• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume I
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• pp.364-367
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• 2006

Nonlinear internal waves (NLIWs) are usually generated by nonlinear process on linear internal waves (IW). Near HengChun Ridge that links Taiwan and Luzon Islands, we found that there are linear internal waves following NLIW and they travel westward at different speed, about 1.5 m/s for IW and 2.9 m/s for NLIW. This phenomenon was observed on site with ship radar and echo sounders, and later verified with thermistor chain. West of Luzon Strait, the separation of NLIW are 5 km or more, while linear internal waves are lines of wave crests at nearly equal distance that is only a few hundred meters apart. The current hypothesis is that most of the energy of internal tide forms a beam that propagates upward from the eastern shoulder of ocean ridge and later interacts with sea surface and thermocline. The interaction with thermocline generates linear internal wave that propagate along the pycnocline at about 1.5 m/s. The interaction with sea surface scatters internal wave energy downward, ensonifies the water column and generates large nonlinear waves that propagate westward at 2.9 m/s as mode 1 in a waveguide.

• 한국해안·해양공학회논문집
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• 제27권4호
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• pp.258-265
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• 2015

지난 20년 동안 해양구조물과 선박 등에 예상치 못한 피해를 주는 freak waves에 대한 연구자들의 관심이 증가하고 있다. 다양한 연구결과에도 불구하고 아직 freak waves의 발생원인, 발생 메커니즘, 발생확률 등에 대한 상반된 결과로 인해 합의된 결과가 도출되지 못하고 있다. 본 논문에서는 동해항 전면 해상에서 측정된 파랑자료를 분석하여 freak waves에 대한 발생확률을 추정하였다. 유의파고 2.5 m 보다 크고 $H_m/H_S{\geq}2$인 freak waves 3개를 발견하였다. Freak waves의 발생확률은 극치파고분포함수를 사용하여 추정하기 적절하며, Mori, Rayleigh, 그리고 Ahn의 극치파고분포함수는 freak wave의 발생확률을 각각 약 O($10^{-1}$), O($10^{-2}$), 그리고 O($10^{-3}$) 정도로 추정하였다. 본 논문에서 분석된 파랑자료의 freak waves의 발생확률은 O($10^{-2}$)와 O($10^{-3}$) 사이에 위치하였다. 즉, Rayleigh와 Ahn의 극치파고분포함수에 의해 예측된 발생확률의 중간에 위치하였다. 현재 Rayleigh와 Ahn의 극치파고분포함수 중에 어떤 분포함수가 정확한지에 대한 판단은 좀 더 다양한 해역에서의 freak waves의 발생확률에 대한 분석이 필요하다고 판단된다.

• 대한전자공학회논문지TC
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• 제41권8호
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• pp.105-111
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• 2004

본 논문에서는 밀리미터파 대역에서 고이득과 광대역 특성을 갖는 MHEMT(Metamorphic High Electron Mobility Transistor) cascode 증폭기를 설계 및 제작하였다. Cascode 증폭기 제작을 위해 0.1 ㎛ InGaAs/InAlAs/GaAs MHEMT를 설계ㆍ제작하였다. 제작된 MHEMT는 드레인 전류 밀도 640 mA/mm, 최대 전달컨덕턴스(gm)는 653 mS/mm를 얻었으며, 주파수 특성으로 f/sub T/는 173 GHz, f/sub max/는 271 GHz의 우수한 특성을 나타내었다. Cascode 증폭기는 CPW 전송선로를 이용하여 광대역 특성을 얻을 수 있도록 정합회로를 설계하였으며, 1단과 2단 증폭기의 2가지 종류로 회로를 설계하였다. 설계된 증폭기는 본 연구에서 개발된 MHEMT MIMIC 공정을 이용해 제작되었다. 제작된 cascode 증폭기의 측정결과, 1단 증폭기는 3 dB 대역폭이 31.3∼68.3 GHz로 37 GHz의 넓은 대역 특성을 얻었으며, 대역내에서 평균 9.7 dB 및 40 GHz에서 최대 11.3 dB의 S21 이득 특성을 나타내었다. Cascode 2단 증폭기는, 3 dB 대역폭이 32.5∼62.0 GHz로 29.5 GHz의 대역폭과 대역내에서 평균 20.4 dB 및 36.5 GHz에서 최대 22.3 dB의 높은 이득 특성을 얻었다.

• 해양환경안전학회지
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• 제21권5호
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• pp.583-590
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• 2015

우리나라 서남해역에서 추진될 해상풍력 발전 단지에서 생산된 전기와 기존의 전력망과의 계통연계를 위해서는 해저케이블 설치가 필수적인 요소이다. 특히 해저케이블 설치에 대한 경제성, 시공성 및 안정성 확보를 위해서는 해저케이블 경과지와 해저케이블 보호공법 설계가 이루어져야한다. 본 논문에서는 1979년부터 2002년까지 한국해양과학기술원에서 구축한 장기 파랑산출자료와 제3세대 파랑 모델인 SWAN(Simulating WAves Nearshore)을 이용하여 해상풍력단지가 조성될 해역에 대해 만조와 간조시 파랑시뮬레이션을 수행하여 해저케이블 경과지와 보호공법 설계를 위한 기초자료를 제공하고자 하였다. 연구결과, 서남해 해상풍력단지가 조성될 해역의 연평균 Hs는 1.03 m, Tz는 4.47s이고, 주파향은 북서(NW)와 남남서(SSW) 방향이다. NW에서 입사되는 조건(Hs: 7.0 m, Tp: 11.76s)에서 만조시 천해설계파랑 Hs의 분포는 약 4.0~5.0 m, 간조시에 약 2.0~3.0 m로 계산되었다. SSW에서 입사되는 조건(Hs: 5.84 m, Tp: 11.15s)에서 만조시 천해설계파랑 Hs의 분포는 약 3.5~4.5 m이고, 간조시에는 약 1.5~2.5 m로 계산되었다. 해저케이블 경과지 중 경도 UTM 249749~251349 구간 약 1.6 km에서는 NW로 입사되는 파랑의 영향이 크며, UTM 251549~267749 구간 약 16.2 km에서는 SSW로 입사되는 파랑의 영향이 지배적이다. 파랑집중 현상이 두드러지게 나타나는 해역은 위도와 하왕등도 사이 해역으로, 이 해역에서는 주변해역 보다 상대적으로 높은 파고를 나타내고 있다.

• 대한조선학회논문집
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• 제54권3호
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• pp.258-266
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• 2017

Numerical simulations of turbulent two phase flows around KCS have been performed to investigate effects of trim conditions on ship resistance of KCS in short waves by utilizing waves2foam. The wave lengths of LPP/2 and LPP/4 with 1m and 2m wave heights were imposed at inlet boundary. The resistance reduction at 2m trim by head and the increase of resistance at trims by stern were observed regardless of wave lengths and wave heights. The hull pressure on fore-and-aft rather than wave patterns around bulbous bows was mainly responsible for the total resistance coefficients of KCS in short waves. A phase diagram of contribution of hull pressure to the total resistance coefficients disclosed that the phase of representing the maximum resistance in time history played an important role in the effect of trim conditions on ship resistance of KCS in short waves.

• 한국해양공학회지
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• 제26권2호
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• pp.8-13
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• 2012

This paper investigates the statistical properties of waves in the sea area of Uljin, which is located in the East Sea area of Korea. The wave data were measured using AWAC (Acoustic Wave and Current Meter), which was installed at a 16-m water depth from November 2010 to March 2011. The wave data acquisition rate, Hmax, monthly mean Hs, Tz, Tp, and wave direction are summarized. The distributions of Hs and Tz were analyzed using the Hs-Tz scatter diagrams. The measurement wave data were analyzed to investigate freak wave characteristics. By comparing the wave spectrum using the measurement wave data with the wave spectrum obtained by varying the JONSWAP wave spectrum, it was possible to approximate the wave spectrum shape at the Uljin Sea area.

• 한국정보통신학회:학술대회논문집
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• 한국정보통신학회 2017년도 추계학술대회
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• pp.425-428
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• 2017

본 논문에서는 진동 에너지를 이용하여 에너지를 수확하는 전파 정류 하베스팅 회로를 설계하였다. 설계된 회로는 저전압에서도 전력효율이 우수하도록 Beta-Multiplier를 이용하여 Body-Bias technique을 Negative Voltage Converter에 적용하였으며, Comparator를 Bulk-Driven type으로 설계하였다. 제안된 회로는 $0.35{\mu}m$ CMOS 공정으로 설계하였으며, 설계된 회로의 칩 면적은 $931{\mu}m{\times}785{\mu}m$이다.

• 대한원격탐사학회지
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• 제29권6호
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• pp.631-644
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• 2013

Significant Wave Height (SWH) data measured by satellite altimeters (Topex/Poseidon, Jason-1, Envisat, and Jason-2) were validated in the seas around Korea by comparison with wave height measurements from marine meteorological buoy stations of Korea Meteorological Administration (KMA). A total of 1,070 collocation matchups between Ku-band satellite altimeter data and buoy data were obtained for the periods of the four satellites from 1992 to the present. In the case of C-band and S-band observations, 1,086 matchups were obtained and used to assess the accuracy of satellite SWH. Root-Mean-Square (RMS) errors of satellite SWH measured with Ku-band were evaluated to roughly 0.2_2.1 m. Comparisons of the RMS errors and bias errors between different frequency bands revealed that SWH observed with Ku-band was much more accurate than other frequencies, such as C-band or S-band. The differences between satellite SWH and buoy wave height, satellite minus buoy, revealed some dependence on the magnitude of the wave height. Satellite SWH tended to be overestimated at a range of low wave height of less than 1 m, and underestimated for high wave height of greater than 2 m. Such regional characteristics imply that satellite SWH should be carefully used when employed for diverse purposes such as validating wave model results or data assimilation procedures. Thus, this study confirmed that satellite SWH products should be continuously validated for regional applications.

• 한국신재생에너지학회:학술대회논문집
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• 한국신재생에너지학회 2011년도 춘계학술대회 초록집
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• pp.167.1-167.1
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• 2011

Sustainable energy generation is becoming extremely imperative due to the expected limitations in current energy resources and to reduce pollution. Especially, because of its considerable energy potential, ocean wave energy has been investigated with regard to power generation. To develop large high power wave generator system, it is important to make a small scale proto type and to test that. Thus the objective of this research is to examine the characteristics of a mechanically excited generator system having small power capacity experimentally. The water reservoir (4 m length, 1.5 m width and 1.8 m depth) having a wave maker to make arbitrary height and period of the water wave was made. The proto type consists of three main parts; a buoy, rack-pinion base one-way mechanism, and a wave generator(Fig.1). The water wave is going up and down and the hexahedron buoy is following the wave. The rack gear attached to the buoy is also going up and down to roll the pinion connected to an electric generator then it produces electricity. The experiments were performed with several conditions of water waves, and the power outputs over 30 W could be measured for some conditions. In future works, to achieve higher performance for the proto type, the effects of primary parameters (buoy shape and mass, etc.) on the system efficiency will be identified.

• Ocean Systems Engineering
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• 제5권3호
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• pp.139-160
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• 2015

The global performance of the 5MW OC4 semisubmersible floating wind turbine in random waves was numerically simulated by using the turbine-floater-mooring fully coupled and time-domain dynamic analysis program FAST-CHARM3D. There have been many papers regarding floating offshore wind turbines but the effects of second-order wave-body interactions on their global performance have rarely been studied. The second-order wave forces are actually small compared to the first-order wave forces, but its effect cannot be ignored when the natural frequencies of a floating system are outside the wave-frequency range. In the case of semi-submersible platform, second-order difference-frequency wave-diffraction forces and moments become important since surge/sway and pitch/roll natural frequencies are lower than those of typical incident waves. The computational effort related to the full second-order diffraction calculation is typically very heavy, so in many cases, the simplified approach called Newman's approximation or first-order-wave-force-only are used. However, it needs to be justified against more complete solutions with full QTF (quadratic transfer function), which is a main subject of the present study. The numerically simulated results for the 5MW OC4 semisubmersible floating wind turbine by FAST-CHARM3D are also extensively compared with the DeepCWind model test results by Technip/NREL/UMaine. The predicted motions and mooring tensions for two white-noise input-wave spectra agree well against the measure values. In this paper, the numerical static-offset and free-decay tests are also conducted to verify the system stiffness, damping, and natural frequencies against the experimental results. They also agree well to verify that the dynamic system modeling is correct to the details. The performance of the simplified approaches instead of using the full QTF are also tested.