• 한국자원식물학회지
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• 제2권2호
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• pp.298-305
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• 1989

벼멸구 상습피해지역인 해남의 벼멸구 비내시기 비내시기기상 특성 및 비내 벼멸구의 생태적 특성을 조사한 결과는 다음과 같다. (1) 초비내시기는 6 월 하순 ~ 7월 하순, 집중비내시기는 7월 하순~중순경으로 전남 내륙지역보다 15~30 일 빨랐으며, 집중비내기의 기상은 온도 $20{\;}~{\;}25^{\circ}C$, 습도 86 ~ 95 %, 남서풍, 풍속 1.0~2.9 m/sec였다. (2) 비내량은 지형에 따라 차이를 해안에 인접한 산의 뒤쪽 들에서 많았고 생태형 구성비는 생태형 I은 감소하는 반면에 생태형II와 III의 비가 증가하는 경향이었다. (3) 비내 벼멸구의 란.약충 및 성충기간은 명명 9 ~ 12 일, 13 ~ 16 일, 12 ~ 36일이었고 부화율과 우화율은 80% 이상으로 발생기의 기상조건에 따라 차이가 뚜렷하였다. 성충의 수명은 ♀이 ♂보다 장혈형이 단혈형이 보다 더 길었으나 산화수는 단혈형이 더 많은 차이를 보였다. (4) 벼멸구의 수치적 활동범위는 수면상 16cm 이내이고 주간에는 위로 야간에는 수면가까이 이동하는 경시적 일주성을 나타냈으며 Hopping에 의한 이동거리는 반경 20cm 이내이었다.

• 대한원격탐사학회지
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• 제14권2호
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• pp.165-174
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• 1998

구름 속의 수액량 분포와 인공강우에 의한 잠재적 증우 가능성을 조사하기 위해 1797년 7월부터 1998년 2월가지 이중채널 마이크로웨이브 레디오메타를 사용하여 안동 지방에서 관측을 실시하였다. 안동 지방의 수액량은 대부분의 시간대에서 0.1mm 이하로 매우 작은 값을 보였다. 계절적 특성을 살펴보면 여름철에 수액량이 가장 풍부하였으며, 봄, 가을, 겨을 순이었다. 수액량의 일변화 양상은 여름철을 제외한 계절에서 12시부터 17시까지 비교적 높은 수액량을 보였으며, 강수량이 많은 여름철에는 수액량의 시간 변동이 심한 것으로 조사되었다 풍향에 따른 수액량의 분포는 소백산맥을 넘어오는 기류인 서풍과 남서풍 계열의 바람에서 수액이 풍부하게 존재하는 것으로 조사되었다. 수평 수액량 플럭스와 연직 강수량의 비인 잠재적 증우 가능량(P$_{en}$)은 대부분 0.5 이하였으며, 계절적으로는 봄철에 0.5, 여름과 가을철에 0.2, 그리고 겨울철에 0.1 이었다. 결과적으로 안동지역에서 인공강우에 의한 최대 증우 가능성은 봄철 서풍계열의 바람에서 높은 것으로 조사되었다. .

• 한국환경과학회지
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• 제23권2호
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• pp.275-289
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• 2014

Asian dust (or yellow sand) occurring mainly in spring in East Asia is affected by the distribution of weather systems. This study was performed to investigate the characteristics of suspended particulate for Asian dust at Busan, Korea in 20 March 2010, which was one of the extreme case for the last 10 years. There was used the data of weather chart, satellite, automatic weather system (AWS), $PM_{10}$, laser particle counter (LPC), and backward trajectories model. In synoptically, the high pressure was located in the northwestern part and low pressure was located in the northeastern part of Korea. The strong westerly winds from surface to upper layer makes it possible to move air masses rapidly. Air masses passing through Gobi Desert in Mongolia and Inner Mongolia plateau covered the entire Korean peninsula. As the results of aerosol analysis, $PM_{10}$ concentration at Gudeok mountain in Busan was recorded $2,344{\mu}g/m^3$ in 2300 LST 20 March 2010 and their concentration was markedly increased at coarse mode particle. In surface condition, westerly wind about 3 ~ 5 m/s was dominant and small particles of $0.3{\sim}0.5{\mu}m$ were distributed on the whole. In heavy metal components analysis, the elements from the land was predominated.

• 한국대기환경학회지
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• 제25권5호
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• pp.432-449
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• 2009

In this study, the effects of high-resolution land cover on the simulation of near-surface meteorological fields were evaluated in two different coastal regions using Weather Research and Forecasting (WRF) model. These analyses were performed using the middle classification land cover data upgraded by the Korean Ministry of Environment (KME). For the purpose of this study, two coastal areas were selected as follows: (1) the southwestern coastal (SWC) region characterized by complex shoreline and (2) the eastern coastal (EC) region described a high mountain and a simple coastline. The result showed that the application of high-resolution land cover were found to be notably distinguished between the SWC and EC regions. The land cover improvement has contributed to generate the realistic complex coastline and the distribution of small islands in the SWC region and the expansion of urban and built-up land along the sea front in the EC region, respectively. The model study indicated that the improvement of land cover caused a temperature change on wide areas of inland and nearby sea for the SWC region, and narrow areas along the coastal line for the EC region. These temperature variations in the two regions resulted in a decrease and an increase in land-breeze and sea-breeze intensity, respectively (especially the SWC region). Interestingly, the improvement of land cover can contribute large enough to change wind distributions over the sea in coastal areas.

• 한국환경과학회지
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• 제1권2호
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• pp.119-124
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• 1992

Cloud streets were successfully simulated by numerical model (RAMS) including an Isolated mountain near the coast, large sensible heat flux from the sea surface, uniform stratification and wind velocity with low Froude number (0.25) in the inflow boundary The well developed cloud streets between a pair of convective rolls are simulated at a level of 1 km over the sea. The following five results were obtained: 1) port the formation of the pair of convective rolls, both strong static instability and a topographically induced mechanical disturbance are strongly required at the same time. 2) Strong sensible heat flux from the sea surface is the main energy source of the pair of convective rolls, and the buoyancy caused by condensation in the cloud is negligibly small. 3) The pair o( convective rolls is a complex of two sub-rolls. One is the outer roll, which has a large radius, but weak circulation, and the other is the inner roll, which has a small radius, but strong circulation. The outer roll gathers a large amount of moisture by convergence in the lower marine boundary, and the inner roll transfers the convergent moisture to the upper boundary layer by strong upward motion between them. 4) The pair of inner rolls form the line-shaped cloud streets, and keep them narrow along the center-line of the domain. 5) Both by non-hydrostatic and by hydrostatic assumptions, cloud streets can be simulated. In our case, non-hydrostatic processes enhanced somewhat the formation of cloud streets. The horizontal size of the topography does not seem to be restricted to within the small scale where non-hydrostatic effects are important.

• 한국환경과학회지
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• 제15권5호
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• pp.387-396
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• 2006

The numerical modeling and comparison with observations are performed to find out the detailed structure of meteorology and the characteristic of related dispersion phenomena of the non-reactive air pollutant at Kyoungin region, South Korea, where several industrial complex including Siwha, Banwol and Namdong is located. MM5 (Fifth Generation NCAR/Penn State Mesoscale Model), 3-D Land/sea breeze model and 3-D diagnostic meteorological model have been utilized for the meteorological simulation for September, 2002 with each different spatial resolution, while 3-D Eulerian air dispersion model for the air quality study. We can see the simulated wind field shows the very local circulation quitely well compared with in-site observations in shoreline area with complex terrains, at which the circulation of Land/sea breeze has developed and merged with the mountain and valley breeze eventually. Also it is shown in the result of the dispersion model that the diurnal variation and absolute value of daily mean $SO_2$ concentrations have good agreement with observations, even though the instant concentration of $SO_2$ simulated overestimates around 1.5 times rather than that of observation due to neglecting the deposition process and roughly estimated emission rate. This results may indicate that it is important for the air quality study at shoreline region with the complex terrain to implement the high resolution meteorological model which is able to handle with the complicate local circulation.

• Environmental Sciences Bulletin of The Korean Environmental Sciences Society
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• 제1권1호
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• pp.19-33
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• 1997

The high oxidants, which occur the daily maximum concentrations in the afternoon, are transported into the other region via long range transport mechanisms or trapped within the shallow mixing boundary layer and then removed physically (deposition, transport by mountain wind, etc.) and chemically (reaction with local sources). Therefore, modeling formation of photochemical oxidants requires a complex description of both chemical and meteorological processes. In this study, as a part of air quality studies, we reviewed various aspects of photochemical modeling on the basis of currently available literature. The result of the review shows that the model is based on a set of coupled continuity equations describing advection, diffusion, transport, deposition, chemistry, emission. Also photochemical oxidant models require a large amount of input data concerned with all aspects of the ozone life cycle. First, emission inventories of hydrocarbon and nitrogen oxides, with appropriate spatial and temporal resolution. Second, chemical and photochemical data allowing the quantitative description of the formation of ozone and other photochemically-generated secondary pollutants. Third, dry deposition mechanisms particularly for ozone, PAN and hydrogen peroxide to account for their removal by absorption on the ground, crops, natural vegetation, man-made and water surfaces. Finally, meteorological data describing the transport of primary pollutants away from their sources and of secondary pollutants towards the sensitive receptors where environmental damage may occur. In order to improve our present study, shortcomings and limitation of existing models are pointed out and verification process through observation is emphasized.

• 전기학회논문지
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• 제66권12호
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• pp.1873-1878
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• 2017

Both the introduction of the Renewable Energy Portfolio Standard (RPS) system into the electric energy market in 2012 and a decrease in the cost of constructing photovoltaic (PV) power plants have been increasing the number of MW PV plants in South Korea. Jeju Island is located at the center of three nations, South Korea, China and Japan, and its provincial government declared in 2012 that the island will be a clean region where greenhouse gases are not emitted by 2030. The Jeju provincial government is now doing its best to install PV plants and wind farms to realize a carbon-free island. In this study we investigated contribution of MW PV plants to the power of the electric grid during summer peak times on Jeju Island. Mt. Halla the highest mountain in South Korea, is located at the center of Jeju Island, and we divided the island into four regions and carried out analyses of a total of 24 PV plants. The average contribution of the PV plants in the respective region to electric power of Jeju Island during summer peak times was investigated and compared with those of the other regions. The best average contribution during the 12.5% maximum load period was obtained from the PV plants in the western region, and the value was 33% during 2015 and 2016.

• 한국전통조경학회지
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• 제34권2호
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• pp.55-62
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• 2016

본 연구는 풍수이론으로 은평뉴타운을 분석하였다. 우선 주거지를 분석하기 위한 틀(천지인합일, 인지제의, 대환경상지분석, 소환경상지분석, 동선상지분석, 주거지조향분석)을 구성하였다. 그 틀로 은평뉴타운을 분석하였으며 결과를 보면 다음과 같다. 광역적으로 분석한 대환경상지분석에서 은평구는 서북향에 산세가 열려 있으므로 겨울 서북풍에 노출되어 불리한 풍수형국으로 나타났다. 소환경상지분석은 사신수형국 기준으로 1지구와 2지구를 구분하여 분석하였다. 분석한 결과 1지구는 배수임산으로 흉지(凶地), 2지구는 비보풍수인 실개천의 복원으로 배산임수의 길지(吉地)로 나타났다. 마지막으로 분석한 결과에 따라 비보풍수 방식을 적용하여 대상지를 길지로 보완하기 위한 대안을 제시하였다.

• Journal of Forest and Environmental Science
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• 제39권1호
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• pp.13-19
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• 2023

We investigated Soil respiration in Bluepine forest of western Bhutan, in relation to soil temperature, moisture content and soil pH and it was aimed at establishing variability in space and time. The Bluepine forest thrives in the typical shallow dry valleys in the inter-montane Bhutan Himalaya, which is formed by ascending wind from the valley bottom, which carries moisture from the river away to the mountain ridges. Stratified random sampling was applied and the study site was classified into top, mid, low slope and further randomized sample of n=20 from 30 m×30 m from each altitude. The overall soil respiration mean for the forest was found 2248.17 CO₂ g yr^-1 and it is ~613.58 C g yr^-1. The RS from three sites showed a marginal variation amongst sites, lower slope (2,309 m) was 4.64 μ mol m^-2 s^-1, mid slope (2,631 m) was 6.78 μ mol m^-2 s^-1 and top slope (3,027 m) was 6.33 μ mol m^-2 s^-1 and mean of 5.92 μ mol m^-2 s^-1, SE=0.25 for the forest. Temporal distribution and variations were observed more pronounced than in the space variation. Soil respiration was found highest during March and lowest in September. Soil temperature had almost inverse trend against soil respiration and dropped a low in February and peak in July. The moisture in the soil changed across months with precipitation and pH remained almost consistent across the period. The soil respiration and soil temperature had significant relationship R²=-0.61, p=0.027 and other variables were found insignificant. Similar relationship are reported for dry season in a tropical forest soil respiration. Soil temperature was found to have most pronounced effect on the soil respiration of the forest under study.