• 한국감성과학회:학술대회논문집
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• 한국감성과학회 2000년도 추계학술대회 논문집
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• pp.181-184
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• 2000

가상현실 시스템은 대부분 가상세계에 대해 사용자의 3차원 제어작업을 요구하게 된다. 이때 3차원 제어작업을 효과적으로 하기 위한 입출력장치의 최적 설계는 매우 중요하다. 본 연구에서는 3차원 표시장치의 주요 설계요소인 공간적 해상도(spatial resolution), 시간적 해상도(temporal resolution or frame rate), 가상세계의 복잡도가 3차원 제어작업의 인간성능에 미치는 영향을 알아보았다. 이를 위해 3 조건의 화면 해상도, 2 조건의 프레임 레이트(18 Hz고정과 18Hz 이상 변동 최대화 조건), 3 조건의 가상세계 복잡도에 대한 18 조합에 대한 실험을 실시하였다. 실험결과 18Hz 로 고정된 프레임 레이트 조건이 프레임 레이트를 그 이상 최대로 하는 것보다 더 좋은 제어성능을 보였다. 화면 해상도는 높을수록 제어성능이 향상되었다. 가상세계의 복잡도에서는 방향정보만 주는 경우가 방향 정보가 없는 경우나 너무 많은 정보가 있는 경우보다 나은 성능을 보였다. 이러한 실험결과는 가상환경 시스템의 표시장치나 가상세계 설계에 참조될 수 있을 것이다.

• 천문학회지
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• 제22권2호
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• pp.141-160
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• 1989

In order to derive time dependence of the atmospheric diffuse light, which consists of the airglow continuum emission and diffusely scattered radiations of the intergrated starlight, the diffuse Galactic light, and the zodiacal light, we have analyzed the meridian scan observations of the sky brightness at $5,080\;{\AA}$ and $5,300\;{\AA}$. Amplitude of the time-variation becomes larger for lower elevation, and maximum amplitude is found to be about $50\;S_{10}(V)_{G2V}$ at elevation $10^{\circ}$. The atmospheric diffuse radiation attains maximum brightness at around midnight, and afterward it decreases slowly with time. The time-variations for the two wavelengths are similar to each other. The observed brightness distribution of the diffuse light along the zenith distance is fitted to an empirical relation of two parameters. By making the two parameters time-dependent, we describe the spatial and time variations of the atmospheric diffuse light. This enables us to make time dependent correction for the atmospheric diffuse component in the reduction of zodiacal light brightness.

• 한국지하수토양환경학회지:지하수토양환경
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• 제11권5호
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• pp.9-19
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• 2006

지하수 함양량을 정확하게 산정하는 것은 지하수계의 적절한 관리를 위해서 매우 중요하다. 국내에서 주로 사용되는 지하수 함양량 추정방법은 지하수위 변동법, 기저유출 분리법, 연단위 물수지 분석법 등이 있다. 그러나, 이들 방법은 집중형 개념을 기반으로 하거나 국지적인 규모로 다뤄지기 때문에 기후조건, 토지이용, 토양조건, 수리지질학적 비균질성에 의한 함양량의 시공간적 변동성을 반영할 수 없다. 따라서 본 연구에서는 유역내의 토양 및 토지이용에 따른 비균질성을 반영할 수 있는 SWAT 모형을 이용하여 시공간적 변동성을 고려한 지하수 함양량을 산정하는 방법을 제시하였다. SWAT 모형은 유역내 일단위 지표면 유출량, 증발산량, 토양저류량, 함양량, 지하수유출량 등의 수문성분을 계산할 수 있는 모형이다. 본 연구에서는 SWAT 모형을 미호천 유역의 최상류인 무심천 유역에 적용하였다. 2001년-2004년까지의 기간동안 지하수 함양량을 포함한 유역의 일단위 수문성분들을 모의하였으며, 유역출구점에서의 실측 일유춘자료와 모의 일유출자료의 비교를 통해서 모의결과의 유효성을 검토하였다. 지하수 함양량의 시공간적 변화를 분석한 결과, 지하수 함양량의 변동성은 토지이용도 뿐만 아니라, 유역경사와 같은 지형인자에도 큰 영향을 받는 것으로 분석되었다.

• 천문학회보
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• 제31권1호
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• pp.31-31
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• 2006

• 한국대기환경학회:학술대회논문집
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• 한국대기환경학회 2009년도 추계학술대회 논문집
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• pp.625-627
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• 2009

• 대한전기학회:학술대회논문집
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• 대한전기학회 2006년도 제37회 하계학술대회 논문집 D
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• pp.2113-2115
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• 2006

This paper proposes a spatio-temporal correlation algorithm that takes advantage of the spatial and temporal correlations in video streams for error concealment. The spatio-temporal correlation algorithm sets the neighborhood area of the damaged part as a reference window, then finds the area that best matches the reference window in the previous frame. The best-matched area in the previous frame replaces the damaged part in the current frame. The results of ten variations of the proposed algorithm are compared with conventional error concealment methods. These methods include the ones applicable to P-frames as well as I-frames. The comparison results show that the proposed algorithm is very efficient for l-frame error concealment with a large motion between frames.

• 한국환경과학회지
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• 제13권4호
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• pp.377-387
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• 2004

This study has been performed to clarify the characteristics of temporal and spatial distribution of surface ozone concentration over Jeju Island, one of the cleanest areas in Korea with low emissions of air pollutants. Ozone data are monitored at four sites in Jeju Island. These monitoring sites are located at two urban area(referred to Ido and Donghong), coastal area(Gosan site) and forest site(Chuna site). Ozone data has been routinely collected at these sites for the late four years. The patterns of seasonal cycle of ozone concentrations at all stations show the bimodal with the peaks on spring and autumn and a significant summer minimum. However, the patterns of diurnal variations at rural station, i.e., Gosan and Chuna sites are considerably different to those at urban stations such as Ido and Donghong sites. The patterns of $\DeltaO_3$ variations are very similar with those of monthly mean ozone concentrations and $\DeltaO_3$ values are exceeded 30 ppb, at urban stations. This may be that urban stations are more influenced by local photochemical reactions rather than rural stations. In order to assess the potential roles of meteorological parameters on ozone formation, the meteorological parameters, such as radiation, temperature, and wind are monitored together with ozone concentrations at all stations. The relationships of meteorological parameters to the corresponding ozone concentration are found to be insignificant in Jeju Island. However, at Gosan and Donghong stations, when the sea breeze blew toward the station, the ozone concentration is considerably increased.

• 환경영향평가
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• 제16권6호
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• pp.421-432
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• 2007

To investigate temporal and spatial variations of hydrodynamics and environmental conditions in Gyeonggi Bay, including Han River estuary, numerical experiments were performed using 3-dimensional fine grid numerical ocean model. The model successfully reproduced the physical phenomena already known in Gyeonggi Bay where tide and fresh water discharge are dominant forcings. The calculated harmonic constants of tide and tidal current agreed well with those of observations at nine tide stations and two tidal current stations. Tidal asymmetries along the Yeomha Waterway, mainly caused by non-linear effect, were well reproduced and agreed well with observations. Time series of salinity at four stations(A, B, C and D) and horizontal distributions of monthly averaged salinity show that Gyodong and Seokmo Waterways play an important role in fresh water discharge into the Gyeonggi Bay rather than Yeomha Waterway.

• 한국환경과학회지
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• 제18권2호
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• pp.141-151
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• 2009

Temperature, salinity, COD, DIN (Dissolved Inorganic Nitrogen), DIP (Dissolved Inorganic Phosphorus), and Chlorophyll ${\alpha}$ obtained from the southern coastal waters during the period of 2003 to 2005 were analyzed. Variability in temperature was not found between groups in southern coastal waters, but significantly different depending on sampling sites (p<0.05). The average temperature in 2003 estimated at $18.33^{\circ}C$ that was annually increased by 2005 and significantly different based on statistics (p<0.05). Unlikely to temperature, salinity was significantly different depending on sampling sites, as well as monthly variations (p<0.05). Likewise to temperature, the value of salinity was annually increased. COD estimated at the average of $>1.7\;mg\;l^{-1}$ for three years, indicating optimal water quality. The fluctuations of nutrients were extremely shown in different sampling sites and monthly variations. Chlorophyll a recorded above $2.0{\mu}g\;l^{-1}$ which was associated with high primary phytoplankton, whereas it showed much fluctuations in temporal and spatial, In particular, Tongyong, Jaranman, Jinjuman, and Samcheonpo located in the southeast were the highest fluctuations in water quality than any other regions. The correlation between salinity/COD and nutrients/chlorophyll a was strongly negative or positive, which was possibly associated with much the introduction of run-off water as well as rainfall in summer.

• 수산해양교육연구
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• 제24권2호
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• pp.333-345
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• 2012

NOAA/AVHRR, Topex/Poseidon, and Jason-1 data were used to analyze sea surface temperatures and thermal fronts in the North East Asia Seas. Temporal and spatial analyses were based on data from 1993 to 2008. The amplitude and phase for the annual mode on SL and SST were investigated with harmonic analysis. The geographical distribution of amplitudes for comparison of SL and SST are slightly reverse in southwest-northeast tilted direction. The time series analysis conducted on the entire researched area presented consistent pattern. Peak of Sea Level was presented 1~2 months after the peak of the surface sea temperature was shown. This explains that Sea Level change occurs after the generation of surface sea temperature change in sea. The Sobel edge detection method delineated four fronts. Thermal fronts generally occurred over steep bathymetric slopes. Annual amplitudes and phases were bounded within these frontal areas.