• 한국해양학회지
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• v.30 no.6
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• pp.550-564
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• 1995

The temporal and spatial characteristics of wind fields over the neighbouring seas of the Korean peninsula are investigated using 10-years daily wind data during 1978${\sim}$1987 which have been spatially smoothed and low-pass filtered. Long term annual and monthly means are examined for synoptic patterns and spectral analyses are made for temporal variability and spatial coherence. Spatial patterns of the annual mean wind stress and curl have a strong resemblance with those of monthly means during the winter season. Two outstanding periodicities are observed at 1 and 2 cycles per year. The synoptic winds over the study area are highly coherent at both the annual and semi-annual periodicities. However, each basin has its own characteristic spatial pattern. For instance, the prevailing wind during the winter season is northerIy over the northern East Sea (ES), Yellow Sea (YS), and northern East China Sea (ECS), while it is northwesterly over the southern ES and northesterly over the northern ES and southern ECS. At the same time, the wind stress curl is positive over the northern ES and southern ECS, while it is negative over the southern ES, YS and northern ECS. On the other hand, the wind field during the summer season, with its strength being much reduced, is completely different from that during the winter season, and frequent passage of tropical storms provokes large temporal variability over ECS. One remarkable point is that the annual cycle, dominated by the Siberian High, tends to propagate from northeast to southwest, i.e., from northern 25 toward southern ES, YS and ECS, while the semi-annual cycle propagates in the opposite direction, from southwest to northeast. The semi-annual periodicity may reflect development of extratropical cyclones in spring and fall which frequently cross the Korean peninsula. In higher frequencies, there are no dominant periodicities, but local winds over YS and ES are highly correlated for frequencies larger than 0.1 cycles per day and phase difference increases linearly with frequency. This linear increase of phase corresponds to phase speed of 550 and 730 km/d at 0.1 and 0.3 cpd, respectively, The phase speed is apparently coincident with moving speed of extratropical cyclones across the Korean peninsula in the west-east direction.

• The Journal of Engineering Geology
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• v.7 no.2
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• pp.139-149
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• 1997

Electrical resistivity monitoring methods were adopted to detect groundwater table change in alluvium. Numerical modelling test using finite element method(FEM) and field resisfivity monitoring were conducted in the study. The field monitoring data were acquired in the alluvium deposit site in Jeong-Dong Ri, Geum River where pumping test had been conducted continuously for 20 days to make artificial changes of groundwater table. The unit distance of the electrode array was 4m and 21 fixed electrodes were applied in numerical calculation and field data acquisition. "Modified Wenner" and dipole-dipole array configurations were used in the study. The models used in two-dimensional numerical test were designed on the basis of the simplifving geological model of the alluvium in Jeong Dong Ri, Geum River. Numerical test results show that the apparent resistivity pseudosections were changed in the vicinity of the pootion where groundwater table was changed. Furthermore, there are some apparent resistivity changes in the boundary between aquifer and crystalline basement rock which overlays the aquifer. The field monitoring data also give similar results which were observed in numerical tests. From the numerical test using FEM and field resistivity monitoring observations in alluvium site of Geum River, the electrical monitoring method is proved to be a useful tool for detecting groundwater behavior including groundwater table change. There are some limitations, however, in the application of the resistivity method only because the change of groundwater table does not give enough variations in the apparent resistivity pseudosections to estimate the amount of groundwater table change. For the improved detection of groundwater table changes, it is desirable to combine the resistivity method with other geophysical methods that reveal the underground image such as high-resolution seismic and/or ground penetrating radar surveys.

• Korean Journal of Fisheries and Aquatic Sciences
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• v.26 no.4
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• pp.392-400
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• 1993

The present study was accomplished to understand the occurrence and time serial variations of oxygen-deficient watermass in wonmun Bay from 1989 to 1991. From the results of this work, oxygen-deficient water was periodically observed in bottom layer and in Summer in this region. The stratification of water began to develop in Spring and the strong formation of oxygen-deficient water showed in Summer but it gradually disappeared in Autumn. It seems that the occurring and continuing period of very low dissolved oxygen watermass is intensively controlled by meteorological conditions and vortical stratification of water column. On formation of oxygen-deficient watermass, high nutrient concentrations in the bottom layer appear to be due to release of nutrients from bottom sediment. The dissolved inorganic phosphate versus AOU shows two linear curves according to the level of AOU. In the relationships between phosphate and AOU, the gradient of a linear curve over approximately 5mg-AOU/l was significantly large, presumably indicating dissolution of phosphate from the sediment.

• Korean Journal of Fisheries and Aquatic Sciences
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• v.26 no.6
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• pp.567-579
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• 1993

The response of sea levels to a typhoon in the north Japanese coast in the Japan Sea is investigated by using hourly ses level data($1966{\sim}1986$) and a numerical shallow water model with high resolution($5'{\times}5'$). The observed sea level analysis shows (1) progressive waves exist between Simonoseki(SS) and Maizuru(MZ) with the mean phase speed of about 4 m/s during the passage of the typhoon, (2) the phase speed between Sasebo(SB) and HK(Hakata) is slower(about 1.7 m/s), and (3) the maximum sea level at HK is achieved about 0.5 day later than that of SS. In many aspects, the numerical model results correspond well to the above observed features. In the model the progressive waves are identified as a topographic wave with the phase speed of about 4 m/s. Before the typhoon passes through the Korea Strait/ the Tsushima Strait, the wave propagations along the Japanese coast are significantly influenced by the southwestward coastal jet induced by the wind stress parallel to the coast. The waves start to propagate northeastward along the coast when the coastal jet is weakened.

• Journal of Labour Economics
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• v.28 no.1
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• pp.1-28
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• 2005

First, The flow into and out of unemployment has been increasing considerably too since the late 1997. Moreover, about half of job changes involve career changes associated with industrial and occupational changes which workers work for. Workers who switch industries and occupations significantly suffer greater wage losses than observed similar workers who find new jobs in their pre-turnover industry or occupation. These findings imply that labor mobility is more likely to cause losses in accumulated skill of workers. Second, this study compared the wage return to past training when a worker remains with an employer with the wage return to past training when a worker moves to a new employer. Surprisingly, training provided by previous employers has significantly positive wage effect. These findings that the skill acquired by employer- provided training is transferable across some firms. Third, this study finds that the likelihood of sectoral mobility decreases with training received in the current industry. It gives an evidence of the industry- specific training. Based on these findings, this paper suggest the way of dividing the costs of benefits of training among employers within their sector to prevent under-investment in training.

• Proceedings of the Korea Water Resources Association Conference
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• 2017.05a
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• pp.408-408
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• 2017

기후변화에 따른 극한 기후의 시 공간적 변동성과 패턴의 이상변화가 가속화되고 있으며, 이에 따른 물 순환 특성의 변화는 이수, 치수, 환경 그리고 친수 등 다양한 분야에서도 예측할 수 없는 결과를 초래하고 있다. 특히, 치수 및 이수 등 국내 수자원 관리의 대부분을 담당하고 있는 다목적댐 운영에서도 기후변화에 따른 유입량의 불확실성 증가로 안정적인 용수공급에 대한 어려움이 점차 증가하고 있는 추세이다. 유역 내의 수문학적 반응은 기상 및 지표 수문 인자의 물리적 상호메카니즘에 의해 발생하게 된다. 특히, 강우, 기온, 습도, 바람 등 기상학적 인자들은 유역 내의 수문 변동성에 직 간접적으로 영향을 주는 대표적인 인자이며, 이들 기상인자의 변동 특성을 반영하기 위한 기후지수(Climate Index, CI)는 지표수문인자인 유출과의 상관관계 분석에 유용하게 활용될 수 있다. 본 연구에서는 낙동강 유역 다목적댐을 대상으로 AR5 RCP 시나리오 기반의 기상인자에 대한 기후지수(CI)를 산정하고 다목적댐 유입량과의 상관성을 분석하였다. 대상유역의 기상 및 유입량 관측자료(1976-2005)는 기상청과 국가수자원관리종합정보시스템(WAMIS)를 이용하였으며, AR5 RCP 시나리오 기반의 유입량 자료(2005-2099)는 통계적 기법(QDM)으로 상세화된 기상자료를 입력인자로 수문모형(PRMS)을 통해 산정하였다. 또한, 기후지수(CI)와 유출지수(Standardized Streamflow Index, SSI)의 상관성 분석을 위해 Pearson 적률상관 분석방법을 적용하였으며, 통계적 유의성 검증은 Student t 검정방법을 적용하였다. 본 연구의 방법론과 결과는 기후변화에 따른 다목적댐 안정적인 용수공급을 위한 다양한 기술개발 시 기초자료로 활용될 수 있을 것으로 기대된다.

• Journal of the Korean Society of Marine Environment & Safety
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• v.22 no.5
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• pp.508-520
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• 2016

In this study, variations in water temperature after the passage of typhoons in Korean waters from 2009-2015 were analyzed. Sea surface temperature (SST) images derived from satellite remote sensing data were used, and water temperature information came from real-time mooring buoys at Yangyang, Gangneung, Samcheok and Yeoungdeok, while wind data was supplied by the Korea Meteorological Administration. Differences in SST observed before and after the passage of a typhoon using the SST images were found to be affected by wind direction as well as hot and cool seasonal tendencies. Coastal water temperatures of the eastern part of the Korean peninsula, located to the right of a typhoon, as in the case of typhoons Muifa, Chanhom, Nakri and Tembin, were lowered by a coastal upwelling system from southerly winds across the water's surface at depths of 15m and 25m. In particular, typhoons Chanhom and Tembin decreased water temperatures by about $8-11^{\circ}C$ and $16^{\circ}C$, respectively. However, temperatures to the left of the typhoons were increased by a downwelling of offshore seawater with a high temperature through the mid and lower seawater layers. After the passage of the typhoons, further mixing of seawater at a higher or lower temperature due to southerly or northerly winds, according to the context, lasted for 1-2 or 4 days, respectively.

• Proceedings of the KIPE Conference
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• 2011.11a
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• pp.273-274
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• 2011

최근에는 풍속변화에 대응하여 최대전력을 발생할 수 있는 가변속 풍력발전 시스템에 대한 연구가 활발히 진행 중이며 국내의 지형적 조건에 따른 바람의 영향으로 풍력발전 시스템의 MPPT제어가 반드시 필요하다. 종래의 풍력발전 MPPT 제어는 풍속변화에 대한 응답속도 등에 대한 문제점이 나타난다. 따라서 본 논문에서는 파라미터 변동에 대해 강인성 제어가 가능한 FLC(Fuzzy Logic Control)을 기반으로 한 풍력발전시스템의 MPPT 제어를 제안하고, 시뮬레이션 결과를 통하여 타당성을 입증한다.

• The Transactions of the Korean Institute of Power Electronics
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• v.4 no.2
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• pp.175-183
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• 1999

For fast response of the dc output voltage in P\hi1'v1 converter, it is desirable that the relation of power balance of the i input and output terminals is introduced to the system modeling. In this case, controller desi밍1 is not easy since the m model is nonlinear. In this paper, a nonlinear control them${\gamma}$ using input-output feedback linearization is used to solve t the nonlinear problem of the system. By nonlinear control. the voltage transient response can be faster, and it is also p possible to control the output voltage to be constant with smaller output filter capacitance for load disturbance.

• The Korean Journal of Financial Studies
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• v.8 no.1
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• pp.253-276
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• 2002

본 논문에서는 전자화폐의 보급이 중앙은행과 은행을 통한 결제시스템에 미치는 영향을 분석하는데 기초가 되는 화폐론적인 분석과 함께 전자적인 결제수단의 보급이 신용창조와 소비자의 화폐수요에 미치는 영향과 아울러 결제시스템으로서의 은행의 독점적인 지위에의 영향에 대해서 분석하였다. 본 연구의 결과로서 전자화폐는 현재로서는 현금과 예금을 완전히 대체할 수 있는 화폐로서가 아니라 어디까지나 현금과 예금에 기초를 두고 있는 결제수단의 하나에 지나지 않는다는 것이 밝혀졌다. 즉 은행부채의 하나의 형태라고 규정지을 수 있다. 따라서 현 발전단계 수준의 전자화폐는 중앙은행의 통화량조절 능력과 은행의 신용창조에 의한 통화창출과 결제시스템으로서의 독점적인 지위에는 그다지 영향을 미치지 않으리라고 판단된다. 향후 전자화폐의 발전에 능동적으로 대처하기 위해서는 전자화폐에 대한 정확한 이해와 함께 현재의 신용제도가 안고 있는 제반 문제를 해결하여야 할 것이다. 특히 전자화폐의 보급으로 통화량의 변동성이 커지게 되므로 통화정책에 있어서는 통화량 관리에 중점을 두기보다는 금리의 기능을 최대한 이용하는 정책으로의 전환이 바람직할 것으로 판단된다.