• Proceedings of the Korean Environmental Sciences Society Conference
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• 2004.05a
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• pp.230-231
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• 2004

일출 후 태양복사에 의한 혼합층 발달과 새벽녘의 안정층 형성이 잘 관측되고 있다. 풍향의 경우, 해륙풍에 의한 풍향 일변화를 보이고 있으며, 이는 해안지역의 특징을 잘 반영하는 것이다. 간척지라는 지면특성을 고려하여 지속적인 관측과 분석이 이루어진다면, 지면성질에 따른 대기경계층 특성과 혼합층 고도를 추정할 수 있을 것으로 기대된다.

• The Journal of the Korea institute of electronic communication sciences
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• v.18 no.6
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• pp.1049-1056
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• 2023

The height of the atmospheric boundary layer indicates the peak developed when turbulence is generated by mixing heat and water vapor, and is generally determined through thermodynamic methods. Wind profilers produce atmospheric information from the scattering of signals sent into the atmosphere. A method for making the spectrum of turbulent components, turbulent kinetic energy dissipation rate, and refractive index structure coefficient was presented to determine the atmospheric boundary layer depth. Compared with the vertical distribution characteristics of potential temperature and specific humidity based on radiosonde data, the determination method of the atmospheric boundary layer height from wind profiler output was evaluated as very useful.

• Journal of the Korean earth science society
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• v.42 no.5
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• pp.504-513
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• 2021

Different physical processes, according to the atmospheric boundary layer types, were used in the Local Data Assimilation and Prediction System (LDAPS) of the Unified Model (UM) used by the Korea Meteorological Administration (KMA). Therefore, it is important to verify the atmospheric boundary layer types in the numerical model to improve the accuracy of the models performance. In this study, the atmospheric boundary layer types were verified using observational data. To classify the atmospheric boundary layer types, summer intensive observation data from radiosonde, flux observation instruments, Doppler wind Light Detection and Ranging(LIDAR) and ceilometer were used. A total number of 201 observation data points were analyzed over the course 61 days from June 18 to August 17, 2019. The most frequent types of differences between LDAPS and observed data were type 1 in LDAPS and type 2 in observed(each 53 times). And type 3 difference was observed in LDAPS and type 5 and 6 were observed 24 and 15 times, respectively. It was because of the simulation performance of the Cloud Physics such as that associated with the simulation of decoupled stratocumulus and cumulus cloud. Therefore, to improve the numerical model, cloud physics aspects should be considered in the atmospheric boundary layer type classification.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2003.11a
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• pp.101-107
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• 2003

해가 지면서 지표면이 냉각되고 지표면의 냉각은 지표부근의 대기를 냉각시켜 상부의 대기보다 차가워지면서 대기의 상태가 안정 상태가 되는데 이 때를 접지 역전층이라고도 하고 야간 경계층이라고도 한다. 야간 경계층은 다음 날 해가 뜨기 전까지 계속 지속되는데 그 고도는 지상 수백m까지 확장될 수도 있다. 이러한 현상은 배출된 대기 오염 물질이 형성된 역전층에 의해 확산이나 수송이 방해를 받게된다. 역전층 상태에서의 오염물질의 배출은 직접적으로 영향을 미치지 않으나, 일출 이후 일사에 의한 지표의 가열로 역전층이 파괴되면서 역전층위의 고농도의 오염물질이 지상으로 유입되어 지표부근에 고농도의 오염을 유발할 수 있다. (중략)

• Journal of the Korean earth science society
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• v.36 no.6
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• pp.553-566
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• 2015

The effects of vertical resolutions and planetary boundary layer (PBL) physics schemes in a numerical simulation with a very high resolution over the metropolitan area were investigated. The numerical experiments using the Weather Research and Forecast model were conducted from 0000 UTC 25 October to 0000 UTC 26 October 2013. We verified the numerical results against with six hourly observation data from the radiosonde at Seolleung, which was located in southern part of Seoul, and forty three auto weather systems in Seoul. In the experiments of vertical resolutions in low level atmosphere with 44, 50, and 60 layers, which are set to be subdivided particularly under 2 km height. The experiment in 60 layers, which has the highest vertical resolution in this study, showed relatively a clear diurnal variation of PBL heights. Especially, the difference of PBL heights and 10-meter wind fields were mainly seen in the area of high altitude lands for the experiments of vertical resolution. In the sensitivity experiment of PBL schemes such as asymmetric convective model-version 2 (ACM2), Yonsei University (YSU), and Mellow-Yamada-Janjic (MYJ) to the temperature, all three PBL schemes revealed lower temperature than observed profile from the radiosonde in the entire period. The experiments with YSU PBL and ACM2 PBL schemes show relatively less biased in comparison with the experiment of the MYJ PBL scheme.

• Proceedings of the Korean Environmental Sciences Society Conference
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• 2003.05a
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• pp.219-222
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• 2003

2002년 3월 28일과 29일에 동해 울릉도에서 존데를 이용하여 관측한 자료와 AWS 자료 등을 이용하여 얻은 이상의 결과를 요약하면 다음과 같다. 일반적인 경우와는 달리 주간에 형성된 혼합층이 일몰 후 야간까지 소멸하지 않았다. 그 이유는 구름으로부터 방출되는 장파복사로 인한 열속(heat flux)이 하층대기를 가열시켜 오히려 기온을 증가시키기 때문이다. 따라서 혼합층은 지면의 열속의 영향을 절대적으로 받는다. 또한 혼합층의 발달과 소멸에 있어서 구름의 영향을 무시할 수 없으며, 구름의 유무에 따라 대기경계층의 일변화는 많은 차이를 나타낸다. 구름 유무에 따른 지속적인 관측이 이루어진다면 더 자세한 영향을 알 수 있을 것이며, 더 나아가 해양대기경계층의 특성 연구에 도움을 줄 것으로 생각된다.

• The Journal of the Korea Contents Association
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• v.19 no.11
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• pp.12-21
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• 2019

In the era of the Fourth Industrial Revolution, drones have become a flexible device that can be integrated with new technologies. The drones were originally developed as military unmanned aircraft and are now being used in various fields. In the environment and weather observation area, the atmospheric boundary layer is near the surface where the atmosphere is the most active in the meteorological phenomenon and has a close influence on human activities. In order to carry out the study of these atmospheric boundary layers, it is necessary to observe precisely the lower atmosphere and secure the observation technology. The drones in the meteorological field can be used for meteorological observations at a relatively low maintenance cost compared to existing equipment. When used in conjunction with various sensors, the drones can be widely used in atmospheric boundary layer and local meteorological studies. In this study, the possibility of meteorological observations using drones was confirmed by conducting vertical meteorological (temperature and humidity) observation experiments equipped with a combined meteorological sensor and a radio sonde on drones owned by NIMS.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2003.11a
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• pp.441-442
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• 2003

복잡한 지형에서 국지적인 순환에 의한 에너지 교환은 기상변화에 중요한 역할을 담당한다. 종관장이 영향이 약하고 양호한 기상조건 하에서 대기 경계층내에서의 온도와 바람장은 국지적인 순환에 영향을 받는다(Kawamura,1979; Kuwagata et al.,1990; Winston et al.,1992). 즉 이러한 기상 조건 하에서는 중규모 순환에 의해 에너지의 수송효과가 크고 각기 수송된 에너지에 의해서 지역별로 대기 경계층내의 가열율에도 차이가 나타난다. (중략)

• Proceedings of The Korean Society of Agricultural and Forest Meteorology Conference
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• 2001.06a
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• pp.65-67
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• 2001

경계층(boundary layer)은 대류권(troposhpere)의 일부분으로써 지구 표면에 직접적인 영향을 주고, 두께는 지표에서 100∼3000m이다. 고기압의 영향을 받는 지역에서 수직 경계층은 일출후부터 일몰 전까지인 낮 시간에 난류 혼합층(turbulent mixed layer), 낮 시간에 형성된 혼합층이 야간에 잔류하는 층, 야간 안정 경계층(Stable Boundary Layer:SBL)으로 나눌 수 있다(Stull, 1988).(중략)

• Proceedings of the Korea Air Pollution Research Association Conference
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• 1998.10a
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• pp.183-185
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• 1998