• 제목/요약/키워드: southeastern Korea

검색결과 591건 처리시간 0.029초

제주 남동부 지역을 대상으로 한 WindPRO의 발전량 예측에 관한 연구 (Study on the Power Performance on WindPRO Prediction in the Southeast Region of Jeju Island)

  • 현승건;김건훈;허종철
    • 한국신재생에너지학회:학술대회논문집
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    • 한국신재생에너지학회 2010년도 춘계학술대회 초록집
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    • pp.184.1-184.1
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    • 2010
  • In order to research the way to evaluate wind resource without actual Met Mast data, this paper has been carried out on the southeastern region of Jeju island, Korea. Although wind turbine has been an economical alternative energy resource, misjudging the prediction of lifetime or payback period occurs because of the inaccurate assessment of wind resource and the location of wind turbine. Using WindPRO(Ver. 2.7), a software for wind farm design developed by EMD from Denmark, wind resources for the southeastern region of Jeju island was analyzed, and the performance of WindPRO prediction was evaluated in detail. Met Mast data in Su-san 5.5Km far from Samdal wind farm, AWS in Sung-san 4.5km far from Samdal wind farm, and Korea Wind Map data had been collected for this work.

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한반도 남동부의 진원위치 재분석 (Reanalysis of hypocenters around the southeastern area of the Korean Peninsula)

  • 박정호;지헌철;강익범;연관희
    • 한국지진공학회:학술대회논문집
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    • 한국지진공학회 2002년도 춘계 학술발표회 논문집
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    • pp.36-41
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    • 2002
  • In this study we produced 1-dimensional p wave velocity structure of the crust using 449 P arrivals of 35 stations and we analysed hypocenters of the southeastern Korean peninsula area. A initial velocity model was selected from the priori studies and 30 different initial models were generated using random number generation from it. Using the veriest program 30 different velocity structures were calculated and the result show that velocities are 5.8 - 6.4 km/sec within 6 - 16 km depth and 7 $\pm$ 0.2 km/sec within 20 - 30 km with resonable resolution. Hypocenters were relocated by using resulted 1-dimensional velocity model as a initial model. Recalculated hypocenters'depth are shallower than initial data and epicenters show a little better lineality around study area but more much earthquake information are needed fur the determination of relation between epicenter distribution and geological tectonic structures.

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남해 EEZ 바다골재 채취에 대한 사회적 합의방안 (Social Consensus on the Marine Sand Mining of the Southeastern EEZ Region)

  • 박선규
    • 한국건축시공학회:학술대회논문집
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    • 한국건축시공학회 2018년도 춘계 학술논문 발표대회
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    • pp.330-331
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    • 2018
  • It's prohibited to take sand from southeastern EEZ(Exclusive Economic Zone) from January 2017 in korea. So, the supply of sea sand has been decreased and costs of sea sand are rising as a result in the southeast region. This paper deal with appropriateness of the taking sea sand, circumstance and fisheries damages by extraction of EEZ sand and proposed control measures for ensuring quality of sea sand and consider fishermen support plan for ensuring a stable supply of sand in southeast region of korea.

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A new record of Caprella aino (Crustacea: Amphipoda: Caprellidae) from the southeastern waters of Korea, with comparison to Caprella mutica

  • Gi Beom Ryu;Won Gyu Park
    • Fisheries and Aquatic Sciences
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    • 제26권7호
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    • pp.455-459
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    • 2023
  • 40 species of the family Caprellidae Leach, 1814 are recorded in Korean waters. Caprella aino Utinomi, 1943 was newly collected from seaweed farms from the southeastern waters of Korea. C. aino was firstly reported in Japanese waters in 1943. Adults of C. aino and Caprella mutica Schurin, 1935 are easily distinguished in that C. aino have pereonite II and gnathopod II without setae and two small tubercles of articulation of gills in pereonite III-IV, while C. mutica do pereonite II and gnathopod II covered with setae and those of pereonites III-VII with many tubercles. However, subadult C. mutica is hardly distinguishable from C. aino in that tubercles of pereonite III are less developed and they have inconspicuous setae of pereonite II and gnathopod II. Nevertheless, C. aino is distinguished from subadult C. mutica because adult C. aino have dorsal tubercles on pereonite IV, V, VI, VII unlike that of C. mutica. We report C. aino as a new record in Korean water with comparison of C. mutica.

한국 동해 남부해역에 출현하는 요각류 Euchaeta plana와 Paraeuchaeta russelli의 생산력 (Production of the Copepods Euchaeta plana and Paraeuchaeta russelli in the Southeastern Sea of Korea)

  • 김가람;박원규;강형구
    • Ocean and Polar Research
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    • 제40권3호
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    • pp.115-125
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    • 2018
  • Production from copepodite IV to adult of two euchaetid species Euchaeta plana and Paraeuchaeta russelli was measured at the southeastern sea of Korea from April to November, 2014. The mean density was $2.0ind\;m^{-3}$ for E. plana and $4.1ind\;m^{-3}$ for P. russelli, with the high contribution of copepodite V to total density. The densities of total individuals, adult females and eggs were highest in November for both species. The mean egg production rate (EPR) was $1.7eggs\;female^{-1}\;d^{-1}$ for E. plana and $3.1eggs\;female^{-1}\;d^{-1}$ for P. russelli. Both of them showed the highest EPR in September but zero EPR in summer. The mean weight-specific EPR was $0.038d^{-1}$ for E. plana and $0.079d^{-1}$ for P. russelli. The mean total production rates of E. plana and P. russelli were $5.3{\mu}g\;C\;m^{-3}\;d^{-1}$ and $17.8{\mu}g\;C\;m^{-3}\;d^{-1}$, respectively, with the largest production in November. The mean Production/Biomass ratio was $0.06d^{-1}$ for E. plana and $0.07d^{-1}$ for P. russelli, with its peak in September for both. The total production of E. plana and P. russelli was positively correlated with the density of a copepod Oncaea venusta, rather than chl-a concentration, indicating that the two copepods might be carnivores. This study evaluates the contribution of euchaetids to the copepod community in the southeastern sea of Korea.

한국(韓國) 남동해안(南東海岸)부근의 해표면(海表面) 냉수(冷水) : 바람의 영향(影響) (Sea Surface Cold Water near the Southeastern Coast of Korea: Wind Effect)

  • 변상경
    • 한국해양학회지
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    • 제24권3호
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    • pp.121-131
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    • 1989
  • 1982년과 1983년 여름 한국 남동 해안부근에서 관측된 냉수를 수온, 염분, 해면, 바람 및 인공위성 영상의 자료를 이용하여 연구하였다. 3층구조의 해양을 보이는 여름철에 수일 동안 지속되는 단속적인 남서풍에 의해 완벽한(full) 용승현상이 나타난다. 용승기간 동안에 고온의 표층수는 외해로 이동하였고, 저온의 중층수가 해표면으로 노출하였으며, 해면은 하강되었으나 표층의 균형(equilibrium) 깊이는 변화되지 않았었다. 관측결과는 해표면의 냉수가 중층으로부터 기원되고 강한 전선은 계절 수온약층이 해표면에 상승된 결과임을 보인다. 해표면 전선위치와 바람입력사이의 상관관계 파악을 위해 Csanady(1982)의 모델을 rigid lid 근사조건에서 해를 구하였다. 그 결과는 전선의 위치가 바람입력 및 한국 남동 해안부근의 해양구조에 의해 결정될 수 있음을 보이고 있다. 여름철 냉수는 $10m^2/sec$ 크기 정도인 최소 바람역적보다 큰 바람이 작용될 경우에만 해표면에 나타날 수 있다.

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