• Bulletin of the Korean Space Science Society
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• 2009.04a
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• pp.44.2-45
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• 2009

• Ocean and Polar Research
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• v.38 no.3
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• pp.235-245
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• 2016

The purpose of this study is to estimate the Willingness To Payment (WTP) of sea-anglers regarding the increase in the abundance of fish resources resulting from the Korean vessel buy-back program using the contingent valuation method. Data was collected through sample surveys of 352 sea-anglers across the nation in 2015. If a 20% increase in the abundance of fish resources resulted from the vessel buy-back program, WTP estimates of sea-anglers per recreational fishing trip were 9,570 won on truncated mean, 16,528 won on mean, and 35,830 won on median, respectively. Additionally, when the number of annual total recreational fishing trips in Korea were estimated as 22,700 thousand trips, the annual increase in national welfare through recreational fishing was estimated to be 217.2 billion won on the truncated mean, 375.2 billion won on the mean, and 813.3 billion won on the median, respectively.

• Ocean and Polar Research
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• v.23 no.3
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• pp.223-242
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• 2001

This paper presents the depth-mean monthly variation in the circulation of the Yellow Sea and the East China Sea computed using a robust diagnostic model. The mixed three-dimensional finite-difference Galerkin function model developed by Lee et at. (2000, 2001) has been extended to take into account baroclinic effects and then used to calculate the depth-mean flow fields as part of the results. In addition to M2 tide and oceanic flows previously considered, the model has been driven by the monthly mean wind stresses from Na and Seo (1998), the density gradient calculated based on by GDEM data set released by US Navy. Model results are very encouraging in that many of observed features including Jeju Cyclonic Gyre and frontal eddies along the shelfside of the Kuroshio main stream and west of Kyushu, are satisfactorily reproduced and are expected to be of value in interpreting observations in various oceanograhic disciplines.

• Korean Journal of Remote Sensing
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• v.34 no.6_2
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• pp.1179-1192
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• 2018

In order to detect the Antarctic Polar Front (PF) among the main fronts in the Southern Ocean, this study is based on the combinations of satellite-based sea surface temperature (SST) and height (SSH) observations. For accurate PF detection, we classified the signals as front or non-front grids based on the Bayesian decision theory from daily SST and SSH datasets, and then spatio-temporal synthesis has been performed to remove primary noises and to supplement geographical connectivity of the front grids. In addition, sea ice and coastal masking were employed in order to remove the noise that still remains even after performing the processes and morphology operations. Finally, we selected only the southernmost grids, which can be considered as fronts and determined as the monthly PF by a linear smoothing spline optimization method. The mean positions of PF in this study are very similar to those of the PFs reported by the previous studies, and it is likely to be well represents PF formation along the bottom topography known as one of the major influences of the PF maintenance. The seasonal variation in the positions of PF is high in the Ross Sea sector (${\sim}180^{\circ}W$), and Australia sector ($120^{\circ}E-140^{\circ}E$), and these variations are quite similar to the previous studies. Therefore, it is expected that the detection approach for the PF position applied in this study and the final composite have a value that can be used in related research to be carried out on the long term time-scale.

• Ocean and Polar Research
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• v.24 no.2
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• pp.147-152
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• 2002

Seasonal and interannual variation of volume transport through the La-Perouse Strait were estimated using the difference of sea level observed at Krillion of Sakhalin, Russia, and Wakkanai of Hokkaido, Japan, during the period of 1975-1988. Historical sea level measurements between Russian and Japanese tide gauge data were normalized using an independent direct volume transport measurement. Volume transport from the East Sea (Sea of Japan) to the Sea of Okhotsk varied from -0.01 to 1.18 Sv with an annual mean value of 0.61 Sv. Monthly water transport rates showed a unimodal distribution with its maximum occurring in summer (August) and minimum in winter (December-February). The annual mean volume transport varied from 0.2 to 0.8 Sv during the period of 1975-1988 with the maximum variance of 0.6 Sv.

• Journal of the Korean Society of Food Science and Nutrition
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• v.13 no.3
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• pp.326-333
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• 1984

The oxidation rate of krill lipids is very slow and no peroxides are accumulated even after long storage. By means of various chromatographic techniques and mass spectrophotometry, the primary antioxidant has been identified as ${\alpha}$-tocopherol. The phospholipid fractions did not show any antioxidative activity but peroxide-decomposing properties of total lipids depended upon the phospholipid contents. The peroxide-decomposing activities of phospholipids were due to the presence of polar materials generated during the storage. The most peroxide-decomposing fractions of oxidized krill lecithin by DEAE-cellulose column chromatography was low-molecule fraction (mean molecular weight: 182) and high-molecule fraction (mean molecular weight: 1942) was the next. The separation of peroxide-decomposing properties from low-molecule fraction was achieved by partitioning between chloroform and methanol/water. The methanol/water fraction showed strong peroxide-decomposing activities and main component of this fraction was assumed hydroxyamine compounds derived from choline.

• Journal of the Korean Society of Clothing and Textiles
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• v.15 no.4 s.40
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• pp.431-435
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• 1991

The dispersion and Poiar force components of the surface free energy of PET fibers untreated and treated with hydrophilic chemicals, such as nonionic-soil release polymer (SRP), anionic, nonionic and hydrophilic silicone, were determined using harmonic-mean and geometric-mean methods. Contact angles of water and methylene iodide on the fibers were determined from the adhesion tensions using tensiometric method. Fibers treated with hydrophilic chemicals have the increased polar force component and the decreased dispersion force component. The adhesion tensions of triolein for the hydrophilic treated fibers were smaller than that for untreated fiber.

• Korean Journal of Remote Sensing
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• v.24 no.5
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• pp.473-481
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• 2008

This paper presents an approach to Back-propagation and Radial Basis Function neural network method with various training set for automatic vehicle detection from aerial images. The initial extraction of candidate object is based on Mean-shift algorithm with symmetric property of a vehicle structure. By fusing the density and the symmetry, the method can remove the ambiguous objects and reduce the cost of processing in the next stage. To extract features from the detected object, we describe the object as a log-polar shape histogram using edge strengths of object and represent the orientation and distance from its center. The spatial histogram is used for calculating the momentum of object and compensating the direction of object. BPNN and RBFNN are applied to verify the object as a vehicle using a variety of non-car training sets. The proposed algorithm shows the results which are according to the training data. By comparing the training sets, advantages and disadvantages of them have been discussed.

• Proceedings of the Korean Society of Embryo Transfer Conference
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• 2002.11a
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• pp.79-79
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• 2002

본 연구에서는 in vitro에서 성숙된 난자의 핵성숙(Polar Body extrusion)에 소요되는 시간과 배반포 단계로의 발달능력 사이의 관계를 비교하여 조기에 발달능력을 가진 embryo를 선발할 수 있는 IVP 체계를 개발하고자 하였으며 in vitro maturation(IVM)에 따른 first polar body(PB) 형성, IVM과 IVF 시간이 oocyte의 발달에 미치는 영향과 생산된 배반포의 세포수를 평가하였다. IVM은 TCM199 배양액을 사용하였고 in vitro fertilization(IVF)은 Fer -TALP용액을 사용하였으며 in vitro culture(IVC)는 CRlaa 배양액을 사용하여 2일까지는 0.3% BSA를 3일 부터는 10%FBS와 bovine oviduct epithelial cell을 첨가하여 배양하였다. IVM 시간에 따른 PB의 출현율은 0hr(0%), 6hr(0%), 12hr(0%), 14hr(8.7%), 16hr(40.5%), 18hr(48.0%), 20hr(65%), 22(68%) 그리고 24hr(74.5%)을 보였으며 IVM 시간에 따른 cleavage 및 8cell 발달율 사이에는 유의적인 차이가 없었으나 배반포(BL) 및 8cell에서 배반포로 발달률은 18시간(BL 31$\pm$6, BL/8cell 82 $\pm$5%)에서 가장 높게 나타났으며 24시간(BL 17$\pm$2, BL/8cell 60$\pm$8%)과 유의적인 차이를 보였다(P<0.05). IVC 7일째 배반포의 총세포수와 trophoblast(TE) 세포수는 IVM 18시간(mean$\pm$S.E.; total: 131.1$\pm$34.0, TE: 97.6$\pm$29.6)에서 24시간(total: 112.2$\pm$17.5, TE: 80.1$\pm$15.6)보다 유의하게 많은 것으로 나왔으나(P<0.05) 7일째의 inner cell mass(ICM) 숫자(18hr 33.5$\pm$12.8 vs 24hr 32.1$\pm$12.0)와 8일째 ICM, TE 그리고 총 세포수에는 유의성 있는 차이가 없었다. IVM 18시간에서 PB 형성과 8cell 발달률 사이에 높은 상관성을 보였고 배반포 및 8cell에서 배반포 단계로 높은 발달률을 보였으며 생산된 배반포의 TE 숫자와 총 세포수가 유의하게 많은 것으로 나타났다. 따라서 IVM 18시간 실시하였을 경우 보다 많은 세포수를 가진 배반포 발달 가능성이 높은 embryo를 조기에 선발 가능할 것으로 사료된다.

• Ocean and Polar Research
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• v.34 no.1
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• pp.73-83
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• 2012

Antarctica is very sensitive to climate change but the number of stations is not sufficient to accurately analyze climate change in this regoin. Model reanalysis data supplements the lack of observation and can be used as long term data to verify climate change. In this study, the 20CR (Twentieth Century Reanalysis) Project data from NCEP/NCAR and monthly mean data (temperature, solar radiation and longwave radiation) from 1871 to 2008, was used to analyze the temperature trend and change in radiation. The 20CR data was used to validate the observation data from Antarctica since 1950 and the correlation coefficients between these data were determined to be over 0.95 at all stations. The temperature increased by approximately $0.23^{\circ}C$/decade during the study period and over $0.20^{\circ}C$/decade over all of the months. This increasing trend was observed throughout the Antarctica and a slight increase was observed in the Antarctic Peninsula. In addition, solar radiation (surface) and longwave radiation (surface and top of atmosphere) trends correlated with the increase in temperature. As a result, outgoing longwave radiation at the surface is attenuated by atmospheric water vapor or clouds and radiation at the top of the atmosphere was reduced. In addition, the absorbed energy in the atmosphere increases the temperature of the atmosphere and surface, and then the heated surface emits more longwave radiation. Eventually these processes are repeated in a positive feedback loop, which results in a continuous rise in temperature.