• 제목/요약/키워드: Southern Waters of Korea

검색결과 347건 처리시간 0.028초

New Occurrences of Two Penaeid Species (Crustacea: Decapoda: Dendrobranchiata) in Korean Waters

  • Kim, Jung Nyun;Choi, Jung Hwa;Lee, Jeong-Hoon;Kim, Joo Il
    • Fisheries and Aquatic Sciences
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    • 제16권4호
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    • pp.325-329
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    • 2013
  • New occurrences in Korean waters were recorded for two penaeid species: Atypopenaeus stenodactylus (Stimpson, 1860) and Metapenaeopsis toloensis Hall, 1962, which were previously known from the Indo-West Pacific up to southern Japan. The specimens were collected from the southeastern coast of Korea by a shrimp beam trawl. The former is the only known member of the genus Atypopenaeus and the latter is the sixth species of the genus Metapenaeopsis reported in Korea. Morphological descriptions and illustrations with color photographs of the specimens are given. At present, the Korean Penaeidae consist of 20 species in 11 genera. A key to the Korean genera of family Penaeidae is also presented.

2000년 여름 남해안에 나타난 Cochlodinium polykrikoides 우점 적조의 발생 특성 (The Outbreak, Maintenance, and Decline of the Red Tide Dominated by Cochlodinium polykrikoides in the Coastal Waters off Southern Korea from August to October, 2000)

  • 정창수;이창규;조용철;이삼근;김학균;정익교;임월애
    • 한국해양학회지:바다
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    • 제7권2호
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    • pp.68-77
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    • 2002
  • 2000년 한반도 남해안에서 발생한 Cochlodinium polykrikoides 적조 초기발생, 진행과 소멸현상을 현장과 NOAA 위성 표층수온 자료를 이용하여 검토하였다. 일반적으로 C. polykrikoides 적조는 1995년에서 1999년에는 적조 띠가 고흥 나로도해역에서 최초 발생되었으나, 2000년에는 여수해만 해역에서 최초로 발생되었다. 이는 한반도 남해해역에서 여러 해수가 영향을 미쳤기 때문으로 생각된다 : 1) 대마난류와 남해연안류, 2) 진도냉수대와 남서해 연안수 및 3) 남동연안의 저온수와 외양난류수, 이 기간동안 실시한 현장조사에서는 C. polykrikoides의 유영세포가 이들의 경계역에 집적되는 경향을 나타내었는데, 특히 8월말에 대마난류와 남해연안류 사이의 남해 해양전선이 여수해만에서 형성되어 2000년 C. polykrikoides 적조가 바로 이 지점에서 시작하는 것을 관찰할 수 있었다.(8월 22일). 이 C. polykrikoides 우점 적조는 Alexandrum tamarense, Gymnodinium mikimotoi, Skletonema coastatum, 그리고 Chaetoceros spp.와 혼합하여 발생하였다. 적조발생 기간 중에 한반도에는 'Prapiroon'과 'Saomai' 2개의 태풍이 C. polykrikoides 적조세력에 영향을 미쳤다. 태풍 'Prapiroon'이 통과한 후 C. polykrikoides 유영세포의 수는 최대를 보였고, 태풍 'Saimai' 통과 후 적조는 소멸하였다(9월 20일). 10월 5일에는 진해만과 한산-거제만에서 C. polykrikoides 적조가 발생하였는데, 이때의 위성사진은 22$^{\circ}C$의 수온전선이 한산-거제만을 거쳐 진해만까지 깊숙이 관입되어 있었으며, 적조발생해역 및 현장수온도 일치하고 있었다. 또한 이 지역에서 가을과 겨울철에 우점 출현하는 Akashiwo sanguinea(=Gym, sanguineum)와 C. polykrikoides이 함께 적조를 형성하였다.

한국 남해안의 잠재어업자원 조사연구 - 저층크롤 어획량의 생물학적 조성 - (Investigations of the Potential Fisheries Resources in the Southern Waters of Korea - Biological Composition of Demersal Trawl Catches -)

  • 이대재;김진건;신형호
    • 수산해양기술연구
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    • 제34권3호
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    • pp.241-258
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    • 1998
  • 우리나라 남해안에 대한 어업생물자원의 평가와 관리 및 유효이용방안 등을 모색하기 위한 기초연구로서, 남해안의 전해역에 설정한 생물학적 샘플링 정점을 대상으로 저층트롤에 의한 시험조업을 실시하고, 이들 정점에서 샘플링된 어획물의 생물학적 조성, 計量魚探調査와 관련한 漁獲選擇性의 영향 底棲漁業資源의 분포실태 등을 분석, 고찰한 결과를 요약하면 다음과 같다. 1. 1996년 10월과 1997년 1월, 3월, 7월~8월, 9월 ~ 10월에 우리나라 남해안에 설정한 64개의 조사정점을 대상으로 저층트롤에 의한 시험조업을 실시한 결과, 魚類 114종, 軟體類 8종, 甲殼類 7종(총 129종)에 총 9,9910.6 kg이 어획되었는 데, 이 중에서 어류의 점유비율은 전갱이 19.8%, 고등어 15.0%, 달강어 6.2%, 전어 6.1%, 병어 5.1%, 아귀 5.1%, 눈볼대 3.6%, 밴댕이 3.5%, 꼼치 3.4%, 꼬치고기 1.4% 등이었고, 甲殼類로서는 깨다시꽃게 0.34%, 보리새우 0.18% 등이었고, 頭足類로서는 창꼴두기 9.0%, 살오징어 5.8%, 참갑오징어 0.28% 등이 어획되었다.2. 1996년 ~ 1997년 사이에 우리나라 남해안에 설정한 트롤조사정점을 대상으로 실시한 저층트롤조업에 의해 어획된 어획량을 트롤예망층의 공간체적으로 나누어 산출한 단위체적당에 대한 어업생물자원의 분포밀도는 해역, 계절, 어획 어종의 조성, 조업시간 등에 따라 큰 차이를 나타내었으나, 그 값은 17.9 x 10$^{-6}$ ~ 1,440.9 x 10$^{-8}$kg/m$^{3}$의 범위였고, 그 평균적인 분포밀도는 153.8 x 10$^{-6}$kg/m$^{3}$이었다. 3.우리나라 남해안에 설정한 64개의 조사정점에서 어구의 파망사고 및 조업장애가 없었던 50개의 트롤정점을 대상으로 끝자루와 커버 네트에 의한 어획비율을 조사한 결과, 커버 네트에 의한 어획비율은 0.7 ~ 91.9%의 범위로서, 그 평균적인 어획비율은 44.4%였다. 이처럼 우리나라 남해안에서는 어족자원의 감소 등에 기인하여 소형어의 어획비율이 매우 높은 실정이기 때문에 향후, TAC제도가 도입되는 경우, 조업어선에서는 상품 가치가 적은 이들 소형어를 바다에 그대로 폐기할 우려가 있으므로 소형어의 어획방지와 서식환경의 보호를 위한 대책의 수립이 절실히 요구된다.

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남해무인도서 백도와 서귀포 인근 섶섬에서 맹독성 저서와편모조류 Gambierdiscus spp.의 출현 (Occurrence of the Toxic Benthic Dinoflagellate Gambierdiscus spp. in the Uninhabited Baekdo Islands off Southern Coast and Seopsom Island in the Vicinity of Seogwipo, Jeju Province, Korea)

  • 백승호
    • Ocean and Polar Research
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    • 제34권1호
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    • pp.65-71
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    • 2012
  • Gambierdiscus toxicus, Adachi et. Fukuyo, is a benthic ciguatoxin-producing armored dinoflagellate, often attached to macroalgae. This organism is the primary causative agent of ciguatera fish poisoning which occurs in tropical and subtropical regions. However, regardless of the fact that the population of Gambierdiscus spp. has expanded to such temperate areas from sub-trophic and trophic areas, monitoring of G. toxicus has been lacking in the Korean coastal waters of temperate areas. This study was performed at the uninhabited Baekdo Islands off the southern coast of Korea and at Seopsom Island in the vicinity of Seogwipo, Jeju Province during April and May, 2011. Cell densities of Gambierdiscus spp. on macroalgae at Baekdo and Jeju Island ranged from zero to 56.4 cells $g^{-1}$. Maximum density was recorded on the brown alga Cladophora japonica at St. 3 of Jeju Island. In particular, the cell densities of Gambierdiscus spp. were influenced by the substrate characteristics of macroalgae. In the future, the continuous monitoring of toxic benthic dinoflagellate is necessary to predict and prevent ciguatera poisoning in Korean coastal waters.

제주도 남부 연안 해역에서 채집된 농어목 망둑어과 한국첫기록종, Callogobius shunkan (First Record of a Goby, Callogobius shunkan (Perciformes: Gobiidae) from the Southern Coastal Waters of Jejudo Island, Korea)

  • 안정현;김병직;김상길
    • 한국어류학회지
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    • 제32권4호
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    • pp.251-256
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    • 2020
  • 우리나라 연안성 어류자원 미발굴 분류군 탐색을 위해 제주도 남부 연안해역에서 SCUBA를 이용한 수중조사 과정 중 2015년 9월 수심 약 15미터에서 망둑어과 한국첫기록종인 Callogobius shunkan 2개체(표준 체장 54.9~66.1 mm)를 채집하였다. 본 종은 살아있을 때 암갈색 바탕에 등지느러미 기저부에서 시작하는 3개의 흑갈색 안상반문이 있는 점, 두부 감각관과 잘 발달된 피습에 공기열이 배열되어 있는 점(특히 비공과 안와 후방에 공기열이 있는 점), 배지느러미막이 잘 발달된 점, 흑갈색 바탕의 체색에 백색 반점이 산재하는 특징이 있다. 본 종의 신한국명으로 '주름망둑'을 제안한다.

2013~2017년 연안해역별 해양기상요소의 시·공간 변화 및 해무발생시 특성 분석 (Temporal and Spatial Variations of Marine Meteorological Elements and Characteristics of Sea Fog Occurrence in Korean Coastal Waters during 2013-2017)

  • 박소희;송상근;박형식
    • 한국환경과학회지
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    • 제29권3호
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    • pp.257-272
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    • 2020
  • This study investigates the temporal and spatial variations of marine meterological elements (air temperature (Temp), Sea Surface Temperature (SST), and Significant Wave Height (SWH)) in seven coastal waters of South Korea, using hourly data observed at marine meteorological buoys (10 sites), Automatic Weather System on lighthouse (lighthouse AWS) (9 sites), and AWS (20 sites) during 2013-2017. We also compared the characteristics of Temp, SST, and air-sea temperature difference (Temp-SST) between sea fog and non-sea-fog events. In general, annual mean values of Temp and SST in most of the coastal waters were highest (especially in the southern part of Jeju Island) in 2016, due to heat waves, and lowest (especially in the middle of the West Sea) in 2013 or 2014. The SWH did not vary significantly by year. Wind patterns varied according to coastal waters, but their yearly variations for each coastal water were similar. The maximum monthly/seasonal mean values of Temp and SST occurred in summer (especially in August), and the minimum values in winter (January for Temp and February for SST). Monthly/seasonal mean SWH was highest in winter (especially in December) and lowest in summer (June), while the monthly/seasonal variations in wind speed over most of the coastal waters (except for the southern part of Jeju Island) were similar to those of SWH. In addition, sea fog during spring and summer was likely to be in the form of advection fog, possibly because of the high Temp and low SST (especially clear SST cooling in the eastern part of South Sea in summer), while autumn sea fog varied between different coastal waters (either advection fog or steam fog). The SST (and Temp-SST) during sea fog events in all coastal waters was lower (and more variable) than during non-sea-fog events, and was up to -5.7℃ for SST (up to 5.8℃ for Temp-SST).

한국해역의 식물플랭크톤의 연구. IV. 동해, 남해 및 서해해역의 식물플랭크톤 (Phytoplankton Studies in Korean Waters. IV. Phytoplankton in the Adjacent Seas of Korea)

  • 최상
    • 한국해양학회지
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    • 제4권2호
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    • pp.49-67
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    • 1969
  • A quantitative phytoplankton study in Korean waters was commenced in 1964 as a part of the primary production studies of Koreans seas, and it was continued with the cruises for Cooperative Studies of the Kuroshio(C.S.K) in 1965-1968. Phytoplankton samples were taken by dipping about 500ml of sea water from the surface, and then fixed by ading neutralized formlin. This report deals with the results obtained during 1965-1966. I examined a total of 298 samples of surface phytoplankton collected in the wate neighboring Korea in the above-mentioned period, and detected 147 species of diatoms and 22 species of dinoflagellates. Among them 123 species of diatoms and 18 species of dinoflagellates occured in the Japan Sea region, 133 species of diatoms and 11 species of dinoflagellates occured in the Korea Strait region, and 49 species of diatom and 8 species of dinoflagellates occured in the Yellow Sea region. And thd phytoplankton standing crops are dept in a fair abundance in the Japan Sea area all the year round, and are poor in the Yellow Sea area. The seas surrounding Korea are divided into seven regions by the planktological characteristics; northern and southern parts of the Japan Sea, eastern, western and southern parts of the Korea Strait, southern and northern parts of the Yellow Sea. The representative of the phytoplankton community in each sea region is generalized as follows; northern part of the Japan Sea is dominant with Chaetoceros group, southern part of the Japan Sea is dominant with Chaetoceros group and Skeletonema costaum, eastern part of the Korea Strait is dominant with Chaetoceros group and Pleurosigma sp., southern part of the Korea Strait is dominant with Chaetoceros group and Rizosolenia group, western part of the Korea Strait is most poor in phytoplankton, southern part of the Yellow Sea is dominant with Pleurosigma sp. and Coscinodiscus group, and northern part of the Yellow Sea is dominant with Pleurosigma sp. and Eucampia zoodiacus. Chaetoceros curvisetus, Leptocylindrus danicus, Pleurosigma normanii, Thalassionema nitzschioides, Thalassiothrix flauenfeldii appeared all the year round in the neighboring sea of Korea. There were 24 species (18 species of diatoms and 6 species of dinoflagellates) of the pecuriar phytoplankton in the Japan Sea, 27 species (25 species of diatoms and 2 species of dinoflagellates) of that in the Korea, and 7 species (5 species of diatoms and 2 species of dinoflagellates) of that in the Yellow Sea, respectively.

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Modification of Sea Water Temperature by Wind Driven Current in the Mountainous Coastal Sea

  • Choi, Hyo;Kim, Jin-Yun
    • 한국환경과학회:학술대회논문집
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    • 한국환경과학회 2003년도 International Symposium on Clean Environment
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    • pp.177-184
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    • 2003
  • Numerical simulation on marine wind and sea surface elevation was carried out using both three-dimensional hydrostatic and non-hydrostatic models and a simple oceanic model from 0900 LST, August 13 to 0900 LST, August 15, 1995. As daytime easterly meso-scale sea-breeze from the eastern sea penetrates Kangnung city in the center part as basin and goes up along the slope of Mt. Taegullyang in the west, it confronts synoptic-scale westerly wind blowing over the top of the mountain at the mid of the eastern slope and then the resultant wind produces an upper level westerly return flow toward the East Sea. In a narrow band of weak surface wind within 10km of the coastal sea, wind stress is generally small, less than l${\times}$10E-2 Pa and it reaches 2 ${\times}$ 10E-2 Pa to the 35 km. Positive wind stress curl of 15 $\times$ 10E-5Pa $m^{-1}$ still exists in the same band and corresponds to the ascent of 70 em from the sea level. This is due to the generation of northerly wind driven current with a speed of 11 m $S^{-1}$ along the coast under the influence of south-easterly wind and makes an intrusion of warm waters from the southern sea into the northern coast, such as the East Korea Warm Current. On the other hand, even if nighttime downslope windstorm of 14m/s associated with both mountain wind and land-breeze produces the development of internal gravity waves with a hydraulic jump motion of air near the coastal inland surface, the surface wind in the coastal sea is relatively moderate south-westerly wind, resulting in moderate wind stress. Negative wind stress curl in the coast causes the subsidence of the sea surface of 15 em along the coast and south-westerly coastal surface wind drives alongshore south-easterly wind driven current, opposite to the daytime one. Then, it causes the intrusion of cold waters like the North Korea Cold Current in the northern coastal sea into the narrow band of the southern coastal sea. However, the band of positive wind stress curl at the distance of 30km away from the coast toward further offshore area can also cause the uprising of sea waters and the intrusion of warm waters from the southern sea toward the northern sea (northerly wind driven current), resulting in a counter-clockwise wind driven current. These clockwise and counter-clockwise currents much induce the formation of low clouds containing fog and drizzle in the coastal region.

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Primary Production System in the Southern Waters of the East Sea, Korea III. Vertical Distribution of the Phytoplankton in Relation to Chlorophyll Maximum Layer

  • Shim, Jae-Hyung;Park, Jong-Gyu
    • Journal of the korean society of oceanography
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    • 제31권4호
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    • pp.196-206
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    • 1996
  • Vertical profiles of the chlorophyll ${\alpha}$, phytoplankton abundance, nutrients and sigma-t were compared with the vertical distribution of phytoplankton species in conjunction with $^{14}$C primary production in the Southern Waters of the East Sea, Korea. In the upper mixed layer the water column was only weakly stratified and ambient nitrogenic nutrient concentrations were markedly depleted. Dissolved silicate seemed to be another limiting nutrient in the surface layer. The occupation of different water depths by several dominant diatom species was well explained by the degree of silicification of each cell and the silicate concentration of ambient seawater. Subsurface chlorophyll maxima were continuously observed in the lower parts of the euphotic layer and the depth coincided with nutricline, supporting our view that chlorophyll maximum was sustained partially by enhancement of in situ growth of phytoplankton and partially by increase of cellular chlorophyll content. The persistence of chlorophyll maximum layer was attributed to the physiological adaptation of the phytoplankters to low light intensities and to the utilization of regenerated nutrients. Integrated water column production of organic matter by photosynthesis appeared to be better related to phytoplankton cell division than to the cell growth in terms of biosynthesis of pigments and other intracellular components.

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