• 제목/요약/키워드: oceanic model

검색결과 167건 처리시간 0.028초

중등학교 지구과학 수업에서 과학적 모델의 활용 양상 분석: 대기 및 해양 지구과학 관련 수업을 중심으로 (Analysis of the Manners of Using Scientific Models in Secondary Earth Science Classrooms: With a Focus on Lessons in the Domains of Atmospheric and Oceanic Earth Sciences)

  • 오필석
    • 한국과학교육학회지
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    • 제27권7호
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    • pp.645-662
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    • 2007
  • 본 연구의 목적은 우리나라 중등학교 과학 수업에서 모델이 활용되는 양상을 탐색하는 것이었다. 대기 및 해양 지구과학에 관련된 총 13개의 비디오 녹화 자료와 그것들의 전사본을 계량적인 방법과 질적인 방법으로 분석하고, 3명의 현장 교사들과 면담을 수행하였다. 연구의 결과는 서로 연관된 여섯 가지 주장들로 요약되었다. 즉, 1) 우리나라 중등학교의 대기 및 해양 지구과학 관련 수업에서는 평면적 그림 모델과 기호 모델, 모상 모델과 도해적 모델이 주로 활용된다. 2) 지구과학 수업에서 교사들은 모델을 교과 내용을 전달하기 위한 하나의 표상 형식으로서 활용한다. 3) 우리나라 중등학교 지구과학 수업에서 교사들은 이미 그 구조가 결정된 전형적인 모델을 집중적으로 활용한다. 4) 지구과학 수업에서 종종 학생들이 직접 모델을 다룰 때에는 모든 학생들이 동일한 모델을 가지고 유사한 절차에 따라 활동에 참여한다. 5) 지구과학 수업에서 교사가 과학적 모델의 본성에 대해 설명하는 경우는 거의 없으며, 학생들이 과학적 모델의 본성에 대해 생각해 볼 수 있는 기회 또한 거의 제공하지 않는다. 6) 교사들은 지구과학 수업에서 과학적 모델을 활용하는 일의 가치가 교사의 교수법적인 의도에 비추어 판단되어야 한다고 생각한다. 이러한 연구 결과를 바탕으로 모델을 활용한 과학 수업과 과학 교육 연구에서 고려해야 할 점들을 논의하였다.

Secondary human impacts on the forest understory of Ulleung Island, South Korea, a temperate island

  • Andersen, Desiree
    • Journal of Ecology and Environment
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    • 제43권2호
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    • pp.202-211
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    • 2019
  • Oceanic islands are biologically important for their unique assemblages of species and high levels of endemism and are sensitive to environmental change because of their isolation and small species source pools. Habitat destruction caused by human landscape development is generally accepted as the main cause of extinction on islands, with exotic species invasion a secondary cause of extinction, especially on tropical islands. However, secondary impacts of human development (e.g., general degradation through resource use and exotic species introduction) are understudied on temperate islands. To determine secondary impacts of human development on the understory vegetation community, 90 field sites on Ulleung Island, South Korea, were sampled during the summer of 2016. Understory vegetation was chosen as it is a proxy for ecosystem health. Diversity and percent cover of introduced, native, and endemic species were tested against proximity to developed areas and trail usage using a model selection approach. Diversity was also tested against percent cover of three naturalized species commonly found in survey plots. The main finding was that distance to development, distance to town, and trail usage have limited negative impacts on the understory vegetation community within best-supported models predicting native and introduced cover and diversity. However, endemic species cover was significantly lower on high usage trails. While there are no apparent locally invasive plant species on the island at the time of this study, percent cover of Robinia pseudoacacia, a naturalized tree species, negatively correlated with plot diversity. These findings indicate that forests on Ulleung Island are not experiencing a noticeable invasion of understory vegetation, and conservation efforts can be best spent preventing future invasions.

규칙파와 수평판의 비선형 상호작용에 의한 고차 조화항 발생 (Higher Harmonic Generation by Nonlinear Interaction between Monochromatic Waves and a Horizontal Plate)

  • 고혁준;조일형
    • 한국해안해양공학회지
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    • 제19권5호
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    • pp.484-491
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    • 2007
  • 규칙파와 수면아래 잠긴 수평판 사이의 비선형 상호작용을 규명하기 위하여 수치파동수조를 이용하여 수치 실험을 수행하였다. 수치모델로 비선형 포텐셜 이론을 근거로 한 고차 경계요소법과 Navier Stokes 방정식과 엄밀한 자유표면 경계조건식을 푸는 CADMAS-SURF을 사용하였다. 두 모델 모두 수평판 위의 천수역에서 발생하는 고차 조화항들을 예측할 수 있으며 점성효과를 포함하는 CADMAS-SURF는 수평판 양단에서 발생하는 와류와 박리에 의한 고차 조화항의 발생을 재현할 수 있다. 수평판의 잠긴 깊이와 길이 변화에 따른 반사율과 투과율을 Patarapanich and Cheong(1989)의 모형실험결과와 비교하였고 서로 잘 일치함을 확인하였다. 수평판의 길이가 길어지고 잠긴 깊이가 얕아질수록 입사파의 에너지가 고차 조화항으로 더 많이 전이됨을 확인하였다.

남인도양에서의 해수면에 대한 위성자료(Topex/Poseidon 고도계)와 현장자료(Tide Gauge 해면계)간의 비교 (Comparison of Topex/Poseidon sea levels data and Tide Gause sea levels data from the South Indian Ocean)

  • 윤홍주;김상우;이문옥;박일흠
    • 한국정보통신학회:학술대회논문집
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    • 한국해양정보통신학회 2001년도 추계종합학술대회
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    • pp.281-285
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    • 2001
  • According to standard procedures as defined in the users handbook for sea level data processes, I was compared to Topex/poseidon sea level data from the first 350days of mission and Tide Gauge sea level data from the Amsterdam- Crozet- Kerguelen region in the South Indian Ocean. The comparison improves significantly when many factors for the corrections were removed, then only the aliased oceanic tidal energy is removed by oceanic tide model in this period. Making the corrections and smoothing the sea level data over 60km along-track segments and the Tide Gauge sea level data for the time series results in the digital correlation and RMS difference between the two data of c=-0.12 and rms=11.4cm, c=0.55 and rms=5.38cm, and c=0.83 and rms=2.83cm for the Amsterdam, Crozet and Kerguelen plateau, respectively. It was also found that the Kerguelen plateau has a comparisons due to propagating signals(the baroclinic Rossby wave with velocity of -3.9~-4.2cm/sec, period of 167days and amplitude of 10cm) that introduce temporal lags($\tau$=10~30days) between the altimeter and tide gauge time series. The conclusion is that on timescales longer than about 10days the RMS sea level errors are less than or of the order of several centimeters and are mainly due to the effects of currents rather than the effects of sterics(water temperature, density) and winds.

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해양 생물 펌프가 대기 중 이산화탄소에 미치는 영향 그리고 기후 변동과의 연관성 (The Impact of the Oceanic Biological Pump on Atmospheric CO2 and Its Link to Climate Change)

  • 권은영;조양기
    • 한국해양학회지:바다
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    • 제18권4호
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    • pp.266-276
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    • 2013
  • 바다-육지-대기로 이루어진 기후 시스템에서 가장 큰 탄소의 저장고는 바다이다. 바다가 대기로부터 탄소를 흡수하는 주요 수단은 생물 활동에 의한 것으로서, 광합성에 의해 유기 물질로 동화된 탄소가 해저로 침강하고 분해되는 과정에서 깊은 바다물은 탄소를 축적하게 된다. 이러한 탄소 수송 작용을 생물 펌프라 부르며, 해수면 탄소 농도를 낮춤으로써 대기 중 이산화탄소 분압을 낮은 상태로 유지해주는 중요한 기작이다. 생물 펌프에 의해 해저에 축적된 탄소는 해양 순환에 의해 해수면에 돌아오고, 해양-대기 기체 교환에 의해 대기로 배출된다. 바다가 대기와 소통하는 이산화탄소의 양은 과거 빙하기-간빙기 기후 변동과 관련하여 과거 수십만년동안 대기 중 이산화탄소 분압변화에 주도적인 역할을 하여 온 것으로 알려져 있다. 본 논문에서는 바다에서 일어나는 탄소 순환을 간단하게 소개하고, 해양 순환의 변화가 어떻게 탄소 순환을 변형시키고, 대기 중 이산화탄소에 영향을 미치는지를 기후 변동의 관점에서 살펴보고자 한다.

하구밀도류와 바람장이 영일만 해수유동에 미치는 영향 (Numerical Prediction of Tidal Current by Effects of Wind and Density Current in Estuaries of Yeong-il Bay)

  • 윤한삼;이인철;류청로
    • 한국해양공학회:학술대회논문집
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    • 한국해양공학회 2003년도 추계학술대회 논문집
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    • pp.277-283
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    • 2003
  • This paper constructed the 3D real-time numerical model for which predicts the water quality and movement characteristics of the inner bay, which consider the characteristics of the wind-driven current and density current in estuaries which generated by the river discharge from the Hyeong-san river and oceanic water of the Eastern sea. The constructed numerical model reappeared successfully the seawater circulation current of Yeong-il Bay, which used the input conditions of the real-time tidal current, river discharge and weather conditions at March of 2001 year. Also to observe the wind-driven current and density current in estuaries effected to the seawater circulation pattern of the inner bay, we investigated the analyzation for the each impact factors and the relationship with the water quality of Yeong-il bay

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PNU CGCM V1.1을 이용한 12개월 앙상블 예측 시스템의 개발 (Development of 12-month Ensemble Prediction System Using PNU CGCM V1.1)

  • 안중배;이수봉;류상범
    • 대기
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    • 제22권4호
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    • pp.455-464
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    • 2012
  • This study investigates a 12 month-lead predictability of PNU Coupled General Circulation Model (CGCM) V1.1 hindcast, for which an oceanic data assimilated initialization is used to generate ocean initial condition. The CGCM, a participant model of APEC Climate Center (APCC) long-lead multi-model ensemble system, has been initialized at each and every month and performed 12-month-lead hindcast for each month during 1980 to 2011. The 12-month-lead hindcast consisted of 2-5 ensembles and this study verified the ensemble averaged hindcast. As for the sea-surface temperature concerns, it remained high level of confidence especially over the tropical Pacific and the mid-latitude central Pacific with slight declining of temporal correlation coefficients (TCC) as lead month increased. The CGCM revealed trustworthy ENSO prediction skills in most of hindcasts, in particular. For atmospheric variables, like air temperature, precipitation, and geopotential height at 500hPa, reliable prediction results have been shown during entire lead time in most of domain, particularly over the equatorial region. Though the TCCs of hindcasted precipitation are lower than other variables, a skillful precipitation forecasts is also shown over highly variable regions such as ITCZ. This study also revealed that there are seasonal and regional dependencies on predictability for each variable and lead.

한반도 연근해를 대상으로 해양 먹이망 기반 3차원 생태모델 구축 연구 (Study on a Three-Dimensional Ecosystem Modeling Framework Based on Marine Food Web in the Korean Peninsula)

  • 조창우;송용식;김창신;윤석현
    • 한국수산과학회지
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    • 제54권2호
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    • pp.194-207
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    • 2021
  • It is necessary to assess and manage the different elements of the marine ecosystem, such as climate change, habitat, primary and secondary production, energy flow, food web, potential yield, and fishing, to maintain the health of the ecosystem as well as support sustainable development of fishery. We set up an ecosystem model around the Korean peninsula to produce scientific predictions necessary for the assessment and management of marine ecosystems and presented the usability of the model with scenario experiments. We used the Atlantis ecosystem model based on the marine food web; Atlantis is a three-dimensional end-to-end model that includes the information and processes within an entire system, from an abiotic environment to human activity. We input the ecological and biological parameters, such as growth, mortality, spawning, recruitment, and migration, to the Atlantis model via functional groups using existing research and local measurements. During the simulation period (2018-2019), we confirmed that the model reproduced the observed data reasonably and reflected the actual ecosystem characteristics appropriately. We thus identified the usability of a marine ecosystem model with experiments on different environmental change scenarios.

Optimal Power Flow of DC-Grid Based on Improved PSO Algorithm

  • Liu, Xianzheng;Wang, Xingcheng;Wen, Jialiang
    • Journal of Electrical Engineering and Technology
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    • 제12권4호
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    • pp.1586-1592
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    • 2017
  • Voltage sourced converter (VSC) based direct-current (DC) grid has the ability to control power flow flexibly and securely, thus it has become one of the most valid approaches in aspect of large-scale renewable power generation, oceanic island power supply and new urban grid construction. To solve the optimal power flow (OPF) problem in DC grid, an adaptive particle swarm optimization (PSO) algorithm based on fuzzy control theory is proposed in this paper, and the optimal operation considering both power loss and voltage quality is realized. Firstly, the fuzzy membership curve is used to transform two objectives into one, the fitness value of latest step is introduced as input of fuzzy controller to adjust the controlling parameters of PSO dynamically. The proposed strategy was applied in solving the power flow issue in six terminals DC grid model, and corresponding results are presented to verify the effectiveness and feasibility of proposed algorithm.

Global Carbon Budget and Ocean Buffering against Rising Atmospheric CO2 Concentration

  • Kwon, O-Yul
    • 한국환경과학회지
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    • 제11권8호
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    • pp.773-781
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    • 2002
  • The natural carbon cycle has been perturbed since the mid-19th century by anthropogenic CO$_2$emissions from fossil fuel combustion and deforestation due to population growth and industrialization. The current study simulated the global carbon cycle for the past 42 years using an eight-box carbon cycle model. The results showed that since the terrestrial biospheric carbon sink was roughly offset by the deforestation source, the fossil fuel emission source was partitioned between the atmospheric and oceanic sinks. However, the partitioning ratio between the atmosphere and the ocean exhibited a change, that is, the carbon accumulation rate was faster in the atmosphere than in the ocean, due to a decrease in the so-called ocean buffering capacity. It was found that the ocean buffering capacity to take up excess CO$_2$decreased by 50% in terms of the buffer factor over the past 42 years. Accordingly, these results indicate that if the current CO$_2$emission trend continues, the future rate of increase in the atmospheric CO$_2$concentration will accelerate.