• 천문학논총
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• 제14권2호
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• pp.69-78
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• 1999

We present the results of one-dimensional numerical simulations of SNR evolution in the in­homogeneous medium considering the effects of the evaporation of the cloud and the thermal conduction. We have included the effects of changing evaporation rate as a function of cloud size and the ambient temperature so that the clouds could be evaporated completely before they reach the center of the SNR. The heat conduction markedly changes the density distribution in the remnant interior. To explain the observed morphologies of the centrally peaked X-ray SNRs(for example W44), the maximal thermal conduction is required. However, this is unlikely due to the magnetic field and the turbulent motion. The effects of the evaporation of the cloud and the thermal conduction described here may explain the class of remnants observed to have centrally peaked X-ray emmision.

• 대한원격탐사학회지
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• 제23권2호
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• pp.71-87
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• 2007

본 연구는 NASA/GSFC에서 제공하는 MODIS 구름 산출물 자료를 활용하여 국지적 현상으로 나타난 영동지역의 14개 대설 사례를 분석하였다. MODIS에 의해 특정시간에 관측된 영동지역의 구름은 운정 온도(CTT), 광학 두께(COT), 유효 입자 반경$(r_e)$, 입자상(CP)과 같이 구름 내 속성의 특징에 따라 A, B, C 형으로 분류하였다. 각각의 구름 형태에 대한 강수량과 구름의 속성 사이의 연관성 분석에서 COT는 A와 B형에서 상당히 높은 통계적으로 유의한 관계성을 보였으며, CTT는 A형에서만 높은 상관성을 보였다. 그렇지만, C형에서는 통계적으로 유의한 관계성이 구름의 특성물에 대해 나타나지 않았다. A형 구름은 작은 크기의 물방울과 함께 주로 낮은 층운형 구름으로 구성되어 있으며, 동해에서 종관적으로 유도된 하층 한기 이류 하에서 발생할 수 있다. B형 구름은 발달하는 적운형 구름과 관련되어 있으며, 이러한 구름은 동해상에서 발달하는 저기압 중심과 밀접하게 관련되어 있다. 그렇지만, C형 구름은 다층 구름들로써 영동대설과 직접적으로 관련된 하층 구름을 상층구름이 덮고 있어 위성 관측이 어렵다. 따라서 MODIS 구름 산출물은 영동대설의 경우에 다층 구름을 제외하고 위성 자료로부터 강수량 추정과 대설 기작을 이해하는데 도움이 될 수 있다고 결론지을 수 있다.

• 대기
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• 제29권4호
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• pp.481-499
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• 2019

National Institute of Meteorological Sciences has conducted a total 54 cloud seeding experiments with a silver iodide and calcium chloride using aircrafts from 2008 to 2018. The goal of the experiments is to improve the techniques of precipitation enhancement in Korea. The cloud seeding experiments using the silver iodide and calcium chloride were 36 and 18 times, respectively. During the cloud seeding experiments of the silver iodide and calcium chloride, the average values of total cloud amount for two kinds of seeding materials were 9.6 for and 8.1, respectively. The cloud type with the highest occurrence was Nimbostratus (Ns)-Stratus (St) (58%) in the silver iodide cloud seeding experiment. It was Altostratus (As)-Stratocumulus (Sc) (44%) in the calcium chloride cloud seeding experiment. Compared to probability of obtaining cloud seeding effect of the experiments using a leased aircraft, the probability using an atmospheric research aircraft increased from 43% to 63% in the silver iodide cloud seeding experiment and from 29% to 75% in the calcium chloride cloud seeding experiment. However, the increasing tendency was only shown during the one year experiment (2018). To get the meaningful statistical tendency of the cloud seeding effects, it is needed to implement many experiments in several years. Further we have to more clearly understand the characteristics of clouds developing in Korea and implement the cloud seeding experiments under a variety of weather conditions in order to develop the optimized precipitation enhancement technology in Korea.

• 대기
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• 제31권5호
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• pp.489-510
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• 2021

In this paper, we propose an algorithm for detecting convective initiation (CI) using GEO-KOMPSAT-2A/advanced meteorological imager data. The algorithm identifies clouds that are likely to grow into convective clouds with radar reflectivity greater than 35 dBZ within the next two hours. This algorithm is developed using statistical and qualitative analysis of cloud characteristics, such as atmospheric instability, cloud top height, and phase, for convective clouds that occurred on the Korean Peninsula from June to September 2019. The CI algorithm consists of four steps: 1) convective cloud mask, 2) cloud object clustering and tracking, 3) interest field tests, and 4) post-processing tests to remove non-convective objects. Validation, performed using 14 CI events that occurred in the summer of 2020 in Korean Peninsula, shows a total probability of detection of 0.89, false-alarm ratio of 0.46, and mean lead-time of 39 minutes. This algorithm can be useful warnings of rapidly developing convective clouds in future by providing information about CI that is otherwise difficult to predict from radar or a numerical prediction model. This CI information will be provided in short-term forecasts to help predict severe weather events such as localized torrential rainfall and hail.

• 대기
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• 제25권4호
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• pp.577-589
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• 2015

An unusual long-period and heavy snowfall occurred in the Yeongdong region from 6 to 14 February 2014. This event produced snowfall total of 194.8 cm and the recordbreaking 9-day snowfall duration in the 103-year local record at Gangneung. In this study, satellite-derived cloud-top brightness temperatures from the infrared channel in the atmospheric window ($10{\mu}m{\sim}11{\mu}m$) are examined to find out the characteristics of clouds related with this heavy snowfall event. The analysis results reveal that a majority of precipitation is related with the low-level stratiform clouds whose cloud-top brightness temperatures are distributed from -15 to $-20^{\circ}C$ and their standard deviations over the analysis domain (${\sim}1,000km^2$, 37 satellite pixels) are less than $2^{\circ}C$. It is also found that in the above temperature range precipitation intensity tends to increase with colder temperature. When the temperatures are warmer than $-15^{\circ}C$, there is no precipitation or light precipitation. Furthermore this relation is confirmed from the examination of some other heavy snowfall events and light precipitation events which are related with the low-level stratiform clouds. This precipitation-brightness temperature relation may be explained by the combined effect of ice crystal growth processes: the maximum in dendritic ice-crystal growth occurs at about $-15^{\circ}C$ and the activation of ice nuclei begins below temperatures from approximately -7 to $-16^{\circ}C$, depending on the composition of the ice nuclei.

• 한국기록관리학회지
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• 제14권3호
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• pp.153-179
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• 2014

2006년 법령이 개정된 후 공공기관에 전자기록관리시스템이 도입되어 대부분의 기관이 기록관에 디지털 저장소를 구축했다. 이 시스템은 도입과 유지에 많은 비용과 인력이 소요되고, 저장소의 확장성이 떨어지며, 상호운용성의 확보가 어려운 단점이 있다. 이에 본 연구에서는 클라우드 컴퓨팅 기술을 전자기록관리시스템에 도입하여 기존 시스템이 지닌 문제를 개선해 더 나은 시스템을 구축할 모델을 제시하였다. 특히 클라우드 컴퓨팅의 장점인 저비용 고효율, 빠른 확장성, 다양한 시스템을 하나로 포용할 수 있는 상호운용성이 공공기관의 전자기록관리시스템 운용에 적용될 때 얻게 될 기대효과를 제시해 향후 클라우드 기술의 도입의 당위성을 제기한다.

• 한국전자통신학회논문지
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• 제7권6호
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• pp.1245-1258
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• 2012

본 연구는 미래예측방법으로 많이 활용되고 있는 시나리오플래닝 방법론을 적용하여 한국 전자정부 기술개발의 바람직한 미래상을 도출하였다. 최근 웹에서 유비쿼터스로의 지식정보화사회의 급속한 진행으로 IT와 컴퓨팅기술에 있어, 전 세계적으로 클라우드 컴퓨팅이라는 새로운 패러다임이 불고 있다. 따라서 이는 한국 정부 및 각국 정부에 있어, 전자정부 구축과 추진에 있어서의 주목할 만한 전환점이 되고 있다. 본 연구는 클라우드 컴퓨팅 기술과 함께하는 한국 전자정부의 상대적 미래우위전략을 찾고자, 기술개발 방향을 고찰하였으며, 그 결과 한국의 전자정부에 부합하는 -서비스 수준관리(SLA)나 자원제공과 같은- 하드웨어 및 인터넷 데이터센터 관련 기술과 함께, -오픈API나 자원가상화 같은- 소프트웨어 (응용)솔루션 기술에 관련된 클라우드 컴퓨팅 기술의 중점적 개발이 그 추진할 전략이었다.

• Asian Journal of Atmospheric Environment
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• 제8권4호
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• pp.175-183
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• 2014

To visually and chemically verify the rainout of soot particles, a model experiment was carried out with the cylindrical chamber (0.2 m (D) and 4 m (H)) installing a cloud drop generator, a hydrotherometer, a particle counter, a drop collector, a diffusing drier, and an artificial soot particle distributer. The processes of the model experiment were as follows; generating artificial cloud droplets (major drop size : $12-14{\mu}m$) until supersaturation reach at 0.52%-nebulizing of soot particles (JIS Z 8901) with an average size of $0.5{\mu}m$-counting cloud condensation nuclei (CCN) particles and droplets by OPC and the fixation method (Ma et al., 2011; Carter and Hasegawa, 1975), respectively - collecting of individual cloud drops - observation of individual cloud drops by SEM - chemical identifying of residual particle in each individual droplet by SEM-EDX. After 10 minutes of the completion of soot particle inject, the number concentrations of PM of all sizes (> $0.3{\mu}m$) dramatically decreased. The time required to return to the initial conditions, i.e., the time needed to CCN activation for the fed soot particles was about 40 minutes for the PM sized from $0.3-2.0{\mu}m$. The EDX spectra of residual particles left at the center of individual droplet after evaporation suggest that the soot particles seeded into our experimental chamber obviously acted as CCN. The coexistence of soot and mineral particle in single droplet was probably due to the coalescence of droplets (i.e., two droplets embodying different particles (in here, soot and background mineral particles) were coalesced) or the particle capture by a droplet in our CCN chamber.

• 전자공학회논문지 IE
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• 제47권1호
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• pp.56-60
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• 2010

IT의 폭넓은 개발, Web 2.0 애플리케이션의 의 발전, 인터넷이 가능한 개인용 단말장치의 증가, 무선 네트워크의 유용성 등은 클라우드 컴퓨팅 모델을 만드는데 매우 중요한 역할을 수행하였다. 클라우드 컴퓨팅은 하나의 비즈니스 모델이며, 웹 애플리케이션의 새로운 트렌드다. 또한 형식은 그리드 컴퓨팅이나 유틸리티 컴퓨팅과 같은 형태를 사용한다. 클라우드 컴퓨팅 환경에서는 서버의 같은 하드웨어 자원을 사용할 수 있으며 정보를 공유하기 쉽다. 본 연구에서는 클라우드 컴퓨팅 환경에서 이러닝 분야를 적용하기 위한 방안을 제시한다. 이를 위하여 클라우드 컴퓨팅환경에서 LMS와 LCMS 기반의 이러닝을 제시하고자 한다. 이는 클라우드 컴퓨팅의 데이터센터에 LCMS를 포함한 LMS를 접속하도록 하였다.

• 대한원격탐사학회지
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• 제39권5_1호
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• pp.507-519
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• 2023

Multi-temporal optical images have been utilized for time-series monitoring of croplands. However, the presence of clouds imposes limitations on image availability, often requiring a cloud removal procedure. This study assesses the applicability of various machine learning algorithms for effective cloud removal in optical imagery. We conducted comparative experiments by focusing on two key variables that significantly influence the predictive performance of machine learning algorithms: (1) land-cover types of training data and (2) temporal variability of land-cover types. Three machine learning algorithms, including Gaussian process regression (GPR), support vector machine (SVM), and random forest (RF), were employed for the experiments using simulated cloudy images in paddy fields of Gunsan. GPR and SVM exhibited superior prediction accuracy when the training data had the same land-cover types as the cloud region, and GPR showed the best stability with respect to sampling fluctuations. In addition, RF was the least affected by the land-cover types and temporal variations of training data. These results indicate that GPR is recommended when the land-cover type and spectral characteristics of the training data are the same as those of the cloud region. On the other hand, RF should be applied when it is difficult to obtain training data with the same land-cover types as the cloud region. Therefore, the land-cover types in cloud areas should be taken into account for extracting informative training data along with selecting the optimal machine learning algorithm.