• 한국환경과학회지
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• 제19권2호
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• pp.171-184
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• 2010

Accurate simulation of the meteorological field is very important to assess the wind resources. Some researchers showed that sea surface temperature (SST) plays a leading role on the local meterological simulation. New Generation Sea Surface Temperature (NGSST), Operational Sea Surface Temperature and Sea Ice Analysis (OSTIA), and Real-Time Global Sea Surface Temperature (RTG SST) have different spatial distribution near the coast and OSTIA shows the best accuracy compared with buoy data in the southeastern coast of the Korean Peninsula. Those SST products are used to initialize the Weather Research and Forecasting (WRF) Model for November 13-23 2008. The simulation of OSTIA shows better result in comparison with NGSST and RTG SST. NGSST shows a large difference with OSTIA in horizontal and vertical wind fields during the weak synoptic condition, but wind power density shows a large difference during strong synoptic condition. RTG SST shows the similar patterns but smaller the magnitude and the extent.

• 대한전기학회:학술대회논문집
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• 대한전기학회 1999년도 하계학술대회 논문집 B
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• pp.969-971
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• 1999

Wavelet analysis is applying to many fields such as the time-frequency localization of a time series and a time varying data. In this paper, a statistical testing based Wavelet power spectrum analysis for the stationary Nino3 Sea Surface Temperature(SST) data was executed. Specially, the 95% confidence level for SST was effective in searching the periods of El-Nino using various wavelet basis functions.

• Ocean and Polar Research
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• 제42권3호
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• pp.179-194
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• 2020

The present study aims to evaluate the effects of satellite-based SST (OSTIA) assimilation on a regional ocean circulation model for the Yellow and East China Seas (YECS), using three different assimilation methods: the Ensemble Optimal Interpolation (EnOI), Ensemble Kalman Filter (EnKF), and 4-Dimensional Variational (4DVAR) techniques, which are widely used in the ocean modeling communities. The model experiments show that an improved initial condition by assimilating the SST affects the seasonal water temperature and water mass distributions of the YECS. In particular, the SST data assimilation influences the temperature structures horizontally and vertically in winter, thereby improving the behavior of the YS warm current water. This is due to the fact that during wintertime the water column is well mixed, which is directly updated by the SST assimilation. The model comparisons indicate that the SST assimilation can improve the model performance in resolving the subsurface structures in wintertime, but has a relatively small impact in summertime due to the strong stratification. The differences among the different assimilation experiments are obvious when the SST was sharply changed due to a typhoon passage. Overall, the EnKF and 4DVAR show better agreement with the observations than the EnOI. The relatively low performance of EnOI under storm conditions may be related with a limitation of EnOI method whereby an analysis is obtained from a number of climatological fields, and thus the typhoon-induced SST changes in short-time scales may not be adequately reflected in the data assimilation.

• 대기
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• 제22권4호
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• pp.483-488
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• 2012

The monsoon front lies on East Asian region, but it gradually propagates to the north during the boreal summer. The equivalent potential temperature (EPT) reveals the thermodynamical features of air masses and monsoon front. Therefore, this study considered the thermodynamical EPT and dynamical wind fields to clarify the peculiarity of East Asian summer monsoon (EASM) variations in June and July, respectively. Western North Pacific subtropical high (WNPSH) and Okhotsk sea high (OSH) both play the crucial role to interannual variations of EASM frontal activity and amount of rainfall. The OSH is important in June, but the WNPSH is key factor in July. Furthermore, the OSH (June) is affected by North Atlantic tripolar sea surface temperature (SST) pattern and WNPSH (July) is influenced by North Indian Ocean SST warming.

• Wind and Structures
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• 제37권4호
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• pp.303-314
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• 2023

In this study, two steady RANS turbulence models (SST k-ω and Realizable k-ε) and four unsteady turbulence models (URANS SST k-ω and Realizable k-ε, SST-SAS, and SST-IDDES) are evaluated with respect to their capacity to predict crosswind characteristics on high-speed trains (HSTs). All of the numerical simulations are compared with the wind tunnel values and LES results to ensure the accuracy of each turbulence model. Specifically, the surface pressure distributions, time-averaged aerodynamic coefficients, flow fields, and computational cost are studied to determine the suitability of different models. Results suggest that the predictions of the pressure distributions and aerodynamic forces obtained from the steady and transient RANS models are almost the same. In particular, both SAS and IDDES exhibits similar predictions with wind tunnel test and LES, therefore, the SAS model is considered an attractive alternative for IDDES or LES in the crosswind study of trains. In addition, if the computational cost needs to be significantly reduced, the RANS SST k-ω model is shown to provide relatively reasonable results for the surface pressures and aerodynamic forces. As a result, the RANS SST k-ω model might be the most appropriate option for the expensive aerodynamic optimizations of trains using machine learning (ML) techniques because it balances solution accuracy and resource consumption.

• 한국지리정보학회지
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• 제23권3호
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• pp.263-274
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• 2020

한국 남동해역은 매년 하계에 집중적으로 냉수대가 형성되어 빈번한 이상해황이 발생한다. 본 연구에서는 이 해역에서 발생하는 표층수온 분포의 공간 변화를 분석하기 위해 2018년 6월에서 9월까지 고리와 정자 부이에서 관측한 해양현장 수온 데이터와 GHRSST Level 4 재분석 해수면 온도(sea surface temperature: SST) 자료를 이용하였다. 부이 자료는 두 지점의 시계열적 수온 변동 분석에, GHRSST 자료는 연구해역 전반에 걸친 일별 SST의 분산과 가중공간중심(weighted mean center: WMC)을 계산하는데 이용하였다. 부이의 수온이 낮아지면 연구해역 SST의 분산이 증가하는 경향을 보였으나, 전 기간 일치하게 나타나지는 않았다. 이는 GHRSST가 재분석 자료로 연안의 민감한 수온변화를 반영하지 못하기 때문이다. 이와 같이 전 해역의 SST 변화를 대표하는 통계적 분산만으로는 연안의 국지적인 소규모의 수온변화를 파악하거나, 냉수대 발생해역의 위치 및 범위를 탐지하기에는 한계가 있다. 따라서 차가운 수괴가 발생하는 공간적인 위치를 정량적으로 파악하기 위해 WMC를 활용하여 분석한 결과 냉수대가 발생했을 때, WMC가 연구해역의 공간중심(mean center: MC)으로부터 북서 해역 쪽에 위치하였다. 이는 SST의 WMC 위치 정보를 통해 차가운 표층수온의 분포가 어디에서 어느 정도 나타나는지를 정량적으로 파악할 수 있음을 의미하며, 향후 냉수대 규모 및 지역 확산 범위 탐지에 WMC의 활용 가능성을 알 수 있었다.

• 대한전기학회논문지:전기기기및에너지변환시스템부문B
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• 제55권12호
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• pp.617-622
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• 2006

It is necessary to measure precisely the magnetic characteristics of electrical steel sheets under rotating magnetic fields, to obtain an accurate numerical performance analysis of electric machines made of electrical steel sheets. In this paper, the two dimensional magnetic characteristics of an electrical steel sheet are measured and explained under rotating magnetic fields using a two-axes-excitation type single sheet tester (SST). Through experiments, the magnetic properties, under rotating magnetic fields, of a non-oriented and grain oriented electrical steel sheet were measured respectively. In addition, the iron losses due to not only the alternating magnetic fields, but also rotating magnetic fields were measured. These experimentally measured results can evidently be applied to the analysis of iron losses in electrical machines.

• 대한전기학회논문지:전기기기및에너지변환시스템부문B
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• 제55권5호
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• pp.250-257
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• 2006

It is well known that Grain-oriented electrical steel sheets have two dimensional magnetic properties according to the direction of exciting field such as non-linear phase difference between magnetic flux density and magnetic field intensity vectors, different iron loss and permeability even when an alternating magnetic field is applied. The measurement and application of the two dimensional magnetic properties of the Grain-oriented electrical steel sheets, therefore, are very important for the design and precise performance analysis of electric machines made of them. As the direction of exciting field changes, in this paper, the two dimensional magnetic properties of a Grain-oriented electrical steel sheet, i.e., non-linear B-H curves, phase difference between B and H, and iron loss characteristics, are measured using SST(Single Sheet Tester) which has two axes excitation. The measured results are presented in two ways: using $(B,\theta_B)$ method and using hysteresis loops along rolling and transverse directions, respectively.

• Nuclear Engineering and Technology
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• 제41권7호
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• pp.907-920
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• 2009

This study was performed to evaluate the prediction capability of a commercial CFD code and to investigate the effects of different geometries such as a 4.4 mm tube and an 8/10 mm annular channel on the detailed flow structures. A numerical simulation was performed for the conditions, at which the experimental data was produced by the test facility SPHINX. A 2-dimensional axisymmetric steady flow was assumed for computational simplicity. The RNG $\kappa-\varepsilon$ turbulence model (RNG) with an enhanced wall treatment option, SST $\kappa-\omega$ (SST) and low Reynolds Abid turbulence model (ABD) were employed and the numerical predictions were compared with the experimental data generated from the experiment. The effects of the geometry on heat transfer were investigated. The flow and temperature fields were also examined in order to investigate the mechanism of heat transfer near the wall. The local heat transfer coefficient predicted by the RNG model is very close to the measurement result for the tube. In contrast, the local heat transfer coefficient predicted by the SST and ABD models is closer to the measurement for the annular channel.

• 한국수산과학회지
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• 제30권2호
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• pp.188-202
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• 1997

본 연구에서는 한국 동해에서의 바람장의 공간적인 분포특성을 정량적으로 파악하기 위하여 해면기압과 해상풍 자료에 EOF 분석방법을 적용하여 모드별로 고유함수의 공간적인 분포특성과 시간계수를 계산하였고 시간계수의 스펙트럼을 구하여 바람장의 공간 및 시간변동성 및 주기적인 특성을 파악하였다. 평균기압의 분포는 서고동저형의 등압선 배치를 나타내며, 기압의 최대 표준 편차는 블라디보스톡 부근에 위치하고 일본연안으로 갈수록 최저 표준편차를 갖는다. 블라디보스톡 부근은 $6.5^{\circ}C$의 해수면 온도의 최대 표준편차를 갖는 지역이기도 하다. 동서성분 해상풍의 제1모드는 분산의 $47.3\%$ 제2모드는 $30\%$를 반영하며 제1모드는 블라디보스톡 해역에서 최대 변화를 보이며 1년 및 6개월의 주기를 갖는다. 특히 제2모드에서 6개월의 주기가 탁월하다. 해상풍의 남북성분의 연평균 분포는 동해전역에서 북풍계열의 바람이 탁월하며, 특히 블라디보스톡 부근에서 최대 2.2m/s 이상의 북풍이 존재하고 3.8m/s의 표준편차 최대치가 존재하며 시간변동이 크다. 해수면 수온의 공간분포 역시 블라디보스톡 해역에서 최대치가 나타난다. 해상풍과 해면 기압의 결합 직교함수의 모드별 특성은 개별 직교함수에 비해 동서성분 해상풍의 제1모드의 기여도가 증가 하였으며, 제2모드의 기여도는 감소하는 양상을 띤다. 이로 인해 동서성분 해상풍과 해면기압의 결합 직교함수 (WU-PR)의 주기성은 해면 기압의 영향으로 제1모드에서는 1년 및 6개월의 주기가 탁월하며, 제2모드에서는 3개월의 계절변화로 해상풍의 개별 직교함수의 주기와 다르게 나타난다. 해수면 온도의 직교함수까지 포함한 3개의 결합 직교함수의 EOF분석에서는 제2모드에서 해상풍의 공간분포는 해수면 온도에 좌우되는 양상을 보인다. 스펙트럼 분석결과는 제1모드에서 1년 주기가 탁월하며 제2모드는 3개월 및 4개월의 계절변화가 나타난다.