• Journal of Astronomy and Space Sciences
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• 제37권1호
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• pp.69-75
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• 2020

We analyze the observations of temperature and ozone measured by the Microwave Limb Sounder (MLS) during the period of 2005-2016, to investigate the vertical structures of temperature and ozone in the stratosphere and mesosphere during stratospheric sudden warming (SSW). We compute the height profiles of the correlation coefficients between 55 height levels of MLS temperature anomalies and compare them with the results of Whole Atmosphere Community Climate Model simulations for three major SSWs. We also construct the temperature and ozone anomalies for the events to investigate the changes in the temperature and ozone distributions with height. There seems to always be a relatively weak but broad negative correlation between the temperature anomaly at 10 hPa and temperature anomalies over the entire mesosphere during the period before SSW events. However, this pattern gets stronger in the lower mesosphere but becomes a positive correlation in the upper mesosphere and lower thermosphere after the onset of SSW. We also found that the temperatures from the simulations show a similar trend to the observational results but with smaller variations and the transition height from negative to positive correlation in the mesosphere is much lower in the simulation than in the actual observations.

• Ocean and Polar Research
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• 제26권3호
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• pp.401-414
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• 2004

Temperature, salinity, alkalinity, pH, nutrient, chlorophyll, and iron were measured within the upper 250m water column around the Antarctic Polar Front in the Scotia Sea from late November to early December 2001. Temperature and salinity showed a rapid change across the Polar Front, and the temperature minimum layer existed only in the southern area of the Polar Front. Total $CO_2$ and nutrient concentrations were relatively high and increased rapidly with water depth in the southern area of the Polar Front, which was resulted from upwelling of the Antarctic deep water containing high concentrations of total $CO_2$ and nutrient. ${\Delta}C:{\Delta}N:{\Delat}P$ ratios measured in the norhem and southern areas of the Polar Front were 75:11.4:1 and 84:12.5:1, respectively, which were lower than the Redfield ratio. ${\Delta}Si:{\Delta}N$ ratio (3.65) measured in the southern area of the Polar Front was two times higher than that (1.95) in the northern area. These two ratios were higher than the ratio (1.0) measured in the temperate and tropical oceans. Chlorophyll concentrations were extremely high in the area of $59^{\circ}{\sim}60^{\circ}S$, which was attributed to favorable environmental conditions for phytoplankton growth in this area, such as sufficient iron, high water column stability, and high silicate concentration.

• Ocean and Polar Research
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• 제27권4호
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• pp.443-450
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• 2005

The ratio of breeding pairs of brown skuas (Catharacta lonnbergi), south polar skuas (C. maccormicki) and mixed species pairs between Barton and Weaver peninsulas remained the same $(X^2-test,\;X^2=0,503,\;df=2,\;p=0.778)$. The nests of skuas were clustered on Barton, whereas they were distributed randomly on the Weaver peninsula. The distance between brown skua nests, and that of mixed species pair nests were longer than those of south polar skua nests. Brown skua nests were distributed along the coast. Whereas, the nests of mixed species pairs and south polar skuas were found more frequently inland (Kruskal-Wallis, $X^2=11.631$, df=2, p<0.005). There was no interspecific difference in the distances between skua nests and Penguin rookery at Barton (Kruskal-Wallis, $X^2=2.153$, df=2, p=0.341) or at King Sejong Station (ANOVA, F=1.483, df=2, p=0.229). In general, skuas prefer lower locales (<125m above sea level) for their nest building sites. Brown skua nests were distributed mainly on the beach, whereas south polar skua were distributed on the predominant periglacial landforms and till areas $(X^2-test,\;X^2=24.988,\;df=8,\;p<0.005)$.

• 대한원격탐사학회지
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• 제34권6_2호
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• pp.1155-1163
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• 2018

최근 기후변화에 의한 극지의 변화 및 역할에 대해 많은 관심이 집중되고 있으며, 다양한 플랫폼을 이용한 연구들이 극지에서 진행되고 있다. 그 중 원격탐사를 이용한 북극 빙권 정보 모니터링은 여러 과학적 활동 중 가장 중요한 관측 역할을 수행하고 있다. 본 특별호는 극지연구소에서 수행 중인 극지 환경 변화 원격탐사 모니터링에 대한 여러 연구를 소개한다. 극지 원격탐사연구에 대한 대외적인 환경변화와 국내 극지 원격탐사의 현 주소 파악과 함께 극지원격탐사의 역할에 대한 정보 공유에 본 특별호가 기여하길 기대한다. 더불어 지속적인 극지원격탐사 분야 발굴 및 국가적인 지원을 이끌어 내기 위해 국내 원격탐사 전문가들의 노력을 기대한다.

• 한국정보통신학회:학술대회논문집
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• 한국해양정보통신학회 2003년도 춘계종합학술대회
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• pp.255-258
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• 2003

디지털화 된 의료영상에서의 데이터 인증 및 변형 여부의 판별을 위해서 디지털 워터마킹을 사용한다. Fourier변환과 Log-Polar변환을 이용한 Fourier-Mellin기법은 영상의 RST변환에 불변한 특징을 가진다. 하지만 실질적인 구현을 위해서는 화소위치가 일치하지 않는 것에 따라 영상값을 보간해야 하는 것과 그에 따른 워터마크의 데이터 손실, 계산량 증가, 원영상의 화질 저하를 해결해야한다. Polar좌표 변환의 손실을 없애기 위해서 Look up table을 사용하였다. 진단이후, 의료영상의 ROI 영역을 중심으로 Polar좌표 변환과 Discrete fourier변환을 하였다. 주파수 진폭성분의 대칭성을 유지하면서, 가우시안 분포의 랜덤 벡터와 이진 영상을 워터마크로 삽입하여 다양한 조건 하에서의 결과를 관찰하였다.

• 대한전자공학회논문지TC
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• 제48권4호
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• pp.24-36
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• 2011

본 논문에서는 Arikan이 제안했던 극 부호의 부호화 및 복호화의 대수적 식을 개선하여 이진 이산 무기억 대칭 채널에서 연속 제거 복호 알고리즘을 이용한 극 부호의 채널의 합성과 분리를 확인했다. 이진 이산 무기억 대칭 채널 W에서 양극화 행렬 ${G_2}^{{\otimes}n}$을 통하여 블록 길이 $2^n$인 극 부호를 효과적으로 구성하여 정보 비트를 전송할 수 있다. 특히, $N{\geq}2$일 때, Arikan 부호의 복잡도 O($Nlog_2N$)이다. 극 부호가 향후 다중점 통신의 문제에 대한 하나의 대안이 될 수 있다는 것을 확인하였다.

• 한국전기전자재료학회:학술대회논문집
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• 한국전기전자재료학회 2003년도 하계학술대회 논문집 Vol.4 No.1
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• pp.506-509
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• 2003

In this paper, the $\Phi$-q-n pattern and average discharge power of silicone rubber have investigated effect of inter impurities. It's changed impurities by silicone oil, water and copper. Applied voltage is AC 3, 4, 4.5, 5, 5.5[kV]. And data acquisition time is 10 second(600 cycles). These results suggest that partial discharge(PD) is shower negative polar than positive polar at 3[kV]. Positive polar's PD value increased with increase of applied voltage. The Conductivities expressed same $\Phi$-q-n pattern in positive polar and negative polar at phase region.

• Ocean and Polar Research
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• 제24권3호
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• pp.301-311
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• 2002

We used diatom and porewater data of two piston cores from the central subbasin and one from the western subbasin in the Bransfield Strait in the northern Antarctic Peninsula to elucidate the depositional mechanism of the layered diatom ooze. The layered diatom ooze is characterized by an abundance of organic carbon, biogenic silica, sulfde sulfur, and lower porewater sulfate concentration. This lack of pore-water sulfate concentration in the diatom ooze interval may reflect development of reducing micro-environment in which bacterially mediated sulfate reduction occurred. The negative relationship between the total organic carbon and sulfate contents, however, indicates that sulfate reduction was partly taking place but does not control organic carbon preservation in this unit. Rather, well-preserved Chaetoceros resting spores in the layered diatom ooze indicate a rapid sedimentation of the diatom as a result of repetitive iceedge blooms on the Bransfield shelf during the cold period (around 2500 yrs BP) when the permanent seaice existed on the shelf, During this period, it is expected that the downslope-flowing cold and dense water was also formed on the Bransfield shelf as a result of sea ice formation, playing an important role for the formation of layered diatom ooze in the Bransfield subbasins.

• 한국통신학회논문지
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• 제36권6C호
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• pp.337-342
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• 2011

2009년 Arikan에 의해 처음 제안된 극 부호(polar codes)는 실용적인 부 복호화 복잡도로 채널 용량을 달성하는 것이 종영된 채널 부호이다. 채널 양극화(channel polarization) 현상을 이용하는 극 부호는 현재 보안 및 데이터 압축 등에 응용되어 활발히 연구되고 있다. 본 논문에서는 극 부호의 실제 통신 시스템 적용을 고려하여, 유한한 길이와 고정 부호율을 갖는 극 부호의 설계 방법을 제안한다. 그리고 모의실험을 통하여 경험적으로 찾아낸 가장 우수한 성능을 보이는 극 부호의 성능과 설계 방법을 제시한다.

• 한국환경과학회지
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• 제2권1호
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• pp.27-42
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• 1993

Based on the Results of Marine Meteorological and Oceanographical Observations during 1966∼1987 and the Ten-day Marine Report during 1970∼1989 by Japan Meteorological Agency, the possible area where the Japan Sea Proper Water (JSPW) can be formed is investigated by analyzing the distribution of water types in the Japan Sea. The Japan Sea can be divided into three subareas of Northern Cold Water(NCW), Polar Front(PF) and Tsushima Warm Current (TWC) by the Polar Front identified by a 6℃ isothermal line at the sea surface in vinter. Mean position of the Polar Front is approximately parallel to the latitude 39∼40。N. The standard deviation of the Polar Front from the mean position of about 130km width is the smallest in the region between 136。E and 138。E where the Polar Front is very stable, because the branches of the Tsushima Current are converging in this region. However, standard deviations are about 180∼250km near the Korean peninsula and the Tsugaru Strait due to greater variability of warm currents. In the NCW area north of 40∼30。N and west of 138。E, the water types of the sea surface to the loom depth are similar to those of the JSPW. This fact indicates that the surface layer of the NCW area is the possible region of the JSPW formation in winter.