• Transactions of the Korean Society of Mechanical Engineers
• /
• v.6 no.2
• /
• pp.160-168
• /
• 1982

수평으로 놓여진 2개의 동심타원 사이의 환상공간에서의 자연대류현상이 수치계산 및 실험적으로 연구되었다. 수치적 연구는 정상 2차원 층류유동영역에서 수행되었으며 유선 및 등온선이 구하여 졌다. 또한 특수한 경우로서 수평동심원 사이의 환상공간에 관한 기존연구와 비교하여 좋은 일치 를 보았다. 실험적 연구에서는 3개의 실험모델을 제작하였으며 마하젠더 간섭계에 의한 간섭사진 으로부터 등온선 분포를 얻었으며 아울러 유동에 관한 정보도 얻을 수 있었다. 실험과 수치계산 결과는 상당히 좋은 일치를 보였으며 기존 동심원환상공간에 편심율이 추가된 이론전개 및 수치 계산방법의 적합성을 알 수 있었고 이로서 환상공간에서의 자연대류에 관한 연구를 확장시켰다.

• Review of KIISC
• /
• v.16 no.3
• /
• pp.25-33
• /
• 2006

본 논문에서는 임베디드 시스템 온칩 적용을 위한 통합 보안 프로세서를 SIP(Semiconductor Intellectual Property)로 설계하였다. 각각의 SIP는 VHDL RTL로 모델링하였으며, 논리합성, 시뮬레이션, FPGA 검증을 통해 재사용이 가능하도록 구현하였다. 또한 ARM9과 SIP들이 서로 통신이 가능하도록 AMBA AHB의 스펙에 따라 버스동작모델을 설계, 검증하였다. 플랫폼기반의 통합 보안 SIP는 ECC, AES, MD-5가 내부 코어를 이루고 있으며 각각의 SIP들은 ARM9과 100만 게이트 FPGA가 내장된 디바이스를 사용하여 검증하였으며 최종적으로 매그나칩 $0.25{\mu}m(4.7mm\times4.7mm)$ CMOS 공정을 사용하여 MPW(Multi-Project Wafer) 칩으로 제작하였다.

• 한국지구물리탐사학회:학술대회논문집
• /
• 2005.05a
• /
• pp.233-236
• /
• 2005

Polarization filtering based on the multicomponent complex trace analysis method is performed to reject Rayleigh waves and to enhance S waves. To test the polarization filter, synthetic seismic data were constructed for a simple two-layer model based on the finite difference method. Rayleigh waves with elliptic motion are eliminated effectively and P and S waves with linear motions are well separated each other.

• Journal of the Korea Society of Computer and Information
• /
• v.10 no.2 s.34
• /
• pp.123-132
• /
• 2005

In this paper, a conventional key exchange method simply Performs the key exchange setup step based on discrete algebraic subjects. But the mutual-authentication procedure of wireless PKI for reducing authentication time uses an elliptical curve for a key exchange setup step. Proposed hand-over method shows reduced hand-over processing time than conventional method since it can reduce CRL retrieval time. Also, we compared proposed authentication structure and conventional algorithm, and simulation results show that proposed authentication method outperforms conventional algorithm in authentication waiting time.

• Journal of the Korean Geophysical Society
• /
• v.8 no.1
• /
• pp.35-38
• /
• 2005

Polarization filtering based on the multicomponent complex trace analysis method is performed to reject Rayleigh waves and to enhance S waves. To test the polarization filter, synthetic seismic data were constructed for a simple two-layer model based on the finite difference method. Rayleigh waves with elliptic motion are eliminated effectively and P and S waves with linear motions are well separated each other.

• Proceedings of the Korea Information Processing Society Conference
• /
• 2013.11a
• /
• pp.1386-1389
• /
• 2013

조영증강 초음파 동영상은 측정 부위의 혈류의 형태와 특성 정보를 포함하지만, 이를 육안으로 판별하는 것은 매우 어려운 일이다. 이에 본 연구에서는 초음파 영상으로부터 간 질환과 연관한 병변을 추출하고 그 특성을 분석하기 위한 기반 기술로서 영상 처리 및 분석 기법을 제안한다. 마이크로버블(microbubble) 형태의 노이즈와 빠른 속도로 변화하는 각 프레임의 영상으로부터 근사화된 원형 또는 타원 형태로 나타나는 병변을 추출하기 위하여 허프 변환(Hough transform)을 이용한 병변 추출 기법을 제시하며, 추출한 병변의 특성을 분석하기 위하여 TIC(time intensity curve)의 특성과 조영 효과의 전이 시간(transit time) 등의 정보를 영상의 형태로 가시화하는 방법과 MRF(Markov random field) 모델을 이용한 영상개선 기법을 소개한다. 제안된 이론은 실제 간 질환 진단 초음파 영상에 적용하여 그 유용성을 평가한다.

• 한국해양학회지
• /
• v.17 no.2
• /
• pp.41-50
• /
• 1982

We present theoretical models for the unstedy transports driven by the time-varying wind stress in horizontally unbounded shallow seas of an uniform depth. We derive linearized transport equations that inchude the acceleration, the Coriolis firce, the wind stress and the bottom friction. The steady transport in a shallow sea is different from the classical Ekman transport because of a presence of non-negligible bottom fricttttion. The transient reansport and an inertial oscillation of which frequency of rotation is the same as the frequency of the wind stress forcing. The transprt associated with a wind stress of which direction changes linearlywith time is decribed by a superpoeition so a free inertial oscillation with a pweiod of one inertial day, The theoretical models of the transports are useful in understanding the time-varying currents and the transports of nutrients in shallow seas.

• Journal of the Korean Society of Marine Environment & Safety
• /
• v.24 no.2
• /
• pp.179-187
• /
• 2018

In order to understand the flow of currents around Aphae Island and the surrounding Archipelago, the numerical model experiments on tidal currents and tide-induced residual currents were carried out. Dominant semidiurnal tidal currents have a reversing form and flow along the narrow channels of the archipelago. During periods of flood, currents flow from the west of Hwawon Peninsula to the archipelago to the northwest together with the currents flowing from the channels at Palgeum Island to Amtae Island and Amtae Island to Jeung Island. Ebb currents flow from the northwest archipelago to the channel of Amtae Island and Jeung Island as well as Amtae Island to Palgeum Island, further flowing south between Palgeum Island and Hwawon Peninsula. Flood currents are separated from east and west at the southern coast of Aphae Island, but flow south from both the west and east of Aphae Island to the channel found between Palgeum Island and Hwawon Peninsula at ebb. Flow speed is high between Amtae Island and Aphae Island where the flows meet and join. Lee wakes or topographical eddies are formed around the islands due to the high speed of the currents flowing along the narrow channel in the archipelago, manifesting as a tide-induced residual current. A weak cyclonic wake and anti-cyclonic eddy both exist at the west and northwestern coast of Aphae Island individually. The speed of the tide-induced residual current become slow on account of the wide littoral zone at exists around Aphae Island.

• Journal of the Institute of Convergence Signal Processing
• /
• v.12 no.1
• /
• pp.67-75
• /
• 2011

This paper presents the systematic optimal design of an overlapped ultrasonic sensor ring for high performance obstacle detection using effective beam overlap. Basically, a set of low directivity ultrasonic sensors of the same type are arranged in a circle at regular intervals with their beams overlapped. First, both real and simplified beam patterns of an ultrasonic sensor and several sensor models for obstacle position estimation within its beam pattern are introduced. Second, the obstacle detection range of an overlapped ultrasonic sensor ring and its simple sensor model for obstacle position estimation are described. Third, for both conic and non-conic shaped beam pattern, the design indices of an overlapped ultrasonic sensor ring for minimal positional uncertainty in obstacle detection are defined. Fourth, the constraints imposed on the structural parameters of an overlapped ultrasonic sensor ring to guarantee non empty beam overlap and to avoid excessive beam overlap are derived. Fifth, the optimal number of ultrasonic sensors for a given radius of an overlapped ultrasonic sensor ring and the optimal radius of an overlapped ultrasonic sensor ring are determined. Throughout this paper, the MA40B8 from Murata Inc. is taken as a representative commercial low directivity ultrasonic sensor.

• Journal of the Korean Society of Surveying, Geodesy, Photogrammetry and Cartography
• /
• v.26 no.1
• /
• pp.51-61
• /
• 2008

The determination of precise geoid model for the Jeju island is needed to minimize the effect of different vertical datums. This study describes the development of gravimetric geoid model referred to GRS80 reference surface for the area of Jeju island. We used ECM96 up to degree and order 360 as a reference model and added the terrain and the residual gravity effects to the reference model. After then 17 GPS/Levelling data were used to correct the difference between the GPS/Levelling-derived geoid heights and gravimetric geoid heights. The least square collocation was applied to derive the correction and the grid values. The final precise geoid model(Jeju_GEOID07) that consist of $0.75'{\times}1'$(about $1.4km{\times}1.5km)$ grid interval was obtained in the region of $33^{\circ}{\sim}33.8^{\circ}N$ and $125.8^{\circ}{\sim}127.2^{\circ}E$. Concerning this works, the precise geoid for the Korean peninsula should be determined by integrating the different geoid developed for the peninsula and Jeju island. It is also need to integrate the vertical datum using long-term tide and GPS observations.