• 수산해양기술연구
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• 제44권4호
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• pp.323-344
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• 2008

To examine species composition, abundance and biomass of demersal organisms in the East Sea, bottom trawl survey was conducted at 7 sea areas from 2005 to 2007. A total of 107 species were collected and were composed of 54 fish species, 16 crustacea, and 37 mollusks in the East Sea from 2005 to 2007. Yearly abundance per area which caught by trawl survey in the East Sea from 2005 to 2007 ranged from a high of $292,234inds./km^2$ in 2005 to a low of $192,092inds./km^2$ in 2006. The abundance by sea area showed a peak in 76 sea area, and the lowest in 63 sea area. The abundance per area by season showed a peak in summer, and the lowest in spring. The most dominant species in abundance were Clupea pallasii, Neocrangon communis, Chionoecetes opilio. Yearly biomass per area which caught by trawl survey in the East Sea from 2005 to 2007 ranged from a high of $10,322kg/km^2$ in 2006 to a low of $7,096kg/km^2$ in 2005. The most dominant species in biomass were Chionoecetes opilio, Clupea pallasii, Dasycottus setiger. The biomass by sea area also showed a peak in 76 sea area, and the lowest in 93 sea area. The abundance by season also showed a peak in summer, and the lowest in spring. As a result of cluster analysis, demersal organisms community of 76 sea area showed a large difference with other sea area, and that of summer showed a large difference with other season.

• ALGAE
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• 제23권2호
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• pp.135-140
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• 2008

A field survey for dinoflagellate cysts was carried out from May 2000 to November 2002 for the Southwest Sea of Korea. A total dinoflagellate cysts identified were 33 species, which belonged to 17 genera, 31 species, and 2 unidentified species. A cysts density were 16-1,501 cysts-gdry$^{-1}$. The dominant species of dinoflagellate cysts in the Southwestern Sea of Korea were Spiniferites bulloideus and Scrippsiella trochoidea, which are autotrophic species. To investigate the environmental characteristics of the Southwestern Sea of Korea using the dinoflagellate cysts, a principal component analysis (PCA) was conducted using the data collected from a total of 51 stations. From the score distribution map by the PCA, the Southwestern Sea of Korea was largely divided into three regions according to the first primary component and the second primary component. In other words, Group 1 was the western sea area of Mokpo and Jindo, Group 2 was the outer sea area of the South Sea, and Group 3 was the coastal areas of the South Sea around the Archipelago. It was found that this division of sea area was influenced by effects of the sea environment of the coastal areas of Korea. The coastal areas of Mokpo and Jindo that belong to Group 1 were affected by the cold Yellow Sea water. The outer sea area of the central parts of the South Sea that belong to Group 2, which is the boundary between the Southern coastal water of Korea and the Tsushima warm water, was subject to the formation of temperature fronts throughout the year, while Group 3 was affected by the coastal waters of Korea. It was also found that this division was in close relationship with the distribution of sediment facies in the bottom layer. From the above results, the environmental factors that influence the cyst distribution in he Southwestern Sea of Korea were found to include the eutrophication status of the sea area, the physical characteristics of the sea environment such as the flow of sea current and fronts, the sediment facies in the bottom layer, and the appearance volume of motile cells.

• 한국환경과학회지
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• 제10권6호
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• pp.431-436
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• 2001

Variations in phytoplankton concentrations result from changes of the ocean color caused by phytoplankton pigments. Thus, ocean spectral reflectance for low chlorophyll waters are blue and high chlorophyll waters tend to have green reflectance. In the Korea region, clear waters and the open sea in the Kuroshio regions of the East China Sea have low chlorophyll. As one moves even closer In the northwestern part of the East China Sea, the situation becomes much more optically complicated, with contributions not only from higher concentration of phytoplankton, but also from sediments and dissolved materials from terrestrial and sea bottom sources. The color often approaches yellow-brown in the turbidity waters (Case Ⅱ waters). To verify satellite ocean color retrievals, or to develop new algorithms for complex case Ⅱ regions requires ship-based studies. In this study, we compared the chlorophyll retrievals from NASA's SeaWiFS sensor with chlorophyll values determined with standard fluorometric methods during two cruises on Korean NFRDI ships. For the SeaWiFS data, we used the standard NASA SeaWiFS algorithm to estimate the chlorophyll_a distribution around the Korean waters using Orbview/ SeaWiFS satellite data acquired by our HPRT station at NFRDl. We studied In find out the relationship between the measured chlorophyll_a from the ship and the estimated chlorophyll_a from the SeaWiFs satellite data around the northern part of the East China Sea, in February, and May, 2000. The relationship between the measured chlorophyll_a and the SeaWiFS chlorophyll_a shows following the equations (1) In the northern part of the East China Sea. Chlorophyll_a =0.121Ln(X) + 0.504, R²= 0.73 (1) We also determined total suspended sediment mass (55) and compared it with SeaWiFS spectral band ratio. A suspended solid algorithm was composed of in-.situ data and the ratio (L/sub WN/(490 ㎚)L/sub WN/(555 ㎚) of the SeaWiFS wavelength bands. The relationship between the measured suspended solid and the SeaWiFS band ratio shows following the equation (2) in the northern part of the East China Sea. SS = -0.703 Ln(X) + 2.237, R²= 0.62 (2) In the near future, NFRDI will develop algorithms for quantifying the ocean color properties around the Korean waters, with the data from regular ocean observations using its own research vessels and from three satellites, KOMPSAT/OSMl, Terra/MODIS and Orbview/SeaWiFS.

• 한국정보통신학회:학술대회논문집
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• 한국해양정보통신학회 2003년도 추계종합학술대회
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• pp.339-342
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• 2003

1993년에서 1997년까지의 위성고도계 자료(Topex/Poseidon)를 이용하여 한반도 주변해역의 해면 변화와 표층흐름을 조사하였다. 해면변화를 보면, 동해에 비해서 서해와 남해는 항상 상대적으로 높았다. 전 조사 기간에 걸쳐서 서해는 북부와 남부 해역에서 각각20-30cm와 18-24cm의 변화범위를 보였으며, 남해는 제주도 북서부 해역에서는 15-20cm 그리고 쓰시마섬 남서부 해역에서는 10-15cm의 변화범위를 각각 나타내었다. 서해의 경우에 황해난류의 표층 유입류와 해저 지형류의 영향을 받아 높은 변화를 보였다. 남해의 경우는 변화가 일어나는 두 곳 모두가 근원적으로는 쿠로시오 해류의 흐름에서 분기된 지류들의 흐름(제주난류와 동한난류) 때문에 해면변화를 보였다. 표층 순환은 동해에서 북한한류, 동한난류와 쓰시마 난류와 관련한 세가지 와류운동이 두드러지게 나타났다. 와류운동은 기본적으로 표층 순환에서 해류의 영향을 받았다; 원산만 앞바다의 반시계방향(0.03 cm/sec)의 흐름은 북한한류, 울릉도 남서쪽 해역의 시계방향(0.06 cm/sec)의 흐름은 동한난류, 그리고 쓰시마섬 북서쪽 해역은 쓰시마 난류와 각각 관계되어있는 것으로 보인다.

• 환경생물
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• 제26권2호
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• pp.102-108
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• 2008

방오도료로 많이 쓰인 유기주석화합물은 일반생물에게 미치는 독성이 매우 강하고 또한 내분비계 장애물질임이 밝혀지면서 이를 대체할 화합물들의 개발이 요구되고 있다. 그 가운데 이런 목적으로 만들어진 화합물인 Sea-Nine 211을 사용하여 이것이 해양생물 특히 저서생물인 패류에게 얼마나 영향을 미치는지를 살펴보고자 북방대합(P. sachalinensis)에게 강제 주사하여 생존율과 중장선의 미크로좀 중 I상 약물대사효소의 변화를 4일째가지 조사하였으며, 또한 비교를 위해 tributyltin chloride (TBTC)의 주사실험을 병행하였다. 생존율에서는 sham구나 Sea-Nine 211 실험구(5, 25 및 50 mg kg$^{-1}$)모두 생존하였으나 TBTC(1, 2 및 5 mg kg$^{-1}$) 실험구의 생존율은 4일째에 각각 70%, 30% 및 0%였다. 한편, 약물대사효소계 중 I상효소인 CYP는 Sea-Nine 211주사 후 시간이 지나면서 유도되었지만, TBTC는 반대로 저해되는 경향을 보였다. 그리고 P450R 활성은 Sea-Nine 211 실험구에서 시간 경과와 더불어 약간 증가하는 추세를 보였지만 sham구와는 유의적인 차이가 없었으나, TBTC실험구는 주사농도와 비례하면서 저해되었다. b5R활성도 마찬가지로 Sea-Nine 211 실험구는 큰 변화가 없었으나, TBTC실험 구에서는 유의적으로 저해되는 경향을 관찰할 수가 있었다. 이처럼 비주석계 방오도료 화합물인 Sea-Nine 211은 북방대합에 대한 독성이 TBTC에 비해 크게 낮았으며, 약물대사효소계에 미치는 영향도 TBTC는 저해하는데 반해서 P450R이나 b5R에는 별다른 변화를 일으키지 않았으나 CYP는 유도하였다.

• 한국식품조리과학회지
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• 제14권1호
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• pp.25-32
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• 1998

To measure the contents of several heavy metal elements (Cr, Mn, Ni, Cu, Zn, Cd, Hg, Pb) in Korean seaweeds which are closely related to food resources, various seaweed samples were collected from thirteen to seventeen seaweed-producing districts. The results obtained from the experiment are summarized as follows: 1. The content of heavy metal elements in seaweeds of individual sample ranged from 0.0005 to 25.0373 ppm. Their mean levels were as follows: laver, 0.0024∼3.9297 ppm; sea lettuce, 0.0011∼25.0373 ppm; sea mustard, 0.0005∼23.5071 ppm; sea tangle, 0.0006∼4.8550 ppm. The mean levels of Cd and Pb were specially low in the samples collected from the area II in Kangwon and area Ⅸ in Kyungbook. 2. The mean levels of heavy metal elements of collected samples ranged from 0.0117 to 4.4944 ppm. Laver showed the lowest level of Hg and sea lettuce showed the highest level of Mn. Their mean levels of elements were as follows: laver, 0.0117∼2.3339 ppm; sea lettuce,0.0232∼4.4944 ppm; sea mustard, 0.0129∼1.5139 ppm and sea tangle, 0.0182∼1.7410 ppm. 3. The mean levels of heavy metal elements from several locations ranged from 0.0085 ppm to 8.4148 ppm. The mean levels of heavy metal elements in sea mustard from area V of Kyungbook were the lowest, but the mean levels of heavy metal elements in sea lettuce from area Ⅷ of Kyungnam were the highest. The mean level of heavy metal elements were as follows: laver, 0.3613∼1.1124 ppm; sea lettuce, 0.1415∼8.4148 ppm; sea mustard, 0.0729-3.1182 ppm; sea tangle, 0.0085∼0.7587 ppm. 4. Generally the heavy metal elements were detected in the seaweed samples from all locations. The mean levels of heavy metal elements varied with locations and kinds of samples. The levels of heavy metals of the samples taken from all locations from the East Sea, the South Sea, and the West Sea areas showed 99% safety range.

• 한국환경과학회:학술대회논문집
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• 한국환경과학회 2008년도 추계학술발표회 발표논문집
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• pp.286-289
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• 2008

• 한국도서관정보학회지
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• 제50권4호
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• pp.57-76
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• 2019

동해 지명의 변천과 표기의 다양성을 고찰하고, 이를 바탕으로 54개 국가도서관 목록레코드를 조사하여 동해관련 자료의 표기 실태 및 특성을 비교 분석하였으며, 결과를 요약하면 아래와 같다. 첫째, 동해관련 자료가 대부분 미국, 러시아, 일본 등 일부 특정 국가도서관에 집중되어 있는 반면, 한 건도 검색되지 않은 곳이 5개관에 달했다. 둘째, 각국의 국가도서관에서 동해관련 자료의 표제 키워드는 일본에서 동해를 지칭하는 용어인 '일본해'로 표기한 경우가 67.9%, '동해' 29.6%, 이들 용어의 병기가 2.5%로 나타났다. 셋째, 각국의 국가도서관에서 동해관련 자료가운데 '일본해' 또는 '일본해(지리한정어)'라는 의미로 주제명을 나타낸 경우가 86.9%, '동해' 1.2%, 일반주제명이거나 주제명이 나타나 있지 않은 경우가 11.9%로 나타났다.

• 한국환경과학회지
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• 제10권6호
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• pp.423-429
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• 2001

Satellite data, with sea surface temperature(557) by NOAA and sea level(SL) by Topex/poseidon, are used to estimate characteristics on the variations and correlations of 557 and SL in the East Asian Seas from January 1993 through May 1998. We found that there are two climatic characteristics in the East Asian seas the oceanic climate, the eastern sea of Japan, and the continental climate, the eastern sea of China, respectively. In the oceanic climate, the variations of SL have the high values in the main current of Kuroshio and the variations of 557 have not the remarkable seasonal variations because of the continuos compensation of warm current by Kuroshio. In the continental climate, SL has high variations in the estuaries(the Yellow River, the Yangtze River) with the mixing the fresh water and the saline water in the coasts of continent and 557 has highly the seasonal variations due to the climatic effect of continents. In the steric variations of summer, the eastern sea of Japan, the East China Sea and the western sod of Korea is increased the sea level about 10~20cm. But the Bohai bay in China have relatively the high values about 20~30cm due to the continental climate. generally the trends of SST and SL increased during all periods. That is say, the slopes of 557 and SL Is presented 0.29$^{\circ}C$/year and 0.84cm/year, respectively. The annual and semi-annual amplitudes have a remarkable variations in the western sea of Korea and the eastern sea of Japan. In the case of the annual peaks, there appeared mainly In the western sea of Korea and the eastern sea of .Japan because of the remarkable variations of SL associated with Kuroshio. But in the case of the semi-annual peaks, there appeared in the eastern sea of Japan by the influence of current, and in the western sea of Korea by the influence of seasonal temperature, respectively. From our results, it should be believed that 557 and SL gradually Increase in the East Asian seas concerning to the global warming. So that, it should be requested In the international co-operation against In the change of the abnormal climate.

• 대기
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• 제28권1호
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• pp.25-35
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• 2018

This study presents future potential sea level change over the seas surrounding Korea using Climate Model Intercomparison Project Phase 5 9 model ensemble result from Representative Concentration Pathways (RCPs), downloaded from icdc.zmaw.de. At the end of 21st century, regional sea level changes are projected to rise 37.8, 48.1, 47.7, 65.0 cm under RCP2.6, RCP4.5, RCP6.0 and RCP8.5 scenario, respectively with the large uncertainty from about 40 to 60 cm. The results exhibit similar tendency with the global mean sea level rise (SLR) with small differences less than about 3 cm. For the East Sea, the Yellow Sea, and the southern sea of Korea, projected SLR in the Yellow Sea is smaller and SLR in the southern sea is larger than the other coastal seas. Differences among the seas are small within the range of 4 cm. Meanwhile, Commonwealth Scientific and Industrial Research Organization (CSIRO) data in 23 years shows that the mean rate of sea level changes around the Yellow Sea is high relative to the other coastal seas. For sea level change, contribution of ice and ocean related components are important, at local scale, Glacial Isostatic Adujstment also needs to be considered.