• 대기
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• 제26권2호
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• pp.277-288
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• 2016

Polar lows are intense mesoscale cyclones that mainly occur over the sea in polar regions. Owing to their small spatial scale of a diameter less than 1000 km, simulating polar lows is a challenging task. At King Sejong station in West Antartica, polar lows are often observed. Despite the recent significant climatic changes observed over West Antarctica, adequate validation of regional simulations of extreme weather events such as polar lows are rare for this region. To address this gap, simulation results from a recent version of the Polar Weather Research and Forecasting model (Polar WRF) covering Antartic Peninsula at a high horizontal resolution of 3 km are validated against near-surface meteorological observations. We selected a case of high wind speed event on 7 January 2013 recorded at Automatic Meteorological Observation Station (AMOS) in King Sejong station, Antarctica. It is revealed by in situ observations, numerical weather prediction, and reanalysis fields that the synoptic and mesoscale environment of the strong wind event was due to the passage of a strong mesoscale polar low of center pressure 950 hPa. Verifying model results from 3 km grid resolution simulation against AMOS observation showed that high skill in simulating wind speed and surface pressure with a bias of $-1.1m\;s^{-1}$ and -1.2 hPa, respectively. Our evaluation suggests that the Polar WRF can be used as a useful dynamic downscaling tool for the simulation of Antartic weather systems and the near-surface meteorological instruments installed in King Sejong station can provide invaluable data for polar low studies over West Antartica.

• 한국지구과학회지
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• 제43권3호
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• pp.446-463
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• 2022

이 연구는 전 지구적 환경 변화에 대응하려는 인류 공동의 노력에 발맞추어 과학교육 측면에서 기후 변화를 설명하는 효과적 개념 체계로서 극지 소양 교육의 필요성을 제안한다. 이를 위해 현재 고등학생들의 극지 소양 현황을 양적 검사와 질적 면담을 통해 조사하고 시사점을 논의했다. 연구에 참여한 대상은 2개 고등학교 2학년 학생 329명으로 극지 소양 원리를 참조해 개발한 진위형 25문항으로 이루어진 검사에 참여했고, 이들 중 13명이 면담에 참여했다. 연구 결과, 극지 소양 원리의 일부 영역에서 다소 미흡한 이해와 함께 개념적 공백이 나타났다. 극지의 지리적 특징에 대한 지식이 견고하지 못하고, 빙권의 구성 요소와 주요 특성을 거의 알지 못했다. 이러한 개념의 결손으로 극지 변화와 전 지구적 기후 변화의 작동 기작을 잘 연결하지 못했다. 학교 교육과정에서 충족되지 못한 개념을 학교 밖 매체로 부터 비판 없이 수용하면서 기후 변화의 기작을 다소 단조롭거나 왜곡되게 인식했다. 한편, 극지와 기후 변화에 대한 모호한 이해와 함께 이를 보완하기 위한 인지 전략으로 언어 정보, 비유, 시각적 관찰 등을 활용했다. 이상의 연구 결과를 바탕으로 학교 과학 교육과정에 기후 변화를 체계적, 종합적으로 이해할 수 있는 새로운 지식 체계로서 극지 소양 교육을 도입할 것을 주장했다. 이밖에도 타교과의 극지 소양 관련 지식의 일관성 검토, 기후 변화를 다루는 학교 밖 매체 정보에 대한 비판적 기준 제공, 학생들의 오개념 점검 및 사고 전략 파악 등을 시사점으로 제시했다.

• Ocean and Polar Research
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• 제33권3호
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• pp.281-290
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• 2011

This study examined the change in sea surface temperature (SST) around the Korean peninsula since industrialization at year 1880, and its possible causes using observation based data from the Hadley Center, the Goddard Institute of Space Studies, and National Climate Data Center. Since year 1880, There have been multi-decadal fluctuations with a gradual reduction from 1880 to around 1940, and from 1950-1980. There has then been a marked increase from 1940-1950, and from 1980 to the present. The ocean surface warming is larger during the boreal winter than summer, and greater in the south. The multi-decadal SST fluctuations around the Korean Peninsula are largely consistent with the negative phase of the Pacific Decadal Oscillation (PDO), which fluctuates with periods of about 20-50 years. Secondly, the El Ni$\tilde{n}$o-Southern Oscillation (ENSO), whose long period component moves along with the PDO, appears to influence the SST near the Korean Peninsula, especially in recent decades. Overall, the SST around the Korean Peninsula has warmed since year 1880 by about $1^{\circ}C$, which is about twice the global-mean ocean surface warming. This long-term warming is aligned with an increase in greenhouse gas concentration, as well as local factors such as the PDO.

• 한국지구과학회지
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• 제42권6호
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• pp.734-751
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• 2021

이 연구는 극지 소양 교육을 학교 교육과정에 반영하기 위한 기초 자료를 마련하고자 수행되었다. 교육과정을 현장에서 구현하는 교사들이 지닌 극지 인식과 교수 경험, 극지 관련 인지적·정의적 특성을 조사했다. 대도시 및 중소도시 10개교의 초·중·고등학교 교사 56명을 대상으로 극지 관련 인식, 교수 현황, 극지 지식, 극지와 기후 변화에 대한 신념 및 태도를 포함한 설문을 실시했다. 그 결과, 교사들은 극지 정보에 대한 효능감은 낮은 편이나, 극지와 기후 변화 문제 해결에 있어 교육자의 위상을 긍정적으로 평가하고 있으며 세계 시민적 가치를 실용적 목적보다 우선했다. 학교에서 극지와 기후 변화 문제를 교수한 경험은 교과와 비교과에 걸쳐 다양했지만, 완성된 형태의 교수-학습 자료를 제공받기 원하는 등 교수 개발에 있어 수동적인 면모를 보였다. 인지적 측면에서 교사들은 극지 변화와 기후가 영향을 주고받는 작동 원리와 과정에 대해 다소 모호한 이해를 드러냈다. 정의적 측면에서 대부분 교사들은 학교급을 초월해서 극지 관련 문제에 대한 신념과 태도에서 높은 경향이 나타났지만, 행동 선택은 근소하게 낮았다. 이상의 결과를 바탕으로 극지 소양을 증진시키기 위한 기회 및 자료 제공, 가치 및 태도 형성을 위한 다양한 맥락의 교육 소재 발굴, 극지 연구 자료를 활용한 교육 자료 개발, 학생과 교사를 포함한 극지 지식에 대한 오개념 파악, 초등 교사의 극지 소양 강화, 정의적 태도와 가치관 함양 등의 시사점을 제안했다.

• 한국제4기학회지
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• 제21권2호
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• pp.64-67
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• 2007

• Ocean and Polar Research
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• 제44권1호
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• pp.83-97
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• 2022

The Amundsen Sea in West Antarctica is one of the most affected regions by climate change, but it is one of the least studied realms due to difficulties in access. Korea Polar Research Institute (KOPRI) launched a research project in the Amundsen Sea in 2010 using the icebreaker research vessel (IBRV) Araon and has been conducting various research initiatives. In this paper, previous researches derived from the Amundsen Sea Embayment by Korean researchers are introduced. Through previous studies, researchers have been able to interpret the environmental and biogeochemical changes according to the inflow Circumpolar Deep Water (CDW) and provide information for climate models. In particular, researches using radiocarbon isotopes (¹⁴C) were introduced to understand the physical and biogeochemical mechanisms of the carbon cycle in the Amundsen Sea. Opportunely, with the construction of a second icebreaker research vessel, the direction for systematic and long-term polar data acquisition can be presented.

• 한국측량학회:학술대회논문집
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• 한국측량학회 2009년도 춘계학술발표회 논문집
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• pp.95-100
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• 2009

Global warming melts polar ice, changes ocean currents, creates variation of local climate, and inundates low-altitude regions resulting in disasters to mankind. Accordingly, developed countries including U.S.A. and U.K. spend great amounts of efforts and money to plan and manage research activities on polar ice which is regarded as a key indicator of climate change. The proposed research aims to provide basic information for chasing and monitoring the melting phenomena of polar ice through multiple GPS to enhance the GPS quality.

• Ocean and Polar Research
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• 제34권1호
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• pp.29-35
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• 2012

We investigated the interannual relationship between chlorophyll concentrations in the western North Pacific and tropical cyclones (TCs) in the western North Pacific by analyzing data collected for >12 years. Despite the short-term scale (2~3 weeks) in the contribution of tropical cyclones to phytoplankton, the current study revealed that the long-term chlorophyll variability in the western North Pacific is profoundly related to long-term variability in the frequency of TCs. It was also found that the Pacific decadal oscillation (PDO) tends to control such relationships between the 2 bio-physical systems. This result suggests a significant climatic relationship between TC activity and marine phytoplankton, and also suggests the possibility of more accurate estimations of primary production in the western North Pacific.

• Ocean and Polar Research
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• 제34권1호
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• pp.73-83
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• 2012

Antarctica is very sensitive to climate change but the number of stations is not sufficient to accurately analyze climate change in this regoin. Model reanalysis data supplements the lack of observation and can be used as long term data to verify climate change. In this study, the 20CR (Twentieth Century Reanalysis) Project data from NCEP/NCAR and monthly mean data (temperature, solar radiation and longwave radiation) from 1871 to 2008, was used to analyze the temperature trend and change in radiation. The 20CR data was used to validate the observation data from Antarctica since 1950 and the correlation coefficients between these data were determined to be over 0.95 at all stations. The temperature increased by approximately $0.23^{\circ}C$/decade during the study period and over $0.20^{\circ}C$/decade over all of the months. This increasing trend was observed throughout the Antarctica and a slight increase was observed in the Antarctic Peninsula. In addition, solar radiation (surface) and longwave radiation (surface and top of atmosphere) trends correlated with the increase in temperature. As a result, outgoing longwave radiation at the surface is attenuated by atmospheric water vapor or clouds and radiation at the top of the atmosphere was reduced. In addition, the absorbed energy in the atmosphere increases the temperature of the atmosphere and surface, and then the heated surface emits more longwave radiation. Eventually these processes are repeated in a positive feedback loop, which results in a continuous rise in temperature.

• Ocean and Polar Research
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• 제34권3호
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• pp.275-286
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• 2012

Over the last 20 years there have been more than 3000 peer-reviewed papers relating to climate change and biodiversity published, and still the numbers are increasing. However, most studies focused on the impacts of climate change at population or community levels, and the results invariably reveal that there has been, or will be, a negative effect on the structure and pattern of biodiversity. Moreover, the climate change models and statistical analyses used to test the impacts are only newly developed, and the analyses or predictions can often be misled. In this review, I ask why an individual's life history is considered in the study how climate change affects biodiversity, and what ecological factors are impacted by climate change. Using evidence from a range of species, I demonstrate that diverse life history traits, such as early growth rate, migration/foraging behaviour and lifespan, can be shifted by climate change at individual level. Particularly I discuss that the optimal decision under unknown circumstance (climate change) would be the reduction of the ecological fitness at individual level, and hence, a shift in the balance of the ecosystem could be affected without having a critical impact on any one species. To conclude, I summarize the links between climate changes, ecological decision in life history, the revised consequence at individual level, and discuss how the finely-balanced relationship affects biodiversity and population structure.