• 제목/요약/키워드: King Sejong station

검색결과 80건 처리시간 0.022초

Lichen Flora around the Korean Antarctic Scientific Station, King George Island, Antarctic

  • Kim, Ji-Hee;Ahn, In-Young;Hong, Soon-Gyu;Andreev, Mikhail;Lim, Kwang-Mi;Oh, Mi-Jin;Koh, Young-Jin;Hur, Jae-Seoun
    • Journal of Microbiology
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    • 제44권5호
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    • pp.480-491
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    • 2006
  • As part of the long-term monitoring projects on Antarctic terrestrial vegetation in relation to global climate change, a lichen floristical survey was conducted around the Korean Antarctic Station (King Sejong Station), which is located on Barton Peninsula, King George Island, in January and February of 2006. Two hundred and twenty-five lichen specimens were collected and sixty-two lichen species in 38 genera were identified by morphological characteristics, chemical constituents, TLC analysis and ITS nucleotide sequence analysis.

대기 복사 모형에 의한 남극 세종기지에서의 복사학적 특징 : 지표면에서 UV-A와 Erythemal UV-B 자외선 양 변화 (Radiative Properties at King Sejong Station in West Antarctica with the Radiative Transfer Model : A Surface UV-A and Erythemal UV-B Radiation Changes)

  • 이규태;이방용;원영인;지준범;이원학;김윤정
    • Ocean and Polar Research
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    • 제25권1호
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    • pp.9-20
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    • 2003
  • A solar radiation model was used to investigate the UV radiation at the surface offing Sejong Station in West Antarctica. The results calculated by this model were compared with the values measured by UV-Biometer and UV-A meter during 1999-2000. In this study, the parameterization of solar radiative transfer process was based on Chou and Lee(1996). The total ozone amounts measured by Breve. Ozone Spectrophotometer and the aerosol amounts by Nakajima et al.(1996) was used as the input data of the solar radiative transfer model. And the surface albedo is assumed to be 0.20 in summer and 0.85 in winter. The sensitivity test of solar radiative transfer model was done with the variation of total ozone, aerosol amount, and surface albedo. When the cosine of solar zenith angle is 0.3, Erythemal UV-B radiation decreased 73% with the 200% increase of total ozone from 100 DU to 300 DU, but the decrease of UV-A radiation is about 1%. Also, for the same solar zenith angle, UV-A radiation was decreased 31.0% with the variation of aerosol optical thickness from 0.0 to 0.3 and Erythemal UV-B radiation was decreased only 6.1%. The increase of Erythemal W-B radiation with the variation of surface albedo was twice that of UV-A increase. The surface Erythemal UV-B and UV-A radiation calculated by solar raditive transfer model were compared with the measured values fer the relatively clear day at King Sejong Station in West Antarctica. The model calculated Erythemal UV-B radiation at the surface coincide well with the measured values except for cloudy days. But the difference between the model calculated UV-A radiation and the measured value at the surface was large because of cloud scattering effect. So, the cloud property data is needed to calculate the UV radiation more exactly at King Sejong Station in West Antarctica.

마이크로 그리드에서의 풍력/디젤 복합발전 전력품질 (Power Quality of Wind/Diesel Hybrid Operation at an Micro Grid)

  • 김석우;고석환;장문석
    • 한국태양에너지학회 논문집
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    • 제29권4호
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    • pp.41-47
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    • 2009
  • Wind/diesel hybrid operation can be one of the most effective option for electrical power production at a remote area such as Antarctica. The king Sejong station at Antarctica relies its power production on diesel engines and diesel oil is supplied every other year by ships. However, the oil transportation processes are liable to potential oil spillage caused by the floating ice around the King George island. The long-term storage of the oil at the station can also contaminate the surrounding soils. A l0kW wind turbine has been installed to save oil consumption and operated in connection with the diesel generators since 2006. The diesel engine that operated poorly during the first year of installation was replaced in 2008 to enhance power production an recent measurements indicate that both diesel power quality and the wind turbine availability have been dramatically improved by the replacement. This report discusses electrical power qualities of wind/diesel hybrid system operating at an isolated micro gird located in the king Sejong station. Our experience reveals that the similar technologies can be applied to domestic islands, for example, in the south sea.

세종기지 주변에서 관찰된 빙벽 후퇴와 바다 결빙 (Ice cliff retreat and sea-ice formation observed around King Sejong Station in King George Island, West Antarctica)

  • 정호성;이방용;장순근;김지희;김예동
    • Ocean and Polar Research
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    • 제26권1호
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    • pp.1-10
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    • 2004
  • Ice cliff retreat and sea-ice formation around King Sejong Station in King George Island were analysed and compared with air temperature change. Analysis of 33-year (1969-2001) air temperature records at Bellingshausen Station has revealed regional atmospheric warming, and the increasing rate of air temperature Is equivalent to a warming of $1^{\circ}C$ for 27-year period. Here we present time-series of observations for the areal extent of the ice cliff and ice sheet, showing that they have retreated dramatically in the past 45 years (1956-2001). Retreat of 1,050 m in length of the ice clifr has changed the Marian Cove into a low rectangular form of 4 km in length and 1 to 1.3km in width. The retreat rates have since increased from 6 m/yr of the Primary investigated Period to 54 and 81m/yr in the recent years. Exceptionally, the ice cliff had been advanced of 21m in length for a year between 1987 and 1988 of cold winters. Ice sheet in King George Island also shows a similar decrease, and the decreasing extent is much larger at the southern part of the Main Cove, relatively more exposed to the sun, than at the northern part. Comparing sea-ice formation in winter with air temperature data shows a pattern starting to freeze below $-5^{\circ}C$ and to thaw over $-3^{\circ}C$. It is conclusively estimated that the patterns and magnitudes of ice cliff retreat and sea-ice formation are consistent with fluctuations of the air temperature, and that the recent rapid retreat of ice cliff and less formation of sea-ice are caused especially by the warming trends in autumn accompanied with expansion of summer thawing period.

남극 세종기지에서의 지표 플럭스 관측: I. 난류 특성과 현열 플럭스 (Surface Flux Measurements at King Sejong Station in West Antarctica: I. Turbulent Characteristics and Sensible Beat Flux)

  • 최태진;이방용;이희춘;심재설
    • Ocean and Polar Research
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    • 제26권3호
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    • pp.453-463
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    • 2004
  • The Antarctic Peninsula is important in terms of global warming research due to pronounced increase of air temperature over the last century. The first eddy covariance system was established at King Sejong Station located in the northern region of the Antarctic Peninsula in December of 2002 and has been operated over one year. Here, we analyze turbulent characteristics to determine quality control criteria for turbulent sensible heat flux data as well as to diagnose the possibility of long term eddy covariance measurement under extreme weather conditions of the Antarctic Peninsula. We also report the preliminary result on sensible heat flux. Based on the analyses on turbulent characteristics such as integral turbulence characteristics of vertical velocity (w) and heat (T), stationarity test and investigation of correlation coefficient, they fallow the Monin-Obukhov similarity and eddy covariance flux data were reliable. ${\sim}47%$ of total retrieved sensible heat flux data could be used for further analysis. Daytime averaged sensible heat flux showed a pronounced seasonal variation, with a maximum of up to $300Wm^{-2}$ in summer. In conclusion, continuous and long-term eddy covariance measurement may be possible at the study site and the land surface may influence the atmosphere significantly through heat transport in summer.

대기 복사 모형에 의한 세종기지에서의 복사학적 특징: 복사 대류 평형 모형을 이용한 기후 변화 연구 (Radiative Properties of King Sejong Station in West Antarctica with the Radiative Transfer Model: Climate Change using Radiative Convective Equilibrium Model)

  • 이규태;이방용;지준범;윤영준;이원학
    • 지구물리
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    • 제9권1호
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    • pp.27-36
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    • 2006
  • 연직 공기 기둥에 대한 복사 및 대류 과정이 포함된 일차원 복사-대류 평형 모형을 구축하였고, 이 모형을 이용하여 남극 세종기지에서 복사-대류 평형 온도를 계산 하고 분석하였다. 이 모형의 반응도에서 지표면 알베도와 태양 천정각의 코사인 및 이산화탄소 증가는 지표면에서의 복사-대류 평형 온도를 감소시켰다. 그리고 구름 광학두께가 비교적 큰 하층운은 지표면 온도를 감소시키나, 구름 광학두께가 작은 상층운은 온실효과 때문에 지표면 온도를 증가시켰다. 남극 세종기지의 44년 (1958∼2001)의 기간에 대하여 계산된 지표면에서의 복사-대류 평형 온도의 연변화는 0.012oC/년이었다. 마찬가지로 13년 동안(1989∼2001)의 자료에 대한 복사-평형 온도 변화는 0.01oC/월이었으며, 동일한 기간의 관측 자료 분석 결과로는 0.005oC/월의 변화를 나타내었다.

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