• Ocean and Polar Research
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• 제44권3호
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• pp.191-207
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• 2022

Using the results of CTD casts made in Spring from 2017 to 2021, in this study we investigated the water mass distribution and occurrence of temperature inversion in the western seas of Jeju Island in spring. The distribution of water masses was characterized by cold and fresh water in the northwest and warm and saline water in the southeast, forming a strong thermohaline front running in the southwest-to-northeast direction. Strong temperature inversion mainly occurred in the frontal boundary when the cold water intrudes beneath the warm water at depths of 30-50 m. Analysis of the mixing ratio demonstrated that Jeju Warm Water is dominantly distributed in the western seas of Jeju Island, but its ratio can be modified depending on the southward extension of Yellow Sea Cold Water (YSCW). Results of in situ measurement showed that in 2020, the YSCW largely expanded to the western seas of Jeju Island, occupying approximately 40 % of the mixing ratio. Due to the expansion of YSCW, a strong thermohaline front was formed in the study area, thereby causing thick and strong temperature inversion. On the other hand, in 2018 the mixing ratio of YSCW was minimum (~18%) during the study period of 2017-2021, and thus a relatively weak frontal boundary was formed, without the occurrence of temperature inversion. The observational results also suggest that the interannual changes of water mass distribution and the associated temperature inversion in the western seas of Jeju Island are closely related with wind-driven Yellow Sea circulation in spring, which is the summer monsoon transition period.

• Ocean and Polar Research
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• 제27권3호
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• pp.277-288
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• 2005

Spatial distribution and vertical structures of water masses around the Antarctic continental margin are described using synthesized hydrographic data. Antarctic Surface Water (AASW) over the shelf regime is distinguished from underlying other water masses by the cut-off salinity, varying from approximately 34.35 to 34.45 around Antarctica. Shelf water, characterized by salinity greater than the cut-off salinity and potential temperature less than $-17^{\circ}C$, is observed on the Ross Sea, off George V Land, off Wilkes Land, the Amery Basin, and the Weddell Sea, but in some shelves AASW occupies the entire shelf. Lower Circumpolar Deep Water is present everywhere around the Antarctic oceanic regime and in some places it mixes with Shelf Water, producing Antarctic Slope Front Water (ASFW). ASFW, characterized by potential temperature less than about $0^{\circ}C$ and greater than $-17^{\circ}C$, and salinity greater than the cut-off salinity, is found everywhere around Antarctica except in the Bellingshausen-Amundsen sector. The presence of different water masses over the Antarctic shelves and shelf edges produces mainly three types of water mass stratifications: no significant meridional property gradient in the Bellingshausen and Amundsen Seas, single property gradient where ASFW presents, and a V-shaped front where Shelf Water exists.

• 한국전기전자재료학회논문지
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• 제26권10호
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• pp.760-765
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• 2013

PID (potential induced degradation) of PV module is the degradation of module due to the high potential difference between the front surface of solar cells and ground when PV modules operate under high humidity and temperature conditions. PID is generally derived from the positive sodium ions in front glass that are accumulated on P-type solar cells. Therefore, some papers for the electrical characteristic of only front components as glass, EVA sheet, solar cell under PID generation condition were revealed. In this paper, we analyzed the different outputs of module with PID by considering the all parts of module including the back side elements such as glass, back sheet. Mini modules with one solar cell were fabricated with the various parts on front and back sided of module. To generate PID of module in a short time, the all modules were applied.1,000 V in $85^{\circ}C$, 85% RH. The outputs, dark IV curves and EL images of all modules before and after experiments were also measured to confirm the main components of module for PID generation. From the measured results, the outputs of all modules with front glass were remarkably reduced and the performances of modules with back and front glass were greatly deteriorated. We suggest that the obtained data could be used to reduce the PID phenomenon of diverse modules such as conventional module and BIPV (building integrated photovoltaic) module.

• 한국전자파학회논문지
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• 제23권8호
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• pp.958-966
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• 2012

본 논문에서는 저온 동시 소성 세라믹(Low Temperature Co-fired Ceramic: LTCC) 기술을 사용하여 블루투스와 WiFi에서 동작하는 무선 전단부 모듈(RF Front-end Module)을 설계, 구현하였다. 무선 전단부 모듈은 2.4/5 GHz 대역 다이플렉서와 2 GHz 대역 발룬, 5 GHz 대역 발룬, 그리고 송 수신용 SPDT 스위치와 SP3T 스위치로 구성되어 있다. LTCC의 설계에 있어, 적층 구조의 특성으로 인해 발생되는 예상 기생 성분은 시뮬레이션을 활용하여 설계하였다. 제작한 무선 전단부 모듈은 내부 접지(inner ground) 3개 층을 포함하여 총 13개 패턴으로 구성되었으며, 무선 전단부 모듈의 크기는 $3.0mm{\times}3.7mm{\times}0.66mm$이다.

• Nuclear Engineering and Technology
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• 제54권3호
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• pp.1085-1097
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• 2022

A printed circuit steam generator (PCSG) is being considered as the component for pressurized water reactor (PWR) type small modular reactor (SMR) that can further reduce the physical size of the system. Since a steam generator in many PWR-type SMR generates superheated steam, it is expected that dryout front oscillation can potentially cause thermal fatigue failure due to cyclic thermal stresses induced by the transition in boiling regimes between convective evaporation and film boiling. To investigate the fatigue issue of a PCSG, a reference PCSG is designed in this study first using an in-house PCSG design tool. For the stress analysis, a finite element method analysis model is developed to obtain the temperature and stress fields of the designed PCSG. Fatigue estimation is performed based on ASME Boiler and pressure vessel code to identify the major parameters influencing the fatigue life time originating from the dryout front oscillation. As a result of this study, the limit on the temperature difference between the hot side and cold side fluids is obtained. Moreover, it is found that the heat transfer coefficient of convective evaporation and film boiling regimes play an essential role in the fatigue life cycle as well as the temperature difference.

• 한국해양학회지
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• 제25권2호
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• pp.84-95
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• 1990

CTD, 해류계, 인공위성 영상사진을 이용하여 황해 중부의 조석전선 주변역을 조사 한 결과 몇 가지 물리적 특성을 알 수 있었다. 전선은 태안반도 끝 부분을 중심으로 하여 4월 중에 태양열에 의한 해표면 가열과 함께 나타나기 시작하여 8월에 가장 뚜렷 하며 11월에는 표층냉각과 함께 소멸한다. 전선의 북측에서는 전선을 가로지르는 조류 에 의하여 수온 염분의 조석주기 변화가 나타남으로써 전선구조를 보여준다. 경기만에 서 나타나는 전선은 통최상의 조석전선과 달리 한강에서 유출된 담수와 외양수의 만남 에 의하여 형성된다. 표층냉수의 중심에서는 조석혼합역이 연안으로부터 약 50 km 외 양하지 분포한다. 전선의 남측에서도 전선의 구조는 비슷하나 전반적으로 혼합 정도가 약하게 나타난다. 이 연안 혼합역의 연안쪽에서는 금강유출된 담수에 의하여 염분전선 이 좁은 범위에서 흥성된다. 이 염분전선 부근의 일부에서는 용승과 같은 현상이 관측 되었다.

• 대한원격탐사학회지
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• 제34권6_2호
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• pp.1179-1192
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• 2018

이 연구는 남빙양(Southern Ocean)에서 나타나는 주된 전선(Front)들 중에 남극 극 전선(Antarctic Polar Front; PF)을 탐지하기 위하여 위성 기반 해수면 온도(sea surface temperature)와 해수면 고도(sea surface height) 자료를 복합적으로 사용하였다. 정확한 PF 탐지를 위하여 일별 SST와 SSH 자료를 각각 기반으로 하여 베이지안 결정 이론(Bayesian decision theory)을 적용하였으며, 이를 근거로 전선/비전선의 신호를 격자 별로 분류하였다. 이후, 시공간적인 합성을 통하여 일차적인 노이즈(noise) 제거 및 지리학적 연결성을 보완하였다. 그러나 이들 과정을 수행하고도 여전히 잔존하는 일부 노이즈를 제거하기 위하여 해빙 및 연안 마스킹(masking)을 수행하였다. 또한 모폴로지 연산(morphology operation)을 통하여 지류 성분을 최대한으로 배제하고 주된 전선 성분만을 추출하였다. 최종적으로 선택된 전선 격자 들에서 PF의 특징을 나타낼 수 있도록 가장 최남단의 전선만을 선택하여 평활 스플라인(smoothing spline) 최적화 방식을 통해 선 형태의 월별 PF를 산출하였다. 산출된 PF는 기존의 연구에서 제시한 PF의 위치와 상당히 유사한 것으로 나타났으며, 특히 바닥 지형에 따라 상당 부분 결정되는 PF의 변화를 잘 모사하는 것으로 보인다. 로스해 주변(${\sim}180^{\circ}W$)과 호주 이남의 해역($120^{\circ}E-140^{\circ}E$)은 PF의 위치에 대한 계절적 변동이 높게 나타나며, 그러한 변동이 기존에 제시된 결과와 상당히 유사한 경향을 지닌다. 그러므로 이 연구에서 산출된 PF의 위치에 대한 탐지 결과가 향후 장기적 관점에서 수행될 연구에 사용될 수 있는 가치를 지닐 것으로 기대한다.

• 한국축산시설환경학회지
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• 제20권4호
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• pp.155-160
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• 2014

This study was researched for use by data for the improvement of ventilation system of optimum environmental control systems. The ventilation system for windowless swine housing was installed negative pressure system that circular pipe duct for inlet was installed on the ceiling and axial flow fan for exhaust was installed on the sidewall. The temperatures in the pen was measured using infrared thermography camera and thermocouple with data-logger. The temperature measurement points was selected by infrared thermography camera is alley (G), inlet (A), front-upper (B), front-lower (C), rear-upper (D), rear-lower (E), forward fan (F). The temperature measured at those selected points for temperature distribution was $28^{\circ}C$ that was maintained setting temperature in suitably. The temperature deviations of F point and A~E points in windowless swine housing was less then average $0.5^{\circ}C$. The result of air velocity of measured points was suitable to the breeding of pigs.

• 한국전자파학회논문지
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• 제21권4호
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• pp.362-370
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• 2010

본 논문에서는 저온 동시 소성 세라믹(Low Temperature Co-fired Ceramic: LTCC) 기술을 이용하여 Wi-Fi와 WiMAX에 적용할 수 있는 무선 전단부(RF front-end) 모듈을 구현하였다. 무선 전단부 모듈은 3개의 LTCC 대역 통과 여파기와 FBAR 여파기, embedded된 정합 회로, Wi-Fi와 WiMAX 모드 선택용 SPDT 스위치, 송 수신택용 SPDT 스위치 그리고 대역 선택용 SP4T 스위치로 구성되어 있다. 모드 선택용 SPDT 스위치의 DC block 패시터를 실장하기 위한 패드 패턴에서 LTCC의 적층 구조의 특성으로 인해 0.2~0.3 pF의 값을 가지는 기생 성분이 생기게 된다. 이러한 기생 성분은 설계된 회로의 매칭을 틀어지게 만들어 결과적으로 모듈의 전기적 성능을 저하시킨다. 따라서 기생 커패시터 성분에 상응하는 칩 인덕터를 DC block 커패시터 패드 패턴과 병렬로 달아서 기생 성분을 상쇄하여 모듈의 특성을 최적화하였다. 제작된 무선 전단부 모듈은 내부 접지(inner GND) 3개 층을 포함한 12층으로 설계되었으며, 크기는 $6.0mm{\times}6.0mm{\times}0.728mm$이다.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume II
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• pp.740-743
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• 2006

We identify two distinct finer-scale frontal bands: 'Mainland China Coastal Front' (MCCF) and 'Kuroshio Front' (KF). The MCCF is along the 50-m isobath with large temperature gradient. The front is a boundary between the Mainland China Coastal Current and the offshore shelf waters. On the other hand, the KF is extending from the northeastern coast of Taiwan toward the northeast and into the shelf of south ECS. It forms a broad semicircle-shape and curving along 100-m isobath, it also deviates from eastward at around 26.5N-122E and leaves the shelf of ECS. This front should be the boundary between the Kuroshio water and the other shelf waters.