술대회논문집
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• 한국컴퓨터정보학회 2019년도 제59차 동계학술대회논문집 27권1호
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• pp.337-338
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• 2019

본 논문에서는 입 바람 인터페이스를 이용하여 레이싱 게임에서의 논플레이어 캐릭터(Non-player character, NPC)를 제어할 수 있는 새로운 프레임워크를 제안한다. 대부분의 게임 콘텐츠에서 캐릭터를 제어하는 손가락을 이용한 인터페이스 방식이다. 이 같은 인터페이스의 제약은 게임의 재미를 감소시킬 뿐만 아니라 콘텐츠를 사용하는데 있어서 사용자의 몰입을 감쇠시키는 원인이 된다. 본 연구에서는 입 바람 인터페이스를 이용하여 자동차의 방향 및 속도를 제어하고 입 바람으로부터 계산된 바람의 강도를 외력으로 이용하여 NPC를 제어할 수 있는 프레임워크를 제안하여, 게임의 몰입과 재미를 향상시킨다. 본 연구는 Unity 게임 엔진에서 개발했으며 레이싱 게임뿐만 아니라 다양한 콘텐츠에서 활용할 수 있다.

• 대한토목학회논문집
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• 제28권3B호
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• pp.315-321
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• 2008

최근 해안환경적 측면 뿐 만 아니라 사용자의 측면에서 도류제나 방파제와 같은 연안구조물에 의하지 않고 연안에서의 해빈을 보존하기 위한 대책이 요구되고 있다. 연안에서의 표사문제의 대책을 수립하기 위해서는 연안에서의 표사 뿐만 아니라 배후지의 하천으로부터 유출되는 유사량을 포함한 종합적인 토사관리의 필요성이 증가하고 있다. 이같은 관점에서 본 연구에서는 연안해역으로 유출되는 하천 유사와 이송, 하구에서의 사주발생과 발달 그리고 하구폐색과 연안으로 유출된 유사의 효율적인 저류문제와 홍수시 외해로 유출되는 유사의 특성에 대해 검토하였다. 최근 강릉 남대천 하구에는 하구폐색과 하구사주의 발생에 따른 대책으로 2005년에 총연장 260 m의 도류제를 건설하였다. 이에따라 본 연구에서는 도류제 건설에 따른 남대천하구에서의 토사이동특성 및 해저지형 변동과 표사이동을 해석하기 위한 다양한 수치실험을 수행하였다. 이를 위해 먼저 남대천 하구역에서 유출되는 유사량을 혼합입경의 관점을 가정하여 1차원 수치해석을 통하여 해석하였다. 또한 하천에서 유출된 유사의 이동특성과 하구현상을 파악하기 위해 하천류의 유동특성과 바람장에 의한 취송류를 검토하였다. 그리고 파동장, 해빈류 및 해저지형변동을 수립하여 본 남대천 하구인근에서의 표사이동 특성을 해석하였다.

• 한국전자통신학회논문지
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• 제10권2호
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• pp.157-164
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• 2015

본 논문은 낙동강 하류 지역 부유쓰레기에 대한 실시간 이동 경로 추적과 수문기상환경 분석을 통해 구체적인 하구 유출 특성을 파악하고자 하였다. 부유쓰레기의 이동 및 하구 유출 경로를 파악하기 위해 위성 위치발신기를 장착한 소형 부이를 활용하였다. 그리고 수문기상환경을 파악하기 위해 하천 유량 및 하구둑 방류량변화, 하구역의 풍향에 대한 분석을 수행하였다. 향후 본 연구 결과는 집중호우시 낙동강 부유쓰레기의 연안유출 여부와 피해 범위를 파악하는데 기초 자료로 활용할 수 있을 것으로 기대된다.