• 제목/요약/키워드: meteorological tower

검색결과 74건 처리시간 0.023초

높이별 기상변화를 고려한 초고층 건축물의 외피종류별 냉난방 부하특성 분석 (Effect of the building envelope on heating and cooling load in super tall building considering the meteorological changes with height)

  • 최종규;김양수;송두삼
    • 한국태양에너지학회:학술대회논문집
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    • 한국태양에너지학회 2012년도 춘계학술발표대회 논문집
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    • pp.337-344
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    • 2012
  • Today, the number of super tall buildings are under construction or being planed in Middle East and Asian Countries. For example the burj Khalifa, the tallest building in the world, is completed in 2008 and the height of that is about 800m. Also, Lotte World Tower is under construction in Korea. External environmental conditions such as wind speed, air temperature, humidity and solar radiation around the super tall building differs according to the building height due to the vertical micro climate change. However, the meteorological information used for AC design of building is obtained typically from standard surface meterological station data(~2m above the ground). In this paper the effect of the building envelope on heating and cooling load in super tall building considering the meteorological changes with height was analyzed with simulation method. As results of this research, the guideline to select the building envelop alternatives for super tall building will be suggested in this paper.

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보성 종합기상탑 자료를 활용한 국지기상 특성 연구 (Study on the Local Weather Characteristics using Observation Data at the Boseong Tall Tower)

  • 황성은;이영태;신승숙;김기훈
    • 한국지구과학회지
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    • 제41권5호
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    • pp.459-468
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    • 2020
  • 본 연구에서는 2016-2017년 봄철(3-5월) 동안 보성 지역에서의 해풍 발생 시 연직 기상 특성을 분석하기 위해, 해풍 발생에 대한 선정 기준을 마련하였다. 이를 위해 지상에서 측정된 강수량, 운량, 풍향과 지상과 해상 기온의 차이, 1km 고도에서의 윈드프로파일러 및 수치모델 자료를 이용한 풍속 값이 사용되었다. 선정 기준에 따라 보성지역에서의 해풍일을 분류하였고, 해풍 발생 시간 및 고도와 풍속의 크기 분석을 통해 해풍의 시공간적 특성을 파악하였다. 해풍의 발생일은 총 183일 중 23일(12%)로서, 보성지역의 경우 봄철 10일 중 최소 1.2일은 해풍이 나타났다. 해풍은 1200 LST부터 1800 LST로 낮 시간에 지상에서부터 700 m 고도까지 주로 발생하였다. 또한, 최대 풍속은 평균 4.9 m s-1로 1600 LST에 40 m 고도에서 나타나, 선행연구보다 비교적 낮은 값을 보였다. 이는 해안지형이 복잡하여 지형 효과에 따른 풍속 감소로 인한 것으로 보인다.

플럭스 타워 관측 자료 및 통합수문모형을 이용한 순복사량 산정: 설마천, 청미천 유역을 대상으로 (Net Radiation Estimation Using Flux Tower Data and Integrated Hydrological Model: For the Seolmacheon and Chungmichen Watersheds)

  • 김다은;백종진;정성원;최민하
    • 한국수자원학회논문집
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    • 제46권3호
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    • pp.301-314
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    • 2013
  • 기후변화로 야기될 수 있는 태양복사에너지의 공간적인 불균형은 수자원을 포함한 전반적인 생태 시스템에서의 에너지 불균형을 초래한다. 따라서 정확한 에너지의 흐름을 이해하기 위하여 정량적인 관측을 목적으로 하는 플럭스 타워가 세계 곳곳에 설치되어 운영되고 있다. 국내의 주역에서도 플럭스 타워를 통안 관측이 실시되고 있는 데, 본 연구에서는 이 중 설마천과 청미천 유역의 플럭스 타워의 자료를 대상으로 수문기상 및 생태학적으로 중요한 역할을 하는 에너지원인 하향 단파 및 장파 복사량과 순복사량을 기존의 연구에서 제안된 물리식을 기반으로 계산하고, 산정된 순복사량과 관측 자료를 비교 검증하였다. 이를 통하여 관측이 미흡한 수문기상인자에 대해 기존의 물리적인 방법의 사용 가능성 및 관측 자료의 활용 가능성을 확인하였다.

도시의 수목이 기온의 조절에 미치는 영향 (Influences of Urban Trees on the Control of the Temperature)

  • 김수봉;김해동
    • 한국조경학회지
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    • 제30권3호
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    • pp.25-34
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    • 2002
  • The purpose of this paper is to discuss the function of microclimate amelioration of urban trees regarding the environmental benefits of street trees in summer, focusing on the heat pollution-urban heat island, tropical climate day's phenomenon and air pollution. We measured the diurnal variation of air/ground temperatures and humidity within the vegetation canopy with the meteorological tower observation system. Summertime air temperatures within the vegetation canopy layer were 1-2$^{\circ}C$ cooler than in places with no vegetation. Due to lack of evaporation, the ground surface temperatures of footpaths were, at a midafternoon maximum, 8$^{\circ}C$ hotter than those under trees. This means that heat flows from a place with no vegetation to a vegetation canopy layer during the daytime. The heat is consumed as a evaporation latent heat. These results suggest that the extension of vegetation canopy bring about a more pleasant urban climate. Diurnal variation of air/ground temperatures and humidity within the vegetation canopy were measured with the meteorological tower observation system. According to the findings, summertime air temperatures under a vegetation canopy layer were 1-2$^{\circ}C$ cooler than places with no vegetation. Due mainly to lack of evaporation the ground surface temperature of footpaths were up to 8$^{\circ}C$ hotter than under trees during mid-afternoon. This means that heat flows from a place where there is no vegetation to another place where there is a vegetation canopy layer during the daytime. Through the energy redistribution analysis, we ascertain that the major part of solar radiation reaching the vegetation cover is consumed as a evaporation latent heat. This result suggests that the expansion of vegetation cover creates a more pleasant urban climate through the cooling effect in summer. Vegetation plays an important role because of its special properties with energy balance. Depended on their evapotranspiration, vegetation cover and water surfaces diminish the peaks of temperature during the day. The skill to make the best use of the vegetation effect in urban areas is a very important planning device to optimize urban climate. Numerical simulation study to examine the vegetation effects on urban climate will be published in our next research paper.

집중관측을 통한 서해연안의 대기 수직구조 특성 (On the Characteristics of Vertical Atmospheric Structure in the Western Coastal Region through the Intensive Observation Period)

  • 문승의;노재식
    • 한국환경과학회지
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    • 제7권3호
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    • pp.335-348
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    • 1998
  • The intensive meteorological observations including pibal balloon at Ungcheon, airsonde and 10m meteorological tower observations at Gulup-Do, where are located In the western coastal region, are taken to Investigate the characteristics of the upper and lower atmospheric structure and the local circulation pattern during the period of 17 to 22 September 1996. The diurnal variations of weather elements(i.e. air temperature, humidity, pressure, and Und speeds at Gulup-Do are analyzed and discussed with those at four inland meteorological stations. The vertical profiles of wind vector, ortho- gonality(Ω), and shear obtained from the pibal obsenrations are also presented to examine the change of wand structure according to the synoptic-scale pressure system's movement. The diurnal temperature changes at Gulup-Do are more sensitive than that of Inland meteorological stations In case of the mow of southwesterlies but are not dominant due to the ocean effect under the Influence of relatively cold northerlies. A well defined mixed layer Is developed from the 500m to the maximum 1700m with a significant capping Inversion layer on the top of it. It can be found from the vertical profiles of wind vector that the wind become generally strong at the interface heights between cloud lay- ers and non-cloud layers. The maximum Und shear Is appeared at the bel각t where the varlauon of wand direction Induced by the passage of synoptic-scale pressure system Is accompanied with the In- crease of Und speed. Based on the wind orthogonality, the change of wind direction with height is more complicated In cloudy day than In clear day. In case of a fair weather, the change of wand direction is showed to be at around 2km.

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북극 다산기지에서의 플럭스 발자취 기후도와 플럭스 자료 품질 (Flux Footprint Climatology and Data Quality at Dasan Station in the Arctic)

  • 이방용;최태진;이희춘;윤영준
    • 지구물리
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    • 제8권4호
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    • pp.201-205
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    • 2005
  • Turbulent fluxes of heat, water vapor, and CO2 have been measured since August, 2003 at Dasan Station (78o 55’ N, 11o50’E) in the Arctic. These data can allow us to better understand the interactions between the Polar ecosystems and the atmosphere together with those at King Sejong Station in the Antarctic. Due to the buildings and measurement platforms around the flux tower, it is required to evaluate how they influence measured flux data. By using one-year turbulence statistics data and footprint model, flux footprint climatology was analyzed together with data availability. The upwind distance of source area ranged from 150 to 300 m, where the buildings and measurement platforms existed. However, flow distortion due to them may be not a major factor to reduce the data availability significantly. Based on, the dominant wind direction of SW and footprint climatology, the location of flux tower is considered suitable for flux measurement.

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Wind characteristics of a strong typhoon in marine surface boundary layer

  • Song, Lili;Li, Q.S.;Chen, Wenchao;Qin, Peng;Huang, Haohui;He, Y.C.
    • Wind and Structures
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    • 제15권1호
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    • pp.1-15
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    • 2012
  • High-resolution wind data were acquired from a 100-m high offshore tower during the passage of Typhoon Hagupit in September, 2008. The meteorological tower was equipped with an ultrasonic anemometer and a number of cup anemometers at heights between 10 and 100 m. Wind characteristics of the strong typhoon, such as mean wind speed and wind direction, turbulence intensity, turbulence integral length scale, gust factor and power spectra of wind velocity, vertical profiles of mean wind speed were investigated in detail based on the wind data recorded during the strong typhoon. The measured results revealed that the wind characteristics in different stages during the typhoon varied remarkably. Through comparison with non-typhoon wind measurements, the phenomena of enhanced levels of turbulence intensity, gust factors, turbulence integral length scale and spectral magnitudes in typhoon boundary layer were observed. The monitored data and analysis results are expected to be useful for the wind-resistant design of offshore structures and buildings on seashores in typhoon-prone regions.

KoFlux 타워에서 관측된 토양수분 값을 이용한 가뭄지수 활용에 관한 연구 (The study of Application of Drought Index Using Measured Soil Moisture at KoFlux Tower)

  • 김수영;조환범;이승오;최민하
    • 대한토목학회논문집
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    • 제30권6B호
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    • pp.541-549
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    • 2010
  • 현재 우리나라는 지구 온난화로 인한 이상기후 현상이 발생하여 평균 강우량은 증가하는 반면에 강우일수는 감소하는 경향을 나타내고 있다. 다시 말하면, 강우가 특정한 기간에 집중되어 내려 홍수에 의한 피해도 심각하지만 가뭄에 의한 피해 또한 심각하다는 것을 나타낸다. 기존의 연구를 살펴보면 홍수에 대한 연구는 비교적 많은 편이지만 가뭄에 대한 연구는 상대적으로 드물다. 본 연구에서는 토양수분과 강수량으로 가뭄지수를 산정하여 비교 검토하였으며 이를 바탕으로 정확한 가뭄의 경향을 파악하고자 한다. 연구지역은 전라남도 해남이며, 토양수분자료로 Soil Moisture Index(SMI)를 산정하였고, 기상 자료로 Standardized Precipitation Index(SPI)와 Palmer Drought Severity Index(PDSI)를 산정하였다. 본 연구에서는 KoFlux 타워에서 측정된 토양수분 값을 이용하여 보다 실질적인 가뭄지수를 산정할 수 있었다. 각 가뭄지수를 월 단위로 산정하였고, 비교분석 결과 세 가지 가뭄지수는 대체로 비슷한 경향을 나타내었다. 따라서 KoFlux 타워에서 측정된 토양수분 값으로 가뭄지수를 산정하는 것은 적절하다고 판단되고 토양수분 값은 모든 기상학적 요인들에 직접적으로 영향을 받기 때문이라고 판단된다.

풍력예보를 위한 단순 앙상블예측시스템 - 태풍 볼라벤 사례를 통한 평가 - (A Simple Ensemble Prediction System for Wind Power Forecasting - Evaluation by Typhoon Bolaven Case -)

  • 김진영;김현구;강용혁;윤창열;김지영;이준신
    • 한국태양에너지학회 논문집
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    • 제36권1호
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    • pp.27-37
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    • 2016
  • A simple but practical Ensemble Prediction System(EPS) for wind power forecasting was developed and evaluated using the measurement of the offshore meteorological tower, HeMOSU-1(Herald of Meteorological and Oceanographic Special Unite-1) installed at the Southwest Offshore in South Korea. The EPS developed by the Korea Institute of Energy Research is based on a simple ensemble mean of two Numerical Weather Prediction(NWP) models, WRF-NMM and WRF-ARW. In addition, the Kalman Filter is applied for real-time quality improvement of wind ensembles. All forecasts with EPS were analyzed in comparison with the HeMOSU-1 measurements at 97 m above sea level during Typhoon Bolaven episode in August 2012. The results indicate that EPS was in the best agreement with the in-situ measurement regarding (peak) wind speed and cut-out speed incidence. The RMSE of wind speed was 1.44 m/s while the incidence time lag of cut-out wind speed was 0 hour, which means that the EPS properly predicted a development and its movement. The duration of cut-out wind speed period by the EPS was also acceptable. This study is anticipated to provide a useful quantitative guide and information for a large-scale offshore wind farm operation in the decision making of wind turbine control especially during a typhoon episode.

영상 선호 처리를 이용한 풍향센서의 진북맞추기 (A Technique for Alignment to True North Using Image Processing)

  • 이정완;남윤수;유능수
    • 산업기술연구
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    • 제22권A호
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    • pp.67-72
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    • 2002
  • A technique for alignment to true north is presented, based on synchronized measurements of vision image by a camera and output voltage of wind direction sensor. The true wind direction is evaluated by means of image processing techniques with least square sense, and then evaluated true value is compared with measured output voltage of the sensor. The proposed technique is applied to real meteorological tower m Daekwanryung test site. In addition, some uncertainty analysis of this method is presented.

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