• Journal of the korean society of oceanography
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• 제37권4호
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• pp.212-223
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• 2002

Cochlodinium polykrikoides bloom in 1995 was studied with a focus on an unusual coastal environment in the South Sea of Korea. Data on temperature, salinity, and zooplankton biomass during 1965-1998 and nutrients during 1990-1998 and chlorophyll-a during 1995-1998 were used in this study. These data were obtained from the serial oceanographic observations in Korean waters carried out by the National Fisheries Research and Development Institute. In 1995 the C. polykrikoides bloom began in the coastal area around Narodo Island in August and consequently occurred to the whole coastal area of the South and East Seas of Korea. During June-October 1995, the coastal environment was unusual compared with the long-term means during 1965-1998. In June 1995, sea surface temperature was 1-2$^{\circ}C$ warmer than in other years in all coastal areas, while salinity was high only to the east of Jeju Island. In August 1995, a strong coastal front appeared inshore of a line between Jeju and Tsushima Islands. In particular, a strong coastal front which showed the characteristics of upwelling front occurred in the coastal area around Narodo and Sorido Islands, not only because of a strong intrusion of the Tsushima Warm Current but also because of the upwelling of cold bottom water. Salinity was low in the neighboring waters of western side of Jeju Island. Nutrients and chlorophyll-a were high in the inshore area between Narodo and Sorido Islands in 1995 in contrast with the other years and areas. Zooplankton showed an unusually high abundance in the coastal area in October 1995. We conclude that the Tsushima Warm Current strongly influenced the South Sea of Korea in 1995 and created strong upwelling front bordering cold upwelled water in the coastal area around Narodo and Sorido Islands. It leads us that these physical structures introduce the favorable environment for the development of C. polykrikoides blooms. We suggest that C. polykrikoides has a bio-physical tolerance of high shear and stress and prefers frontal and upwelling relaxed areas as its habitat. We also find that nutrients were not supplied to the coastal area from the offshore where a low salinity water mass with high nutrients appeared around Jeju Island. Because the strong upwelling front protect the reach of offshore low saline water mass. The main source of nutrients was the upwelled water mass in the coastal area of Wando-Narodo-Sorido.

• 한국수산과학회지
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• 제34권3호
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• pp.225-237
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• 2001

소리도를 포함한 주변 해역에서 저서동물 군집 구조 파악을 위한 조사를 수행하였다. 저서동물의 채집은 광양만 입구에서부터 소리도 주위에 이르는 해역에 여름철인 1996년 8월, 가을철인 11월에는 12개 조사 정점을, 겨울철인 1997년 2월과 봄철인 1997년4월에는 정점 13과 14를 추가하여 14개 정점에서 van Veen grab(표면적 $0.1 m^2$)을 사용하여 매 정점당 3회씩 해저 퇴적물을 인양하였다. 조사결과 총 217종의 저서동물이 출현하였으며, 다모류가 80종으로서 전체 출현종수의 약 $37\%$, 갑각류는 60종으로서 약 $28\%$ 그리고 연체동물은 46종으로서 약 $21\%$를 차지하였다. 밀도는 1,068개체/$m^2$였는데 다모류가 904개체/$m^2$로서 가장 우점하여 전체 밀도의 약 $85\%$를 차지하였다. 생체량은 $110.02g/m^2$였으며, 극피동물의 생체량이 가장 우점하여 $57.62g/m^2$로서 전체 생체량의 와 $52\%$를 차지하였다. 주요 우점종은 연안 유기 오염역에서 주로 출현하는 Tharyx sp., Lumbrineris japonica, Magelona japonica 였다. 이들은 각각 582개체/$m^2$, 72개체/$m^2$ 그리고 41개체/$m^2$의 밀도로 출현하였는데, 외해역인 소리도 주변 정점에서는 극히 밀도가 낮았다. 집괴분석 결과 본 조사해역의 저서동물 군집은, 소리도 동측에서 광양만과 여수항에 인접한 정점군 (정점군 A)과 외해역의 영향을 받는 해역 (정점군 B, C, D)로 구분되었다. 소리도 주변 해역의 정점군 C에서는 정점별 저서동물의 출현종수가 가장 많고 밀도와 생체량은 상대적으로 낮아 다양도가 높았다. 저서동물 가운데 Ampeliscidae spp. 및 Amphipoda의 밀도는 PAHs농도와 음의 상관관계를 나타내었다.

• 수산해양교육연구
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• 제29권3호
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• pp.646-654
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• 2017

소리도 주변해역에서 어류의 종조성을 파악하기 위하여 1999년 8월과 10월, 2000년 2월과 5월에 총 4회에 걸쳐 조사하였으며, 소형 Trawl 어망을 5톤급 어선으로 30분간 예인하였고 소리도 주변해역에 서식하고 있는 어류의 종조성은 총 9목 34과 36속 39종 1920.6개체/$1,000m^3$가 출현하였고 그 중 준치가 460.2개체/$1,000m^3$로 23.96%를 차지하여 가장 많은 개체수가 출현하였으며, 다음으로 고등어가 312.4개체/$1,000m^3$로 16.27%, 멸치가 210.9개체/$1,000m^3$로 10.98% 순으로 출현하였다. 주요 어종의 출현빈도 조사 결과, 연중 출현한 어종은 붕장어, 준치, 양태, 주둥치, 베도라치 실망둑 등으로 소리도 연안의 정착성 어종이였고, 특정 계절에만 출현한 어종은 군평선이와 얼룩통 구멍은 봄철에만 출현하였으며, 풀넙치는 여름에만 출현하였고, 돌돔, 고등어 그리고 삼치는 가을에만 출현하였다. 군집분석을 분석한 결과 종 다양도지수는 1.970~2.528, 풍부도지수는 2.747~4.729, 균등도지수는 0.669~0.759, 우점도지수는 0.455~0.576로 나타났다. 계절별 군집의 유사도는 봄철과 겨울철이 0.0043로 가장 작아 군집상이 매우 유사하였으며, 여름철과 겨울철에는 우점종과 출현종이 유사하지 않아 상대거리차가 0.10135로 군집상에 차이가 가장 컸다.

• 한국해양학회지
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• 제11권2호
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• pp.77-88
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• 1976

The water movements in the south sea of Korea are deduced from the distributions of water properties. In summer the flow path of the Tsushima Current is deflected off from the Korean coast; between the coast and the current there exist eddies. Cyclonic eddies are particularly dominant in the southeastern area of Sorido Is. In winter, the sunken coastal water flows out along the bottom toward the southeast, and compensation is made at the surface by the coastward intrusion of off-shore waters. The so-called coastal counter- current of the area seems to be a cyclonic eddy which prevails in summer and autumn.

• 수산해양기술연구
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• 제29권1호
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• pp.1-10
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• 1993

In order to investigate the environmental properties of set net grounds located in the coastal waters of Yeosu, oceanographic observations on the fishing grounds were carried out by the training ship of Yeosu Fisheries University from Jun. 1988 to Dec. 1990. The resultes obtained are summarized as follows; 1) The water mass in the fishing grounds were divided into the inner water (29.50-31.00$\textperthousand$), the mixed water (31.10-32.70$\textperthousand$) and the offshore water (32.70-34.30$\textperthousand$) according to the distribution of salinity from T-S diagram plotted all salinity data observed from Jun. 1988 to Dec. 1990. In spring the mixing water prevailed and in summer the inner and mixing water. But in autumn and winter the mixing and offshore waters prevailed. 2) The inner water which was formed by land water from the river of Somjin and the precipitation in the Yeosu district flowed southerly along the coast of Dolsando and spread south-easterly in the vicinity of Kumodo. The inner water and offshore water which supplied from the vicinity of Sorido and Yokchido formed the thermal front and halofront. 3) As the mixing water flowing from the western sea of Cheju to the southern coast of korea was low in temperature, the water mass of low temperature which appeared at the offshore bottom of Sorido in summer was considered not to be the Tsushima warm current. 4) As vertical mixing was made frequently in spring, autumn and winter, the differences in temperature and salinity between surface and bottom was respectively small. In summer, however, the mixing was not made because of the inner water expanded offshore through the space between surface and 10m layer and so a thermocline of $2.0^{\circ}C$/10m and halocline of 4.0$\textperthousand$/10m respectively in vertical gradient was formed. 5) In the vicinity of Dolsando and Kum a water low in salinity prevailed, but in the vicinity of Namhaedo and YoKchido the reverse took place. The inner and mixing waters formed at these arease was limited to the observation area not to spread widely.

• 한국양식학회지
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• 제17권1호
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• pp.51-57
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• 2004

소리도 주변해역에서 서식하는 새우류의 종조성과 계절변동을 파악하기 위하여 2000년 6월부터 2001년 5월까지 매월 1회씩 사리기간중 간조시에 채집하였다. 조사기간 동안 채집된 새우는 6과 16종이었으며, 그라비새우, Ρ. gravieri, 꽃새우, Τ. curvirostris, 마루자주새우, C. hakodatei, 중하, Μ. joyneri등이 연중 우점하였다. 월별 출현종수는 8월, 10월, 11월에 14종으로 가장 많이 출현하였으며, 하계인 6월과 7월에 각각 8, 10종으로 가장 적은 종이 출현하였다. 종다양도 지수는 0.14∼0.82의 범위를 나타내었으며, 5∼7월에는 비교적 낮은 값을 보였는데, 이는 균등도 지수에서도 마찬가지 결과였으며, 반면 9∼12월에는 비교적 높은 종다양도 지수 값을 보였다. 본 연구 해역에서 채집된 새우류는 출현 양상에 따라 주거종과 계절종, 일시방문종으로 나눌 수 있었다.

• ALGAE
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• 제19권4호
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• pp.339-347
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• 2004

Seaweed community of the sub tidal rocky habitats along the coast of Geumo Archipelago in the central South Sea of Korea is described. This area is characterized by archipelago in which islets are separated by shallow bottom sediments (primary, muddy sand), and turbidity is generally high due to the resuspension of bottom sediments. The hard substrata available for algal attachment are limited to less than 10 m in depth. Thirty sites were randomly chosen along the coast from August 2003 to September 2003 and a 50 m long transect was established at each site. The transect began at a depth of 1 m and ended at the depth of 9 m. The percent cover of all species other than crustose coralline algae was estimated at 2 m depth intervals along the transect using a 0.25 m$^2$ PVC quadrat with 25 squares. Thirty-six species were identified including 6 Chlorophyta, 10 Phaeophyta and 20 Rhodophyta. Species with more than 5% mean bottom cover were Gelidium amansii, Corallina pilulifera, Amphiroa dilatata and Carpopeltis cornea, which formed dense turf-forming algal assemblages at 1-5 m depth. At all sites except S11-S15 located in the western coast of Sorido, bottom covers of seaweed species at the depth deeper than 7 m were less than 6%. The lower limit of algal assemblages was 9 m in depth. We speculate that the limited water clarity and vertical extent of hard substrata available for the settlement of seaweed species are the direct cause of reducing the diversity, abundance and distributional extent of algal assemblages in the area.

• 수산해양기술연구
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• 제30권3호
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• pp.142-149
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• 1994

In order to investigate the environmental properties of set net grounds located in the coastal waters of Yeosu. The current in the vicinity of set net grounds was observed by drogue and current meter in 1990 and 1992. The results obtained are summarized as follows: The direction of tidal current at the north enterance of Yeosu bay was southerly in ebb and northwesterly in flood without the distiction of the neap tide and the spring tide. In spring tide the maximum Velocity of the tidal current was 68 cm/sec in ebb and 66 cm/sec in flood. In neap tide the maximum velocity of the tidal current was 37 cm/sec in ebb and 35 cm/sec in flood. And so the direction of residual current was the south ward mainly and 21 cm/sec. The direction of tidal current at set net fishing grounds was southwesterly in ebb and westerly or northwesterly in flood. Regardless of the distinction of neap and spring. The maximum velocity of the current in spring tide was 50 cm/sec in ebb and 40 cm/sec in flood and that in neap was 28 cm/sec in ebb and 25 cm/sec in flood. In spring tide the speed vector along the major axis of semidiurnal tide component was three times as large as diurnal tide. In neap tide, however, the speed vector was about 50% less then that in spring tide, and the semidiurnal tide and diurnal tide were equal in the size of current ellipse and the direction of major axis. The sea area had a southwesterly residual current. 11 cm/sec in spring tide and 7 cm/sec in neap tide. According to the result of drogue tracking, the vicinity of set net fishing ground had a southerly residual current which formed in Yeosu Bay and a weak westerly residual current toward Dolsando from Namhedo. Therefore, set net fishing ground in coastal water of Yeosu was distributed in boundary of inner water which formed from Seamjin river and offshore water supplied from the vicinity of Sorido and Yochido.

• 수산해양기술연구
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• 제35권3호
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• pp.301-311
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• 1999

The investigation to evaluate the possible effects of fish behaviour on acoustic target strength was carried out during the 1997 and 1998 hydroacoustic-demersal trawl surveys in the southern waters of Korea.The swimming speed and the target strength of individual, acoustically resolved fished swimming through the sound beam were measured using the split-beam tracking method on board R/V Kaya.The results obtained can be summarized as follows:1. The alongship and athwartship angles between -3dB poionts of a hull mounted 38 kHz split beam tranducer used in these surveys was >$3.76^{\circ}\;and\;6.74^{\circ}$ respectively, and the equal energy contour obtained from the measured beam pattern showed approximately the circular pattern. 2. The swimming speed measured off the south coast of Sorido in 23 January 1997 ranged 0.10 to 0.80 m/s with the average swimming spped of 0.36 m/s, and the target strength ranged -64.8 to -31.7 dB with the average target strength of -52.7 dB. The most dominant species sampled in this survey area were Japanese scaled sardine, Sardinella zunasi and Konoshiro gizzard shad, Konosirus punctatus, respectively.3. The swimming speed measured off the east coast of Kojedo in 24 March 1997 ranged 0.10 to 1.10 m/s with the average swimming speed of 0.40 m/s, and the target strength ranged -64.8 to -51.5 dB with the average target strength of -59.2 dB. The most dominant species sampled in this survey area were Swordtip squid, Photololigo edulis, Konoshiro gizzard shad and Japanese flying squid, Toddarodes pacificus, respectively and the swimming activity of these species seems to be controlled at speeds between 0.20 and 0.60 m/s. 4. The swimming speed measured the south coast of Kojedo in 25 March 1997 ranged 0.10 to 1.40 m/s with the average swimming speed of 0.51 m/s and the target strength ranged -64.3 to -47.7 dB with the average target strength of -55.1 dB. The most dominant species sampled in this survey area were Swordtip squid, Blotchy sillage, Sillago maculata and japanese scaled sardine, respectively and the swimming activity of these species seems to be controlled at speeds between 0.20 and 0.70 m/s.5. The swimming speed measured during morning twilight in the southeastern water of Cheju Island in 11 July 1998 ranged 0.20 to 1.0 m/s with the average swimming speed of 0.53 m/s, and the target strength ranged -65.0 to -47.0 dB with the average target strength of -57.1 dB. The most dominant species sampled in this survey area were Swordtip squid, Black scraper, Thamnaconus modesutus and japanese flying squid, respectively and the tile angle ranged$ +28^{\circ}\;to\;+2^{\circ}$ with the average tilt angle of -8.1$^{\circ}$ showing the downward migration.

• 한국해양학회지:바다
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• 제6권2호
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• pp.49-62
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• 2001

Cochlodinium polykrikoides 유해성적조 발생지역인 한국 남해 나로도와 소리도 사이 해역의 물리적인 환경을 연구하기 위하여 1998년 5월31일부터 9월 24일까지 7회에 걸쳐 수온 및 염분을 관측하였다. 연구해역의 표층에서 30m깊이까지의 수층에서는 관측 초기인 춘계부터 하계로 갈수록 수온이 증가하고 염분은 낮아지는 물성의 계절적인 변화가 뚜렷하였는데 수층전체의 평균수온은 총 조사기간동안 $6^{\circ}C$ 증가하고 평균염분은 2.71 psu 낮아졌다. 관측된 평균염분의 변화는 연구해역의 강수와 인접육지에 의해 공급될 수 있는 담수량만으로는 설명할 수 없었으며, 남해외해역으로부터 유입되는 저염수에 의해 일어났을 것으로 해석되었다. 이 해역에서 적조의 발생시기, 진행시기 및 적조가 사라진 시기에 염분의 공간적인 분포가 다른 특징을 보였으며, 특히 적조가 사라진 시기에는 염분이 직전 시기에 비해 크게 낮아지고 수층구조도 직전시기의 성층구조에서 혼합층구조로 변화하였는데, 이와 같은 변화는 남해 외해역으로부터 저염수의 유입으로만 설명할 수 있었다. 이로부터 물리적인 해수유동이 이 해역에서 적조가사라진 주요한 원인의 하나로 제시되었다. 본 연구결과는 차후 남해 연안역의 적조현상을 이해하기 위해서는 인접 육지로부터 유입되는 환경적 요소들은 물론 대상해역을 포함한 남해 외해역의 해수순환특성, 그리고 해수순환에 의해 이송되는 해수의 물리, 화학 및 생물학적 요소를 종합적으로 연구해야할 필요성을 시사한다.