여수 연안 승망 어장의 주변 해역을 중심으로 조사한 해양 관측 자료와 현지에 조사한 어획량 등을 이용하여 여수 연안 승망 어장의 환경특성과 어획량 변동과의 관계를 분석 정리한 결과를 요약하면 다음과 같다. 1) 승망 어장에서의 수온의 분포범위는 13.0-25.0˚C이고, 4월부터 상승하기 시작하여 8월에 최고 수온 25.0˚C을 나타내다가 9월부터 하강하기 시작했다. 2) 어장에서의 염분의 분포범위는 28.6-33.8‰이고, 4월과 5월에는 32.0‰이상의 염분수가 분포하며, 6월부터 하강하기 시작하여 8월에는 최저염분 28.6‰를 나타내다가 9월부터 다시 상승하기 시작한다. 3) 여수 연안 승망에 어획되는 주어종인 숭어의 어획량은 5월에 최대 어획을 나타내고 6월부터 감소하기 시작하여 11월에는 최소 어획을 나타냈다. 수온이 높아지기 시작한 시기인 5월의 수온이 15.0-1625.0˚C에서, 저염보다 고염분인 32.6-33.8‰에서 어획이 양호하게 이루어졌다.

우리나라 동해안 명태어장의 어업환경 개선을 위한 기초연구로서 , 1998년 6, 7월과 1999년 5, 7, 8월에 걸쳐서 강원도 고성군 근해에서 사조묘로 수거 한 침체어구의 실태를 조사·분석하였다. 1. 폐어구는 어업활동에 의해서 발생된 것으로 저자망과 통발의 2종류였다. 2. 폐어구의 무게는 저자강이 1,170 t,통발이 4 t 으로, 저자망이 압도적으로 많았다. 3. 마일당 저자강의 수거량은 1998년 22.74 t에서 1999년 10.72 t 으로 12.02 t 감소 하였다. 4. 폐어구 수거율은 1998년 38.0%, 1999년 41.9%로 낮았고 CPUE는 1998년 11.27 t /회, 1999년 7.48 t /회이었다. 5. 사조묘에 의한 본 조사방법은 어장에서 발생한 침체어구의 수거에 유효한 수단이라고 생각된다.

한국 연근해에서 조업하고 있는 어선을 효율적으로 관리할 수 있는 어선관제시스템의 구축을 위한 기초 연구로서 제주도 성산포항을 거점으로 하여 조업중인 대형선망어선단의 어로과정의 ARPA 영상을 디지털신호로 변환시켜 분석하고 VTMS를 이용하여 모의실험을 행한 결과를 요약하면 다음과 같다. (1) 대형선망어선단의 어로과정을 분석한 결과 투망소요시간은 16분, 양망소요시간은 35분이었고, 앞잡이 배가 끌어 주는 로프의 길이는 200m, 투망시 선회경은 340.8m, 선회속도는 약 6kts로써 조업 과정을 명확하게 파악할 수 있었다. (2) 실선실험에서 구한 투.양망과정에 유향.유속을 NE, 2kts와 SW, 2kts로 가상하여 시뮬레이션한 결과, 각각 SW, NE 방향으로 편위됨을 알 수가 있었다. 이와 같이 어장환경정보 또는 어업 정보나 조선정보를 관제시스템에 가미함으로써 실제조업과 같은 상황을 예측할 수 있었으며, 클로즈업시킨 화면을 통해 투 양망중 예상되는 상황과 문제점을 검토할 수 있었다. (3) 시뮬레이션에서 사용한 VTMS의 레이더 관제범위는 16mile이었고, 관제범위를 넘었더라도 타관제선으로의 이관이 가능하였다. 또한, 관제선과 집단선단들과의 거리와 방위를 측정하고 분석하면 관제선의 위치선정이 용이함을 알 수 있었다. (4) 조업선들이 어황정보와 안전항행정보를 제공받아 안전하고 효율적인 조업을 행할 수 있는 어선관제 시스템(FVTMS)의 예측모델을 제시하였다. 이와 같이 VTMS용 관제시스템을 이용하여 선단조업어선의 어로과정에 대한 시뮬레이션 한 결과, 근접조업에 따른 잦은 경보와 추적 상실 등 몇가지 기능상의 문제점이 발견되었으므로 어선관제시스템(FVTMS)에 적합한 프로그램이 시급히 개발되어야 할 것으로 사료된다.

한국 남해 중부 연안 어장에서 여수대학교 실습선을 이용하여 1998년 5월, 8월, 11월 및 1999년 2월에 조사한 해양 관측 자료를 이용하여 남해 중부 연안어장의 수괴의 특성을 분석한 결과를 요약하면 다음과 같다. 1)남해 중부 연안 어장에서 수온 염분의 측정값을 이용한 T-S diagram으로부터 염분을 기준으로 수괴를 구분한 결과 연안수는 30.0~31.6‰, 혼합수는 31.7~33.4‰ 및 외해수 33.5~35.0‰의 범위였다. 2) 한국 남해 중부 연안 어장에 출현하는 춘계 염분의 분포 범위는 32.2~34.9‰였고, 하계 염분의 분포 범위는 29.0~34.7‰였다. 또한, 추계의 경우는 염분 31.4~34.5‰의 범위였고, 동계 염분의 분포 범위는33.5~34.6‰였다. 3)본 조사 해역에 출현한 연안수, 혼합수 및 외해수의 분포는 계절별로 약간의 차이는 있으나 대체적으로 춘계에는 거의 전역이 혼합수와 외해수로 형성되었고, 하계에는 연안수가 유입되기 시작하여 전역이 연안수와 혼합수로 형성되었다가 추계가 되면서 연안수의 범위가 현저하게 축소되고 혼합수가 주체를 이루고 있으나 외해수가 출현하기 시작하여 주로 외해수와 혼합수로 이루어지고, 동계에는 혼합수는 소멸하고 전역이 외해수로 형성되었다. 4) 수온과 염분의 변화가 연안역에서는 주로 표층과 30m층 사이에서 이루어지나 외양역에서는 표층과 50m층 사이에서 일어났다. 춘계와 추계에는 수온과 염분의 변화는 적고, 하계에는 수온과 염분경도가 강하게 형성하여 연안역은 10.5℃ /30m의 수온경도와 4.0‰/30m 의 염분경도를 보였으며, 외해역은 13.0℃/50m 〈/TEX〉의 수온경도와 약 3.8‰/50m의 염분경도를 보였고, 동계에는 연직혼합이 일어나 상하층간에 균질한 해수가 분포하였다. 또한, 외해역의 수심 50m 이하에서는 4계절에 34.0‰이상의 염분이 분포하고 있다.

In order to investigate the properties in distribution and movement of anchovy school catches by the lift net in the Kamak bay and their relation to the environmental factors, I. e., the amount of chlorophyll-a and turbidity were observed from June to August in 1997 and compared with the catch of anchovy by the lift net. The results obtained are summarized as follows;1) The amount of chlorophyll-a ranged from 4.0 to 12.0 mg/m3 on July and from 3.0 to 15.0 mg/m3 on August in horizontal distribution, the amount of chlorophyll-a ranged from 3.0 to 8.0mg/m3 on June, from 5.5 to 11.6 mg/㎥ on July, and from 6.0 to 11.1 mg/m3 on July and from 1.0 to 6.0ppm on August, respectively. 2) Anchovy school can be presurmed, they are come from north of bay, visited and distributed through east of bay at the middle of June. Moreover, they spreaded in all bay. Then gradually, when July arrive, they go to the south the nearest the coasts, and they are outflow through the south entrance of bay at the end of August.3) The catch of anchovy was highest on July, poor second on August, and lowest on June. The chlorophyll-a and the turbidity influenced remarkably on the distribution and movement of anchovy school and the influence of chlorophyll-a was alrgest.

In order to investigate the oceanic condition of fishing ground in the southwestern coastal sea of Korea, the oceanographic observation were carried out by the trainingship of Yosu university on May, August and November in 1998. Main features in the observation are as follows; 1) the ranges of temperature, salinity, density and chlorophyll-a were from 14.5℃ to 18.0℃, from 33.5‰ to 34.5‰from 24.0 to 25.5 and from 1.0μg/l in spring (May) from 15.0℃ to 27.5℃, from 0.0‰ 35.0‰9.0 to 26.0 and from 0.5μg/l to 4.0μg/l in summer(August), and from to 21.0˚ 31.0‰, from 22.0 and from 4.0μg/l to 20.0μg/l in autumn(November), respectively, 2) the temperature in the coastal region was higher than that in the open ocean while salinity, density and chlorophyll-a were lower, and the convection was identified between the surface and the bottom during in spring and autumn, 3) the chlorophyll-a in the this region was varied in each season, being highly distributed offshore Yosu Bay, 4) on evidence of sea water intrusion toward Kumun island was observed.

In order to investigate the properties in distribution and movement of anchovy school catches by the lift net in the Kamak bay and their relation to the environmental factors, i.e., the water temperature and the salinity were observed form June to August in 1997 and compared with the catch of anchovy by the lift net. The results obtained are summarized as follows;1) The water temperature and salinity ranged form 20.0 to 27.0℃ and from 31.2 to 33.8‰, respectively. The water temperature and salinity at the fishing points ranged form 19.7 to 27.2℃ and, from 30.5 to 33.8℃ respectively.2) The water temperature influenced remarkably on the distribution and movement of anchovy school. But the salinity influenced little on the distribution and movement. 3) The catch of anchovy was highest on July, poor second on August, and lowest on June. Anchovy school can be presurmed, they are come from north of bay, visited and distributed through east of bay at the middle of June. Moreover, they spreaded in all bay. Then gradually, when July arrive, they go to the south th nearest the coasts, and they are outflow through the south entrance of bay at the end of August.

Temperal and spacial analysis for catches have been drawing up a catch distribution chart and analysing catches and CPUE(Catch Per Unit Effort) using catch data with purpose of obtaining basic data to establish a selective method of effective fishing the tuna purse seine fishing ground.The temperature profile section and catch was surveyed to analyse the effect of catch in relation to the fishing ground environment.The results are as follows ;1. As for the catch variation between 1983 and 1984, the catch mainly took place on150˚E, and after that it moved eastward enlarging the range of catch. In the monthly catch variation between January and February, the catches mainly happened on 135˚~ 150˚E, and then moved to the gradually westward. However, from July it moved to the South and from October Southeast.2. As to the eatch ratio for the school associated with the drifted object, the pelagic migrating school and the school associated with the biological objects, the catch ratio for the school associated with the drift objects was the highest. The catch ratio for the school associated with the drifted object was high in June, July and November whiles between January and March for the pelagic migrating school.3. SST(Sea Surface Temperature) was around 28~29〈/TEX〉C〈/TEX〉 on the observing line of 137˚E〈/TEX〉 and the catches took place in the north equatorial counter-current situated on around 5˚~6˚N. SST in the northern summer was 1〈/TEX〉C〈/TEX〉higher than winter and it was about 29~30〈/TEX〉C〈/TEX〉. The catch happened with the center of north equatorial counter-current. The reason why the catch mainly took place on the north equatorial counter-current is that main catch of tuna purse seine was the school associated with drift objects. It is thought that the fishing grounds are made in waters that have many drift objects like drift logs from the coast.

Floating debris was recorded from a training ship, #1 Kwarnksan, of Pukyong National University with about 10 knots speed during March, May and July of 1997. The area sampled is the Southeastern Coast of Korea, divided into 40 unit segments on survey routes. Debris fabrication materials were categorized using the following ; man-made or natural wood items, paper, cardboard, nylon rope, netting, styrofoam and plastics, floating metal and glass containers. All identified items within a 〈TEX〉100 ± 2 m〈TEX〉 wide band were recorded but ignored if beyond this boundary.The results of distribution and composition of floating debris in the area as follows:1. The quantities of debris during the duration of survey were distributed from 2~605 items per km2. The most obvious trend is the widespread distribution of all debris. 2. The highest densities of all debris were discovered in the coastal waters of Seoimal lighthouse, the southeastern part of Koje island, next near Nakdong estuaries. Especially styrofoam & plastics were observed in 77.4~87.2% of sampled area, next is wood items, 9.1~ 13.5%. And nylon netting & rope, 3.6%, was the third item of pollutant. Others are very small. 3. Compared with the East Coat of Korea, the quantities of all debus in theSoutheastern Sea are 6 times as large as the East Coast. The survey provides a basis for more detailed survey work in the South Sea. Further surveys are being investigated, and from this it is hoped that a much wider coverage can be achieved, perhaps on all sites of the Coast of Korea and contributed to the removal method, finding of sources, stationary area of debris.

In order to investigate the relation between the environmental factors influencing on the fluctuation of fishing condition and the catch of anchovy in gill nets in the coastal waters of Yosu, five oceanographic factors, i.e., water temperature, salinity, chlorophyll-a and the catch of anchovy in gill nets are observed from June 6 to August 12 in 1993. The results obtained are summerized as follows: 1) The water temperature ranged from 16.0℃ to 22.6℃ and the salinity from 30.13‰ to 33.65‰. the water temperature and salinity showed no significant influence on the catch of anchovy, but the catch did not expose high values in low temperature and salinity. 2) The catch of anchovy increased with the amount of chlorophyll-a. It is therefore emphasized that the amount of chlorophyll-a is the greatest one of environmental factors influencing on the catch of anchovy.

The study on the Assembling Mechanism of the Hairtail, Trichiurus lenpturus, at the Fishing Grounds of the Cheju Strait had been investigated by analyzing the relationship of the oceanographic conditions and the fishing ground of the Hairtail in the Cheju Strait. 1. The fishing grounds of the hairtail at the Cheju Strait are formed at the bottom of a high temperature of the tidal front at the coast. area of northern Cheju Island, the tip of the linguiform is high in salinity at the eastern and western entrances of Cheju Island, low salinity eddy on the surface and its surrounding front, various water masses in the Strait and coastal waters of the South Sea in Korea. 2. The fishing grounds of the Hairtail at the Cheju Strait begins with the sea surface temperature higher than 15℃ and the incoming of low salinity water now from the East China Sea. 3. Estimation of optimum temperature and salinity per season based upon analysis for relationship between temperature of water and salinity of the bottom layer and the catch is : 15.2~16.4℃, 34.20~34.40‰ in spring(June); 14.4~ 17.0℃, 33.70~34.30‰ in summer(July~September); and 15.7~ 18.6℃, 33.70~34.50‰ in autumn(October~December). Hairtail are mostly caught at the Yellow Sea Warm Current and Tsushima Current with temperature over 14.5℃ and salinity over 33.70‰ at the bottom layers of the Cheju Strait. 4. Considering the relationship between the amount of hairtail catch and the water temperature of bottom layer, when the bottom water being above 14.0℃ flowed into Cheju Strait through the western entrance of the strait in summer, the ca-h appears to have been abundant. In contrast, the catch has been poor when the temperature of such water was recorded to be below 13℃ Therefore, distribution patterns of water at the bottom layer can be used as a forecast index whether the catch of a certain year will be good or poor.

In order to find out the environmental factors influencing the catch of anchovy lift nets in kamakbay, the three oceanographic factors, i. e., the water temperature, the salinity, the amount of chlorophyll-a were observed respectively from August 1 to 12, 1995 and from September 20 to 26, 1995, and each of them was compared with the catch of anchovy by the lift net. The results obtained are summerized as follow : 1) The water temperature was ranged from 17.3 to 29.6℃ and its difference between the surface and bottom was 1 to 3℃. In the three areas, A, B and C, the area A was the hightest in temperature, the area B being a second, and the area C being the lowest. 2) The salinity was ranged from 32.20 to 33.47‰ and its difference between the surface and bottom was not significant. In the three areas, the area A was the highest in salinity, the area B being a second, and the area C being the lowest. 3) The amount of chlorophyll-a was ranged from 0.19 to 5.30mg/m supper(3) and its difference among the three areas was not significant. Daily variation of the amount was very irregulated because the position operated was changed daily. 4) A comparison of the water temperature, the salinity and the amount of chlorophyll-a with the catch gave that the water temperature and the amount of chlorophyll-a had large influence on the catch and the salinity did not so. However, the influence of the amount of chlorophyll-a was larger than that of the water temperature. 5) The catch of anchovy was large respectively during two hours after sun set and during two hours before sun rise.

This study was performed with survay in the field and literature. The result were; 1. In Vietnam, They took their meal in three times a day. They have taken Nuoc nam (fish sauce) with sliced red pepper, half a lime, etc... in every day every night. Fish Sauce was prepared with small fish (generally fresh- water fish), the same amount of salt, and stored in 8 months, and made filltered fluid. It's Nuoc mam. They have gained protein sauce from it. 2. Their basic menu were composed with rice, soup, food with marine products and meat (generally pork), various vegetables, tropical fruit. 3. Food of cereals were Com Trang (white rice), Pho (rice noodle), Chao (rice gruel), Banh Trang (rice paper), Banh mi (bread) etc... Food of meat were Ho sua, Banh bao chien (barbecued little pork), Suon Nuon (grilled pork), Cha Lua (sausage of pork) etc..., Thit be nhung (grilled beef, Dog meat, Chicken, Duck, Frog. Food of fish were generally fresh-water fish, Ca Chien (grilled fish), Canh chua (soup with sour taste), Ca chem chung (steamed fish with fragrant vegetable), Lobster, Crab, Oyster, Cuttlefish, Shellfish, etc... Food of vegetables were Doa Hanh (Kimchi with a welsh onion), Rau xao hon hop (roasted vegetables), Goi Tom (salad), Canh he dau hu (soup) etc..., and They took much food of trophical fruit, Tra (Tea), Coffee, Lua Moi (distilled liquor). 4. For example, Their Daily meal were composed of Sup Bong Ca (Soup), Heo Sua, Banh Bao Chien (barbecued little Pork), Top Hap (steamed shrimp), Cua (steamed Crab), Luon Um (bioled a fresh-water eel), Lau Thap Cam, Hai Sam Sac Nam Dong Co, Trai Cay.

본 연구는 원양 다랭이 연승 어업의 어획량을 데이터 베이스 처리하여 합리적인 조업 계획의 수립과 어장 선정에 대한 기초 자료를 제공 하고자 하였다. 어획량 자료는 국립수산진흥원에서 발행한 '75~'92년의 18년 간의 12종의 다랭이 및 새치류의 통계자료를 이용하였으며, 데이터 베이스 처리를 위한 프로그램은 Quick basic으로 작성하였다. 데이터 베이스 프로그램은 구획별 조획율을 어장도에 나타내는 프로그램, 어획 마리수를 이용한 그래프 및 도표의 작성 프로그램, 그리고 어장평가 지수를 나타내는 프로그램 등으로 구성되어 있다. 1)연도구간별 어장도에서 보면, 조획율은 연도가 경과함에 따라 전반적으로 점차 낮아지는 경향이 나타났고 인도양은 그러한 현상이 두드러졌다. 또한 황다랭이의 조획율은 적도 부근의 서부 태평양에서 눈다랭이의 조획율은 동부 태평양에서 높게 나타났으며 조획율이 높게 나타난 해역은 과거의 인도양, 대서양에서 태평양으로 이동한 것으로 나타났다. 2)전 해역에서 황다랭이와 눈다랭이의 어획량 변동 패턴은 비슷하게 나타났으며, 12개 어장구역별 어획량은 태평양 북서 해역이 가장 부진하고, 인도양 서부, 태평양 서부 저위도 해역이 가장 좋았다. 3)어장 가치를 평가하는 시뮬레이션에서 12개 어장구역 중 경제성이 높은 어장은 태평양 저위도 해역의 서부, 중부, 동부, 인도양의 서부, 동부, 그리고 대서양 순으로 나타났으며, 북미대륙 서부역이 중간정도, 나머지 해역은 경제성이 낮은 어장으로 나타났다. 4)본 데이터 베이스 프로그램을 이용하여 방대한 어획량 자료를 분석하여 시기별, 위치별의 어종 및 어획량을 검토하고 어장 평가 시뮬레이션을 실시함으로써 경제성 있는 어장 선정 및 탐색을 할 수 있다고 판단된다.

In order to investigate the relation between the environmental properties and the catch fluctuation of set net fishing grounds located in the coastal waters of Yosu, oceanographic observations on the fishing grounds were carried out by the training ship ofYosu Fisheries University from January, 1990 to September, 1992, and the data obtained were compared with the catch data from the joint market ofYosu fisheries cooperative society from 1984 to 1993. The resuItes obtained are summerized as follows : 1. The ranges of water temperature and salinity in the fishing ground was 7.0 to 27℃.and 26.6 to 33.2‰, and water temperature increased from March to August and decreased from September to February of following year. 2. The salinity in the fishing grounds was relatively high without significant changes from November to June of the following year. From July, however, the salinity decreased to continue a low value till September and then increased. The salinity in the fishing ground was dominated mainly by the precipitation and its variation was large at the north entrance of set net fishing ground, influenced greatly by the land waters from the river of Somjin, but small in the offshore of the fishing grounds. 3. The fishes caught by the set nets were arranged in order of catch as follows; Spanish mackerel〉 Horse mackerel 〉 Sardine 〉 Anchovy 〉 Hair tail. The catches of Anchovy and Sardine were high in April to May and those of Hair tail in June to July, but Spanish mackerel and Horse mackerel were caught for whole period of fishing. Spanish mackerel was caught most in September and least in April and their means were largest in August and smallest in June. 4. The ranges of optimum water temperature for fishing by the set nets was 13.5 to 25℃., and in the ranges the catches increased with increasing temperature. The ranges of optimum salinity for fishing varied between 25.0 and 32.0‰.

This paper described on relation between the catches of tuna and the distribution of water temperature of eastern fishing ground of Tropical region in the Pacific Ocean. The data of catches and water temperature used in this paper were based log book which # 27 CHENG RONG(Gross tonnage : 399 ton) had been worked eastern fishing ground(Lat : 09˚N- 14˚S, Long : 115˚- 149˚W)from January to October, 1991. The obtained result are as follows : 1. On the relation between the catches and the geographical distribution, bigeye tuna was higher catches at Lat 4˚- 9˚N, Long 135˚- 139˚W area in the equatorial counter current region where surface water temperature was range of 27.5℃ to 27.9℃, yellowfin tuna was higher catches at Lat 4˚- 9˚S, Long 145˚- 149˚W in the south equatorial current region where surface water temperature was range of 28.0℃ to 28.4℃ and albacore tuna was higher catches at Lat 10˚- 14˚S, Long 120˚- 124˚W area in the south equatorial current region where surface temperature was range of 26.5℃ to 26.9℃ 2. On the relation between catches and distribution of vertical water temperature, bigeye tuna was higher catches at the water temperature of 10℃ to 12℃ on depth layer between 300m and 360m, yellowfin tuna was higher catches at the water temperature of 15℃ to 19℃ on depth layer between 180m and 280m and albacore tuna was higher catches at the water temperature of 12℃ to 14℃ on depth layer between 280m and 310m. Above the result, it seemed that bigeye tuna distributed deeper layer than yellowfin and albacore tuna.

득량만의 키조개 어장의 해양 환경을 알아보기 위하여 1994년 7월 12일(대조기)과 19일(소조기)에 걸쳐 득량만의 수형 분포 특성을 조사하였다. 득량만은 관측 기간중에 대조기와 소조기에 따른 빛의 연직감쇠계수(k)가 0.6인 곳을 경계로 하여 3개 해역으로 구분될 수 있었다. 조석 주기에 따른 k가 0.6인 등치선의 변화는 대조기에는 약 10m인 등수심선, 소조기에는 약 5m인 등수심선과 유사하게 분포하였다. 따라서 득량만의 수심 약 5~10m인 해역은 조석 주기에 따라서 수형의 특성이 뚜렷하게 바뀌는 수역이라고 할 수 있다. 즉, 수심 약 5~10m인 만 중앙 해역은 T-S diagram에서 대조기때는 수심이 얕은 해역의 수형군에 가까이 분포하고, 소조기때에는 수심이 깊은 수형군에 가까이 분포하였다. 그리고 성층 정도를 나타내는 변수인 log 하(10)(H/U 상(3))의 값은 수심 5m와 10인 등수심선에서 약 2.1~2.2의 값을 나타내었다. 특히, 본 연구 기간인 1994년 7월 동안은 혹서와 갈수로 인하여 예년치보다도 기온은 약 2℃이상 높았으며, 강수량은 예년치보다도 훨씬 낮은 음의 값을 나타내었다. 이러한 영향으로 인하여 득량만의 수괴의 밀도는 관측 기간동안 주로 수온에 의해서 결정되고 있었다. 앞으로는 기상 자료 및 득량만에서의 과거 누년자료를 분석하여, 이상(abnormal) 고수온년에 대한 만내의 물리적인 변동, 조류와 해저 지형에 기인한 내부파의 형성이나 연속 관측에 의한 급조등에 관한 연구도 필요하리라 생각된다.