• 한국지구과학회지
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• 제45권3호
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• pp.192-202
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• 2024

해양재분석 자료는 관측 자료를 수치 모델에 동화함으로, 관측 자료의 시공간적인 제약을 극복하고 해양 변수 간의 물리적 상호작용을 고려한 격자화된 고해상도 정보를 제공함으로써 해양순환 및 기후 연구에 광범위하게 사용되고 있다. 이 연구에서는 기존에 생산된 12년간(2011년부터 2022년까지)의 북서태평양 지역해양 재분석 자료를 확장하여 30년간(1993년부터 2022년까지)의 1/24° 수평해상도를 갖는 장기 재분석 자료(K-ORA22E)를 생산하고, 이를 분석하여 한반도 주변해역에서의 장기 해양기후변화를 진단하였다. K-ORA22E 데이터를 통해 한반도 주변 해역의 수온 상승 경향을 분석한 결과, 쿠로시오 확장역에서 쿠로시오의 경로가 지난 30년 동안 1년에 약 6 km 씩 북상하였으며, 쿠로시오 경로의 북쪽에서 수온 상승이 두드러졌다. 한반도 주변 해역 중에서는 동해에서 수온 상승이 가장 뚜렷했다. 특히, 동해에서는 표층보다는 중층에서 수온 상승이 두드러졌으며, 동한난류의 수온 상승률은 전 지구 평균보다 2-3배 높았다. 황해저층냉수가 출현하는 황해 중앙부에서는 장기적으로 수온이 상승하였으나, 한반도 서해안과 남해안에서는 수온이 오히려 감소하는 경향이 나타났다. 이러한 수온의 장기변화의 공간적인 차이는 쿠로시오 해류의 북상에 따른 열수송의 경로와 밀접한 관련이 있을 것으로 보인다. 이 연구에서 구축된 K-ORA22E와 같은 고해상도 지역 해양 재분석 자료는 한반도 주변 해역의 장기 변동성을 이해하고 기후 변화의 영향을 분석하는 데 중요한 기초 자료로 활용될 수 있을 것이다.

• 한국생물공학회:학술대회논문집
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• 한국생물공학회 2005년도 생물공학의 동향(XVI)
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• pp.334-334
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• 2005

• Animal Systematics, Evolution and Diversity
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• 제22권1호
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• pp.109-115
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• 2006

Two marine gastrotrich species are reported from sublittoral sand bottom of Korea: Diplodasys ankeli Wilke, 1954 and D. meloriae Todaro, Balsamo and Tongiorgi, 1992. Both species are redescribed in detail, with the discussion on the intraspecific variability between Korean specimens and the original description or among Korean specimens. The genus Diplodasys is newly recorded from Korea as well as the Northwest Pacific.

• Asian Pacific Journal of Cancer Prevention
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• 제16권13호
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• pp.5459-5462
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• 2015

This case series study was performed for all 83 children below 14 years old suffering from cancer during 2010-2013 who were registered in Ardabil pediatric cancer registry (APCR). The required data were collected by questionnaire and analyzed with SPSS.19 statistical methods software. Some 51 (61.4%) of cases were male. The mean age of patients was 5.8 years. Of the total, 60 (72.3%) of cases were from urban areas. Results showed that leukemia with 54.2%, CNS with 12% and neuroblastoma with 8.4% were the most prevalent childhood malignancies in Ardabil province. Based on the under 14 year old population estimated from Ardabil province, the cumulative incidence rate was 95.4 patients per one million. The incidence rate was relatively high so that childhood cancers should be considered as an important issue in health policy making in Ardabil province of Iran.

• International Journal of Human Ecology
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• 제9권2호
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• pp.45-54
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• 2008

This study examines the influence of acculturation level and ethnic groups as a fashion reference group on Korean-American consumer attitude toward luxury fashion brands. Of interest is the role of Korean culture, which emphasizes luxury brand consumption due to the Confucion value of 'face', on Korean-American attitudes toward luxury brands. Data were collected from 108 young Korean-Americans living in the Pacific Northwest of the United States. Descriptive statistics, factor analysis, and multiple regressions were conducted for the analysis. In general, the respondents had relatively negative attitudes toward luxury fashion brands. Even though the acculturation level did not have a significant influence, attitudes toward luxury fashion brands were influenced by Korean reference groups. Age at immigration did not have a significant relationship with attitudes toward luxury brands. Korean-Americans who maintain ties with Korean culture are more likely to have a positive attitude towards luxury fashion, regardless of familarity with American culture.

• Journal of the korean society of oceanography
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• 제33권3호
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• pp.80-89
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• 1998

Three cores were taken from the northwest Pacific Ocean (Shikoku Basin) to determine the accumulation rates of both biogenic and terrigeneous fractions since the last penultimate interglacial period. The sediment is characterized by large amounts of terrigenous materials with low biogenic fractions and intermittent volcanic-ash layers, suggesting a hemipelagic origin. Composition of major elements shows no significant differences among sites. Relatively small variation of TiO$_2$/Al$_2$O$_3$ ratios with respect to SiO$_2$ content is the strong evidence for the common origin of terrigenous materials. The fraction of biogenic carbonates varies from near 0% in ash layers to about 35%, with a gradual increase toward the south (St. 4 through St. 6 to St. 20). However, carbonate contents show step-wise increasing tendency from St. 4 through St. 6 to St. 20, which suggests a southward increase of carbonate production. The color reflectance indicates that the sediment of the southern sites contains relatively higher amounts of biogenic carbonates. The mass accumulation rate of terrigenous fractions during the glacial period was 2-3 times higher than that of interglacial period. This enhanced mass accumulation rate of terrigenous materials was concomitant with the high accumulation rate of biogenic fractions. The total sediment accumulation rate is considered as the most important factor controlling mass accumulation rates of the biogenic and terrigenous materials. The enhanced sediment accumulation during the glacial periods is interpreted as a consequence of climate-induced change in the supply of eolian dust from the Asian continent. Enhanced wind strength during the glacial time may have increased transportation of terrigenous materials to the ocean. Thus, variation of sediment accumulation is highly linked with climatic variations.

• Journal of the korean society of oceanography
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• 제31권4호
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• pp.207-216
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• 1996

A geochemical study of three piston cores (ST.4, ST.6 and ST.20) taken from the Northwest Pacific (eastern edge of Shikoku Basin) provides information about changes in surface water paleoproductivity and sedimentation during the last 127 kys. Paleoproductivity variations were estimated on the basis of total organic carbon content and carbonate mass accumulation rate. The paleoproductivity based on total organic carbon shows significant spatial variations between glacial and interglacial periods. During the last glacial maximum (LGM) paleoproductivity increased about 1.5 times with deglaciation decrease compared with those of the Holocene at inner side of the Shikoku Basin (ST.4 and ST.6). On the other hand, paleoproductivity at outer side of Shikoku Basin (ST.20) indicating not distinctive increase but deglaciation increase. The C/N ratios fall below 10 for cores ST.4 and ST.6, but C/N ratios between 100 ka and 80 ka in ST.20 which show around 10 or larger values suggest a predominance of marine organic carbon with some admixture of terrigenous materials. The carbonate mass accumulation rate of three cores show different patterns of calcareous record with respect to organic carbon based paleoproductivity variation. In the inner side of Shikoku Basin (ST.4 and ST.6) the carbonate mass accumulation rate decreased during last glacial maximum, and significant increase of carbonate mass accumulation rate is recognized at outer side of Shikoku Basin (ST.20). Thus, this set of data reveals that spatial paleoproductivity variations between inner and outer side of Shikoku Basin during the glacial and interglacial periods.

• Ocean and Polar Research
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• 제26권4호
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• pp.559-565
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• 2004

Total magnetic field measurements were performed to study paleomagnetism of three seamounts (OSM7, OSM8-1, and OSM8-2) to the northwest of the Marshall Islands in the western Pacific. The study area is located at the Ogasawara Fracture Zone which is a boundary between the Pigafetta and East Mariana basins. The magnetic parameters and paleopoles of three seamounts were derived from inversion of the measured magnetic field. The goodness-of-fit ratio of OSM7 is too low to be included to the estimation of parameters. The complex magnetic anomalies of center, scarcity of flank rift zones and steep slope at OSM7 suggest that the multiple intrusions of magma converge into the center of volcanic edifice. Inclination calculated from the magnetic anomalies of OSM8-1 and OSM8-2 is $-41.2^{\circ}$, and the paleolatitude calculated from the inclination is $23.6^{\circ}S$. The corresponding paleopoles for OSM8-1 and OSM8-2 are $(24^{\circ}42'W,\;48^{\circ}54'N)\;and\;(18^{\circ}18'W,\;48^{\circ}30'N)$, respectively. In comparison with the apparent polar wander path (APWP) of the Pacific plate, the paleopoles are close to 129-Ma pole. The paleopoles and paleolatitudes of OSM8-1 and OSM8-2 suggest that they were formed at similar time and location. The seamounts have drifted northward about $41^{\circ}$ from the paleolatitude to present latitude of seamounts.

• 한국수산과학회지
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• 제10권4호
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• pp.237-241
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• 1977

1976년 9월 20일 부터 24일 사이에 북서태평양(Kamchatka 근해에서 투명도, 태양광선의 적색광(과장 : 600\~620\;nm)에 대한 표면조도 및 수심별 수중조도와 태양고도, 기온 및 표층수온 등을 조사한 결과를 요약하면 다음과 같다. 1. 본 조사해역의 평균투명도는 $10.6m(9\~l2m)\$로 나타났다. 2. 태양광선의 적색광에 대한 해수의 흡수계수는 $0.178\~0.376$(평균 0.278)였다. 3. 적색광에 대한 해수의 흡수계수 m와 투명도 D와의 관계는 m=3.347/D로 나타났다. 4. 관측된 평균기온은 $9.49^{\circ}C(7.8-12.6^{\circ}C)$ 였고, 평균표층수온은 $6.58^{\circ}(5.8-7.6^{\circ}C$)로 나타났다. 5. m층에서 적색광에 대한 수중투과율은 수심 5 m층에서 표면창의 $6.45\~23.5\%$(평균 $16.36\%$), 수심 10 m층에서는 $1.38\~7.31포$(평균 $3.65\%$)였고, 수심 20 m층에서는 $0.048\~0.647\% $(평균 0.276\%)로 나타났다.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume I
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• pp.467-470
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• 2006

Geostationary Ocean Color Imager (GOCI) onboard its Communication Ocean and Meteorological Satellite (COMS) is scheduled for launch in 2008. GOCI includes the eight visible-to-near-infrared (NIR) bands, 0.5km pixel resolution, and a coverage region of 2500 ${\times}$ 2500km centered at 36N and 130E. GOCI has had the scope of its objectives broadened to understand the role of the oceans and ocean productivity in the climate system, biogeochemical variables, geological and biological response to physical dynamics and to detect and monitor toxic algal blooms of notable extension through observations of ocean color. To achieve these mission objectives, it is necessary to develop an atmospheric correction technique which is capable of delivering geophysical products, particularly for highly turbid coastal regions that are often dominated by strongly absorbing aerosols from the adjacent continental/desert areas. In this paper, we present a more realistic and cost-effective atmospheric correction method which takes into account the contribution of NIR radiances and include specialized models for strongly absorbing aerosols. This method was tested extensively on SeaWiFS ocean color imagery acquired over the Northwest Pacific waters. While the standard SeaWiFS atmospheric correction algorithm showed a pronounced overcorrection in the violet/blue or a complete failure in the presence of strongly absorbing aerosols (Asian dust or Yellow dust) over these regions, the new method was able to retrieve the water-leaving radiance and chlorophyll concentrations that were consistent with the in-situ observations. Such comparison demonstrated the efficiency of the new method in terms of removing the effects of highly absorbing aerosols and improving the accuracy of water-leaving radiance and chlorophyll retrievals with SeaWiFS imagery.