• 대기
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• 제29권1호
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• pp.41-51
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• 2019

The characteristics of the sea breeze were investigated using the wind and temperature data collected from 300-m tower at Boseong from May 2014 to April 2018. Sea breeze day was detected using following criteria: 1) the presence of a clear change in wind direction near sunrise (between 1 hour after sunrise and 5 hours before sunset) and sunset (from 1500 LST to midnight), 2) presence of thermal forcing of sea breeze and 3) no heavy precipitation (rain < $10mm\;d^{-1}$). Sea breeze days occurred on 569 days for 4 years. The monthly distribution of sea breeze day occurrence shows maxima in May and September and minimum in December. The average onset and cessation times of the sea breeze are 0942 LST and 1802 LST, respectively. Although the 10-m wind shows clockwise rotation with time in the afternoon, the observed hodograph does not show an ideal elliptical shape and has different characteristics depending on the upper synoptic wind direction. Vertical structure of sea breeze shows local maximum of wind speed and local minimum of virtual potential temperature at 40 m in the afternoon for most synoptic conditions except for southeasterly synoptic wind ($60^{\circ}{\sim}150^{\circ}$) which is in the same direction as onshore flow. The local minimum of temperature is due to cold advection by sea breeze. During daytime, the intensity of inversion layer above 40 m is strongest in westerly synoptic wind ($240^{\circ}{\sim}330^{\circ}$) which is in the opposite direction to onshore flow.

• 대한토목학회논문집
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• 제29권3A호
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• pp.209-216
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• 2009

풍하중이 지배적인 구조물의 경우에 정확한 설계풍속의 산정은 구조적 안정성뿐만 아니라 경제성까지도 좌우하게 된다. 본 연구에서는 광양대교 현장에 설치된 관측탑에서 약 1년간 측정한 풍속을 사용하여 풍환경을 분석하였고, MCP(Measure-Correlate-Predict) 방법을 적용하여 관측치로부터 장기 풍속을 추정하였다. 그 결과를 보면, 광양만은 바다이지만 개활지에 가까운 풍속 특성을 나타내고 있으며, 조도지수는 고도에 따라 달라지는 것으로 나타났다. 아울러 풍향에 따라 난류강도와 조도지수가 상당히 차이나는 것으로 나타났다. MCP 방법으로 추정한 200년빈도 설계풍속은 초기설계치보다 20 m/s이상 낮았으며, 실측된 풍속과 거스트계수를 고려한 설계풍하중은 초기설계치의 36%밖에 안되는 것으로 나타났다. 이를 볼 때 국부적인 지형의 영향으로 추정한 교량 현장의 풍환경과 직접 측정한 풍환경은 차이가 나므로, 경제적이고 안전한 설계를 위해서는 단기간이라도 현장 풍환경 관측이 필요하다고 판단된다.

• Journal of Astronomy and Space Sciences
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• 제28권1호
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• pp.27-36
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• 2011

The present study examines the morning-afternoon asymmetry of the geosynchronous magnetic field strength on the dayside (magnetic local time [MLT] = 06:00~18:00) using observations by the Geostationary Operational Environmental Satellites (GOES) over a period of 9 years from February 1998 to January 2007. During geomagnetically quiet time (Kp < 3), we observed that a peak of the magnetic field strength is skewed toward the earlier local times (11:07~11:37 MLT) with respect to local noon and that the geosynchronous field strength is larger in the morning sector than in the afternoon sector. That is, there is the morning-afternoon asymmetry of the geosynchronous magnetic field strength. Using solar wind data, it is confirmed that the morning-afternoon asymmetry is not associated with the aberration effect due to the orbital motion of the Earth about the Sun. We found that the peak location of the magnetic field strength is shifted toward the earlier local times as the ratio of the magnetic field strength at MLT = 18 (B-dusk) to the magnetic field strength at MLT = 06 (B-dawn) is decreasing. It is also found that the dawn-dusk magnetic field median ratio, B-dusk/B-dawn, is decreasing as the solar wind dynamic pressure is increasing. The morning-afternoon asymmetry of the magnetic field strength appears in Tsyganenko geomagnetic field model (TS-04 model) when the partial ring current is included in TS-04 model. Unlike our observations, however, TS-04 model shows that the peak location of the magnetic field strength is shifted toward local noon as the solar wind dynamic pressure grows in magnitude. This may be due to that the symmetric magnetic field associated with the magnetopause current, strongly affected by the solar wind dynamic pressure, increases. However, the partial ring current is not affected as much as the magnetopause current by the solar wind dynamic pressure in TS-04 model. Thus, our observations suggest that the contribution of the partial ring current at geosynchronous orbit is much larger than that expected from TS-04 model as the solar wind dynamic pressure increases.

• 한국농림기상학회지
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• 제16권3호
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• pp.246-260
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• 2014

90m 고해상도 SRTM 지형자료를 장착한 WRF 수치모형을 이용하여 광릉 활엽수림 KoFlux 타워(GDK)와 침엽수림 KoFlux 타워(GCK)가 위치한 계곡 및 주변에서의 국지 대기순환을 식생-대기 이산화탄소 순환 및 미기상학적 관점에서 연구하였다. 지표 부근 온도와 바람에 대하여 모형과 관측 결과를 비교함으로써 모형의 전반적인 성능을 평가하였고, 연구 지역에 국지순환이 발생한 맑은 날(Case I)과 흐린 날(Case II) 사례를 선정하여 수치모의를 수행하고 그 결과를 정성적으로 분석하였다. 관측된 바람장은 GDK와 GCK 간에, 또 Case I과 Case II 간에 주간 및 야간 국지풍의 시작, 종료, 지속시간, 강도 등에 차이를 보였다. 모형의 수치모의 결과들은 광릉 KoFlux 타워 관측으로부터 그 가능성이 제기된 관측지 계곡의 배수류가 실제로 존재함을 증거하였다. 전반적으로 모형이 모의한 바람장은 아침의 배수류-사면활승풍 전이와 저녁의 사면활승풍 역전 등을 포함하여 계곡 및 주변에서 관측된 국지풍의 일변화를 현실적으로 모사하였다. 또한 국지풍 간 상호작용의 복잡성도 지시하였는데, 가령 주간에 광릉 관측지 계곡 내부의 서풍은 반드시 산풍인 것은 아니었으며, 종종 약한 종관규모 바람 또는 서쪽에서 불어온 해풍과 같은 보다 큰 규모의 중규모 바람 등 다른 풍계와 결합이 되어 있었다. 광릉 생태계의 에너지, 물질, 정보 흐름의 시공간적 변동을 입체적으로 이해하는데 있어서 이러한 고해상도 국지순환 수치모의 결과는 상당히 유용한 것으로 판단되며, 구축된 국지모의 시스템을 지속적으로 개선하는 노력이 향후 뒤따라야 할 것이다. 아울러, 다른 농림생태계 관측지도 모의 영역에 포함시켜 모형 결과의 활용도를 넓힐 필요가 있다.

• 한국해양공학회지
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• 제21권1호
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• pp.1-6
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• 2007

While a typhoon is traveling, characteristics of its wind fields are continuously changing, producing severe changes in local water level and wave conditions, especially, when a typhoon comes into shallow water. However, there have not been many studies related to local typhoon effects, especially, considering real time changes of wind direction related to the coastal topography. In the study, the characteristics of the wind field by typhoon and topographical characteristics in shallow water are considered, as well as conditions of wave climate estimation. These are performed by the SWAN (Simulating waves nearshore) model, in order to estimate the growth of wave energy due to the wind field. It can be strongly suggested that the wave energy of theof an inner bay should be estimated when the direction of the bay entrance and the wind direction of the typhoon are identical. The result of the numerical calculations is in better agreement with the observed data than the result of the conventional estimation techniques.

• 환경영향평가
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• 제20권4호
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• pp.539-555
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• 2011

Newly constructed, high-rise dense building areas by urban development can cause changes in local wind fields. Wind fields were analyzed to assess the impact on the local meteorology due to the land use changes during the urban redevelopment called "Eunpyeong new town" in north-western Seoul using CFD_NIMR_SNU (Computational Fluid Dynamics, National Institute of Meteorological Research, Seoul National University) model. Initial value of wind speed and direction use analysis value of AWS (Automatic Weather Station) data during 5 years. In the case of the pre-construction with low rise built-up area, it was simulated that the spatial distribution of horizontal wind fields depends on the topography and wind direction of initial inflow. But, in the case of the post-construction with high rise built-up area, it was analyzed that the wind field was affected by high rise buildings as well as terrain. High-rise buildings can generate new circulations among buildings. In addition, small size vortexes were newly generated by terrain and high rise buildings after the construction. As high-rise buildings act as a barrier, we found that the horizontal wind flow was separated and wind speed was reduced behind the buildings. CFD_NIMR_SNU was able to analyze the impact of high-rise buildings during the urban development. With the support of high power computing, it will be more common to utilize sophisticated numerical analysis models such as CFD_NIMR_SNU in evaluating the impact of urban development on wind flow or channel.

• 전력전자학회:학술대회논문집
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• 전력전자학회 2010년도 하계학술대회 논문집
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• pp.178-179
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• 2010

This paper presents a simulation model and analysis of grid-tied wind turbine generator with batteries using the PSCAD/EMTDC software. The modeled system is consist of two inverters and one bidirectional DC/DC converter. These inverter are to capture the maximum active power under varying wind conditions and to keep the DC-Link voltage magnitude at a specific level. And the bidirectional DC/DC converter makes battery charging or discharging depend on power gap between wind turbine output and local load. Aerodynamic models are applied for a wind turbine blade simulator.

• 한국태양에너지학회 논문집
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• 제27권3호
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• pp.29-35
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• 2007

In accordance with Madrid and Kyoto Protocols, a 10kw wind turbine installed about 625m away from the King Sejong Station in the Antarctica has been in operation successfully. The current location of the wind turbine has different geographic surroundings from the previous candidate site considered in 2005 and that makes re-evaluation of wind resource at the current site including geographic effects necessary. Especially, strong wind flow derived by steep and complex terrain is dominant in the Antarctica so that computational flow analysis is required. The wind rose measured at the previous and current installation location are identical with strong meteorological correlation but prevailing directions of wind power density are different because of local wind acceleration due to complex terrain. Numerical analysis explains which effects brings this discordance between the two sites, and a design guideline required for additional wind turbine installation has been secured.

• Wind and Structures
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• 제20권4호
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• pp.565-578
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• 2015

A wind energy assessment is an integrated analysis of the potential of wind energy resources of a particular area. In this work, the wind energy potentials for Mauritius have been assessed using a Computational Fluid Dynamics (CFD) model. The approach employed in this work aims to enhance the assessment of wind energy potentials for the siting of large-scale wind farms in the island. Validation of the model is done by comparing simulated wind speed data to experimental ones measured at specific locations over the island. The local wind velocity resulting from the CFD simulations are used to compute the weighted-sum power density including annual directional inflow variations determined by wind roses. The model is used to generate contour maps of velocity and power, for Mauritius at a resolution of 500 m.

• 한국항해항만학회지
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• 제43권3호
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• pp.209-218
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• 2019

연안도시는 내륙도시보다 태풍이나 해일 등에 의한 풍수해가 크며 도시마다 풍수해 특성이 서로 다르다. 그래서 연안도시는 풍수해 특성을 고려하여 풍수해 유형별 그리고 지역별 특성에 적합한 풍수해 관리체계가 필요하다. 따라서 본 연구에서는 도시관리, 연안관리, 재해관리 측면에서 우리나라 풍수해 관리체계 현황을 분석하여 문제점을 도출하고 미국과 일본 풍수해 관리체계를 검토한 후 연안도시 특성에 적합한 풍수해 관리체계 개선방안을 제안한다. 연구결과로서 도시관리 측면에서 방재지구 대상지 선정 의무화, 연안도시통합관리계획 수립, 자연재해위험개선지구를 방재지구로 지정, 방재지구를 풍해방재지구 수해방재지구 침식방재지구로 세분화, 방재지구 내 건축제한을 조례로 지정 등을 제안한다. 연안관리 측면에서 연안침식관리구역 지정권을 지자체장에게 위임, 연안침식관리구역은 연안침식심각구역 연안침식진행구역 연안침식발생우려지역으로 세분화, 연안침식관리구역의 건축제한을 조례로 결정, 연안도시 침식예상도 작성 등을 제안한다. 재해관리 측면에서 "자연재해대책법"과 "재난및안전관리기본법"의 통합, 지자체 주도 방재체계로 전환, 지역단위 재해관리네트워크 구축, 맞춤형 지역방재계획 수립 등을 제안한다.