• 한국해안·해양공학회논문집
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• 제33권1호
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• pp.30-37
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• 2021

조선왕조실록에는 1741년 8월 29일 강원도 동해안에 쓰나미 피해가 발생했다는 기록이 등장한다. 이 쓰나미는 일본 홋카이도 남서해역의 오시마섬 인근에서 발생한 것으로 당시 한반도 동해안에 대한 쓰나미 영향 분석을 위해 파향선추적모형 시뮬레이션을 수행하였다. 서로 다른 네 가지의 수치격자형 수심자료(ETOPO2m, ETOPO1m, SKKU1m, GEBCO15c)를 이용하여 모형 결과를 산정하였으며, 그 중 해상도가 제일 높은 GEBCO15c 수심을 이용한 결과가 조선왕조실록에 기록된 피해 상황을 가장 잘 설명하는 것으로 나타났다. 이를 토대로 당시 강원도 동해안의 주요 지역에 쓰나미가 도달한 시간과 이동 경로를 추정하는 등 세부 분석결과를 제시하였다.

• Fisheries and Aquatic Sciences
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• 제5권1호
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• pp.5-20
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• 2002

To investigate the effect of mechanical parameters on the circulation and its fluctuation in Sagami Bay, baroclinic model experiments were carried out by use of a two-layer source-sink flow in a rotating tank. In the experiment, a simple coastal topography with flat bottom was reproduced. The results show that the path of the Through Flow, which corresponds to the branch current of the Kuroshio, depends on external Rossby number (Ro) and internal Rossby number $(Ro^*)$, and divided into two regimes. For $Ro^*\leq1.0$ in which Rossby internal radius of deformation of the Through Flow is smaller than the width of the approaching channel, the current flows along the Oshima Island as a coastal boundary density current separated from the western boundary of the channel. For $Ro^*>1.0$ it changes to a jet flow along the western boundary of the channel, separated from the coast of Oshima Island. The current is independent on both Ro and Ro* in the regime of $Ro^*>1.0,\;Ro\geq0.06$ and $Ro^*\leq1.0,\;Ro\geq0.06$. The pattern of the cyclonic circulation in the inner part of the bay is also determined by Ro and Ro*. In case of $Ro^*\leq1.0$, frontal eddies are formed in the northern boundary of the Through Flow. These frontal eddies intrude into the inner part along the eastern boundary of the bay providing vorticity to form and maintain the inner cyclonic circulation. For $Ro^*>1.0$, the wakes from the Izu peninsula are superposed intensifying the cyclonic circulation. The pattern of the cyclonic circulation is divided into three types; 1) weak cyclonic circulation and the inner anticyclonic circulation $(Ro<0.12)$. 2) cyclonic circulation in the bay $(0.12\leq Ro<0.25)$. 3) cyclonic circulation with strong boundary current $(RO\geq0.25)$.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2003년도 Proceedings of ACRS 2003 ISRS
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• pp.1246-1248
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• 2003

Internal wave with a soliton-like, large amplitudes within several kilometers, is frequently observed in the sea surface caused by tidal rectification due to sill or rough topographic changes. Internal waves can perturb current and density field, initiate bottom sediment re -suspension and mix nutrients to photic zone. Previous studies indicate that the appearance of internal wave in the Lombok Strait have been detected in SAR image data. This paper studies effect of internal wave in the Lombok Strait to chlorophyll distribution in the surrounded areas using SeaWiFS and ERS SAR images data during 1996-2001 periods. The preliminary result concludes that the internal waves presumably affect phytoplankton distribution spreading southeastward in the coast off Bali Island. The distribution of phytoplankton at southern coastline off Bali Island when internal wave occurred is elongated and distributed further to westward (from 8.8$^{\circ}$ to 10.7$^{\circ}$LS) than the area when internal wave did not occur on August 2000 (from 9.25$^{\circ}$ to 10.25$^{\circ}$LS) as shown in figure 3. It shown that the surface phytoplankton concentration near coastal area, i.e. from 8.8$^{\circ}$ to 9.25$^{\circ}$ LS, increased when internal wave is occurred.

• 한국해양환경ㆍ에너지학회지
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• 제15권3호
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• pp.198-207
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• 2012

본 연구에서 식물플랑크톤 뿐 아니라 동물플랑크톤을 포함하는 생태계 모델을 이용하여 해양 심층수의 해역 비옥화의 효과를 검증하였다. 모델은 2종의 식물플랑크톤, 3종의 동물플랑크톤, 질산염, 암모늄염, 규산염, 입자성 유기질소, 용존 유기질소, 입자성 규소 총 11개 요소로 구성된 NEMURO에 기초하고 있다. NEMURO의 11개 요소 외에도 두 종의 식물플랑크톤내 질소 셀 쿼터와 대형 식물플랑크톤내 규산염 셀 쿼터를 추가하였다. 해역 비옥화 효과를 조사하기 위해서 이즈 오시마 섬에서 실험을 실시하였지만, 본 실험에서 심층수의 유무에 의한 명확한 차이를 확인할 수 없었다. 이 실험 결과의 원인들을 모델 시뮬레이션에 의해 조사하였으며, 그 원인의 하나는 실험에 사용된 표층수의 높은 영양염 농도이다. 다른 원인은 무기질소 섭취율이 $NH_4$에 대한 $NO_3$의 비율에 관련되어 있으므로 무기질소의 총 농도의 증가가 광합성 속도를 반드시 증진시키지 않는다는 것이다. 이 모델로 실험 결과들을 재현할 수 있었기 때문에 우리는 이 모델을 이용하여 해양 심층수에 의한 해역 비옥화의 효과를 검증하였다. 해양 심층수의 공급 간격이 너무 짧거나 해양 심층수의 양이 너무 많을 때 해역 비옥화 효과는 나타나기 어려운 것으로 밝혀졌다. 해양 심층수의 첨가가 너무 비번하거나 너무 많이 첨가하면 플랑크톤 농도의 희석이 식물플랑크톤의 광합성 증진 효과를 초과해 버린 것으로 추측된다.

• 한국어류학회지
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• 제8권1호
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• pp.22-48
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• 1996

1988년 9월부터 1996년 3월까지 우리 나라의 전 연안에서 채집된 놀래기아목(亞目)(Labroidei) 어류에 대하여 분류학적으로 재검토하고, 미세 분포를 조사하였다. 한국산 놀래기아목 어류는 자리돔과(Pomacentridae), 키크리과(Cichlidae), 망상어과(Embiotocidae), 놀래기과(Labridae)와 파랑비늘돔과(Scaridae)의 5과에 22속(屬)32종(種)으로 정리되어, 이들의 과, 속 및 종 검색표를 제시하였다. 본 조사에서 직접 표본을 입수한 15속 21종은 표본을 중심으로 계수 계측형질을 재 기재하였다. 이중에 1996년 3월 전남 완도에서 채집된 망상어과 어류 Ditrema viridis Oshima는 국내에서는 처음으로 보고되는 종이다. 외래도입종인 키크리과 어류를 제외한 대부분의 놀래기아목 어류는 쿠루시오 난류의 영향을 받는 제주도 연안과 남해안, 그리고 동해 남부와 울릉도 근해에까지 분포하였다.

• 수산경영론집
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• 제39권1호
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• pp.87-114
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• 2008

The cultured tuna production which has suddenly expanded at the short time and the demand for it attract attention. Farming mode, distribution transactions, change of the market (domestic and international) and the price trend are reviewed from the Japan's position which is the biggest consuming country. This paper tries to describe the current status of the food system related to the cultured tuna. Japanese government began the development of the tuna culture technology in 1970. It was by the Fisheries Agency's project. Kinki University which is the large scale private university in Japan participated in the project. After that, 32 years have passed. Kinki University established the full farming of the bluefin tuna in August, 2002. On the other hand, in 1974, one Japanese private enterprise began its tuna farming business in Canada. Kinki University gave this company technical cooperation. Also, in the early stages of the 90s, as for the policy of the overseas fishery cooperation foundation, it supported the tuna farming business in Australia. It is very clear to understand that the long-term technological-development has supported the take-off scene of the tuna culture business not only in foreign countries but also in Japan. The total shipment scale of the cultured tuna expanded very much within about 10 recent years. However, the decrease of the wild tuna catch, the reinforcement of the fisheries regulation and the tuna body to dwarf are remarkable now. Under the condition as the mentioned above, Japan's tuna consumption, especially, in the market at the fatty meat of tuna of the cultured tuna is building up firm status. At present, the Mediterranean Sea coastal countries, Australia, Mexico and Japan have the tuna farming sites. Australia farms the southern bluefin tuna. The others do the bluefin tuna. About for 3 years, Japan farms the juvenile of the tuna. The global production areas are as follows. 8 coastal countries of the Mediterranean Sea; 18,000 tons (61 % of the cultured tuna quantity in foreign countries), Mexico; 4,500 ton (15%), Australia; 7,000 tons (24%). In 2003, Japan has 32 managements and 39 offices for tuna farming. In Japan, Kyushu and Okinawa district, the share shows itself as 80 % of the domestic production quantity. Especially, the share of Amami-oshima Island in Kagoshima Prefecture exceeds 60 %. Therefore, this island has the maximum production scale of Japan. The amount of supply of BT and SBT was 56,000 tons in 2004. In Abroad, the tuna farming business forms a fixed connection between the importer and the wholesaler which have their office in Japan. In the field of the capital composition, the payment in advance, transaction and the way of settlement, each maintains their fixed relation. The market conditions of the cultured tuna are supported by "the decline of price level" and "the expansion of the general public consumption segment". These lead a team merchandising, and it is supported by the fixed business connection of each. This makes the profit of each business which are on the cultured tuna distribution. However, they have competition on the power balance among them.