대류열전달은 겨울철 온실 열손실의 중요한 원인이 되며, 일반적으로 복사열에 의한 손실보다 더 크다. 스크린의 대류열전달계수를 자연상태에서 측정한 연구가 수행된 바는 있지만 상하면의 재질이 동일하고 공극이 없는 스크린에 대해서는 적용을 할 수 없는 방법이다. 이러한 재질의 스크린은 한국에서 많이 사용되고 있으나 대류열전달 특성을 파악하는데 많은 어려움이 있는 실정이다. 본 연구에서는 공극이 없는 3가지 종류의 스크린에 대해 대류열전달계수를 구하였으며, 계수를 산정하기 위하여 복사열수지 이론에 근거하여 산정방법을 개발하였다. 실험장치에 스크린을 설치하고 일사량, 장파복사량, 대기온도, 스크린 및 흑색천의 표면온도, 풍속 등을 측정하였다. 스크린의 표면온도와 주변온도의 차이에 따른 대류열전달계수를 산정하였다. 풍속이 거의 없는 상태에서 온도의 차이가 증가함에 따라 계수는 감소하는 것으로 나타났다.

Red-Green-Blue (RGB) imagery techniques are useful for both forecasters and public users because they are intuitively understood, have advantageous visualization, and do not lose observational information. This study presents a novel RGB convective cloud product and its application to tropical cyclone analysis using Communication, Oceanography, and Meteorology (COMS) satellite observations. The RGB convective cloud product was developed using the brightness temperature differences between WV (6.75 μm) and IR1 (10.8 μm), and IR2 (12.0 μm) and IR1 (10.8 μm) as well as the brightness temperature in the IR1 bands of the COMS, with the threshold values estimated from the Korea Meteorological Administration (KMA) radar observations and the EUMETSAT RGB recipe. To verify the accuracy of the convective cloud RGB product, the product was applied to the center positions analysis of two typhoons in 2013. Thus, the convective cloud RGB product threshold values were estimated for WV-IR1 (−20 K to 15 K), IR1 (210 K to 300 K), and IR1-IR2 (−4 K to 2 K). The product application in typhoon analysis shows relatively low bias and root mean square errors (RMSE)s of 23 and 28 km for DANAS in 2013, and 17 and 22 km for FRANCISCO in 2013, as compared to the best tracks data from the Regional Specialized Meteorological Center (RSMC) in Tokyo. Consequently, our proposed RGB convective cloud product has the advantages of high accuracy and excellent visualization for a variety of meteorological applications.

본 연구의 목적은 2011년 4월 22일부터 10월 22일까지 우리나라에서 강수가 있는 총 75일 동안 COMS 위성의 적외 채널 10.8 μm 휘도 온도(IR), 적외 채널 10.8 μm와 수증기 채널 6.7 μm의 휘도 온도차(IR-WV), 정규화 된 가시 반사도(VIS)와 기상 레이더의 강우강도를 이용하여 2-D와 3-D 대류운의 강우강도 (CRR) 조견표를 향상시키는 것이다. 특별히 한국형 2-D와 3-D CRR 조견표를 검증하기 위해 2011년 강수가 있는 24일 동안의 기상 레이더 강우강도 자료 가 사용된다. 2-D와 3-D CRR 조견표는 각 채널의 등급 범주별 강우 총수와 비강우 총수의 행렬을 이용하여 구한 강 우 확률에 평균 누적강우강도와 최대 강우강도를 각각 곱함으로써 2-D (IR, IR-WV)와 3-D (IR, IR-WV, VIS) 조견표 의 기본과 최대 행렬을 얻을 수 있다. 최종적으로 새로운 2-D와 3-D의 CRR 조견표는 경험적으로 기본과 최대 강우강 도 행렬의 회귀 분석으로 얻어진다. 그 결과 새로운 CRR 조견표는 기존보다 낮은 IR 휘도 온도, 낮은 IR-WV 휘도 온 도차일 때에도 비교적 많은 강우 현상을 나타내며, 10 mm h−1 이상의 강우강도 영역이 확대되어 나타난다. 정확도와 범 주별 통계가 주어진 기간 동안 발생했던 CRR 자료에 대해 계산된다. 새로운 2-D와 3-D CRR 조견표의 평균 오차, 평 균절대 오차, 제곱근평균 오차가 기존 조견표보다 작게 나타나며, 예측 거짓경고비율은 감소하고, 탐지확률은 증가하며, 임계성공지수는 개선된다. 태풍과 뇌우와 같은 기상 이변에서의 강한 호우를 고려하기 위해서 습윤 보정 계수를 교정한 다. 이 인자는 수치모델이나 COMS에서 복원한 지면에서 500 hPa까지 평균한 총가강수량과 상대습도의 곱 (PW·RH) 으로 정의된다. 이 연구에서는 PW·RH에 근거하여 IR 운정 휘도 온도가 210 K 이하일 때, 상대습도가 40% 이상일 때 1에서 2사이를 경험적으로 정한다. 새로운 2-D와 3-D CRR 조견표를 적용한 결과 평균 오차, 평균 절대 오차, 제곱근 평균 오차가 줄어든다.

Self-assembled monolayers(SAM) of microspheres such as silica and polystyrene(PS) beads have found widespread application in photonic crystals, sensors, and lithographic masks or templates. From a practical viewpoint, setting up a highthroughput process to form a SAM over large areas in a controllable manner is a key challenging issue. Various methods have been suggested including drop casting, spin coating, Langmuir Blodgett, and convective self-assembly(CSA) techniques. Among these, the CSA method has recently attracted attention due to its potential scalability to an automated high-throughput process. By controlling various parameters, this process can be precisely tuned to achieve well-ordered arrays of microspheres. In this study, using a restricted meniscus CSA method, we systematically investigate the effect of the processing parameters on the formation of large area self-assembled monolayers of PS beads. A way to provide hydrophilicity, a prerequisite for a CSA, to the surface of a hydrophobic photoresist layer, is presented in order to apply the SAM of the PS beads as a mask for photonic nanojet lithography.

FePt nanoparticles suspension was synthesized by reduction of platinum acetylacetonate and decomposition of iron pentacarbonyl in the presence of oleic acid and oleyl amine. FePt nanoparticles were coated on a substrate by convective assembly from the suspension. To prevent the coalescence during the annealing of FePt nanoparticles double convective coatings were tried. First convective coating was for silica particle assembly on a silicon substrate and second one was for FePt nanoparticles on the previously coated silica layers. It was observed by scanning electron microscopy (SEM) that FePt nanoparticles were dispersed on the silica particle surface. After annealing at 700˚C for 30 minutes under nitrogen atmosphere, FePt nanoparticles on silica particles were maintained in a dispersed state with slight increase of particle size. On the contrary, FePt nanoparticles that were directly coated on silicon substrate showed severe particle growth after annealing due to the close-packing of nanoparticles during assembly. The size variation during annealing was also verified by X-ray diffractometer (XRD). It was suggested that pre-coating, which offered solvent flux oppose to the capillary force between FePt nanoparticles, was an effective method to prevent coalescence of nano-sized particles under high temperature annealing.

대류 상자 실험을 통해 대류 순환 모형을 유추하지 못하는 학생들의 원인을 분석하여 대류 실험을 재설계하였다. 초기 형식적 조작기에 있는 학생들이지만 직접 보지 못한 자연 현상에 대해서는 유추하기가 어려우므로 자연 현상을 축소한 대류 상자를 개발하여 학생들의 과학적 이해도를 높일 수 있는 방법을 연구하였다. 기존 대류 상자 실험의 문제점을 개선하여 제작한 대류 상자를 통해 수업에 적용한 결과 학생들의 이해도가 크게 증가하였다. 바람의 이동 현상만을 관찰하는 것이 아니라 향을 여러 위치에서 넣어봄으로써 과학적 사고를 자극하고 직접 관찰할 수 있었다. 또한 자연 현상의 축소판에 가깝게 설계하여 학생들이 과학적 오개념을 갖지 않는다. 모둠원이 양방향에서 관찰함으로써 수업의 참여도가 높아졌다. 새로 개발된 대류상자는 기존 대류상자에 비하여 저렴한 비용으로 제작할 수 있으며, 선명한 대류 현상을 볼 수 있다.

한반도 집중호우를 유발시키는 중규모대류복합체는 매우 복잡한 특성을 띠고 있다. 2004년 7월 14일 발생한 중 규모 대류복합체의 발달메커니즘을 분석한 결과, a) 대류복합체 생성 전에 강한 남서기류의 유입이 있었으며, b) 600hPa고도에서 강한 역전층이 나타났다. 역전층은 상층과 하층간의 상당온위의 차이를 유발하여 대기불안정을 더욱 강화시켰다. 그리고 c) 일반적인 중규모대류복합체 특징인 풍향의 쉬어보다는 풍속의 쉬어에 의해 대류계의 열역학 불안정이 강화되었다. 그리고 d) 흑산도 등 해안지방에 의해 유발되는 난류 및 대기불안정으로 인하여 중규모 대류복합체가 해안지방에서 발달한 것으로 보인다. 그러므로 지형에 의한 중규모 대류 복합체의 발달메커니즘 규명이 필요하다.

본 논문은 비균일대칭성 열Flux인 수직사각 Duct내의 층류조합대류 열전달 효과를 해석하기 위하여 그 유동의 특성 지배 방정식 및 비균일 열Flux의 경계조건을 무차원화 시켜 이를 Galerkin's 방법에 의해 유한요소식으로 정식화하고 이에 대하여 R 하(a) 수 및 압력구배 변수에 대해서 Duct 내의 온도분포, 속도분포 및 Nusselt 수의 값을 계산하였고 온도분포를 열 Flux가 일정 및 없는 경우와 비교하였으며 또 닥트내의 열전달 특성을 R 하(a) 수, 응력구배변수 및 Corner에 따른 변호경향을 조사하였다. 그 결과 1. 본 해석의 경계벽 온도분포 계산치와 유효자료들과의 비교에서 열 Flux가 일정 또는 없는 경우는 그 값이 일치하였다. 2. 닥트내의 온도분포와 Nusselt수의 값은 R 하(a) 수 및 압력구배 변수에 비례하여 증감하였다. 3. Nusselt수는 Corner에서 유속지연에 의한 온도분포의 특성 때문에 그 값이 감소하였으며 최대치는 0.7부근이었다

Effect of the ratio of mixing length to the pressure scale-height α =l/HP on the effective temperature has been investigated under some simplifying assumptions. The result is compared with that of the existing model calculations. The role of convection zone in the stellar evolution is briefly summarized.

Successful launch requires state-of-the-art launch vehicle technology and constant test operations, However, the meteorological threat to the launch vehicle flight trajectory is also an important factor for launch success. Atmospheric stability above the Naro Space Center at the this time is very important, especially because the initial flight operation can determine the success of the launch. Moreover, during the flight of launch vehicle with rapid pressure and thrust into the atmosphere, convection activity in the atmosphere may create environmental conditions that cause severe weather threats such as thunderstorms. Hence, studies of atmospheric instability characteristics over the Naro Space Center are a necessary part of successful launch missions. Therefore, the main aims of this study were to (1) verify the atmospheric stability index and convection activity characteristics over the Naro Space Center using radiosonde data observed from 2007 to 2018 by the Naro Space Center, (2) analyze changes in the atmospheric stability index according to monthly and seasonal changes, and (3) assess how the calculated atmospheric stability index is related to actual thunderstorm occurrence using statistical analysis. Additionally, we aimed to investigate the atmospheric characteristics above the Naro Space Center through the distribution chart of the atmospheric stability index during summer, when convection activity is highest. Finally, we assessed the relationship between lightning occurrence and unstable atmospheric conditions, through predictability analysis performed using the lightning observation data of the Korea Meteorological Administration.

On the study of the characteristics and life cycle of mesoscale convective band in type of airmass that occurred in the Honam area from June to September for only 4 years in the period of 2009~2012, 10 examples based on the amount of rainfall with AWS 24 hours/60 minutes rainfalls, Mt. Osung radar 1.5 km CAPPI/X-SECT images and KLAPS data for convective band with heavy rainfall event were selected. There were analyzed and classified by using the convective band with heavy rainfall occurred along the convergence line of sea wind in the form of individual multi-cellular cell and moving direction of convective band appeared in a variety of patterns; toward southwestern (2 cases), northeastern (4 cases), congesting (2 cases), and changing its moving direction (2 cases). The case study dated of the 17th Aug. 2012 was chosen and implemented by sequentially different evolution of its shape along the convergence line of sea wind cell and moving direction of convective band as equivalent potential temperatures at the lower layer have increased to the upper layer 500 hPa, that the individual cells were developed vertically and horizontally through their merger, but owing to divergence caused by weakened rainfall and descending air current, the growth of new cell was inhibited resulting in dissipation of convective cells.

Meteosat-5 IR 위성영상을 사용하여 1999년과 2000년 여름몬순기간 동안 발생한 네팔과 인디아 북쪽 히말라야 산악지역에 발생하는 여러 형태의 대류계 즉, 중규모 대류계들 (Mesoscale Convective Complex, MCC and Convective Cloud Clusters, CCC) 와 보다 약한 Disorganized Short-lived Convection (DSL)의 이동특성 및 시공간적인 생성특성 등을 조사하였다. 대상지

A Jump model was evaluated for the calculation of hourly mixing height and mean potential temperature within the height. The Jump model was modified for estimation of downward heat fluxes by mechanical convections and surface heat fluxes. The surface heat fluxes were estimated from routine weather data such as solar radiation and air temperature. Total of 8 upper-air data observed at 0000UTC and 0600UTC in Osan station during April 23 to 26, 1996 were analyzed, and compared to the model results in detail. The calculated mixing heights and potential temperatures within the height were comparable to the observations, but some differences were showed. The calculated mixing heights were generally higher than observations. And, when variations of wind directions were large, the large difference of potential temperature was occurred. From the results, it was important to note that vertical motions and advections of air masses would affect to the growth of the mixing height.

We examined the drying characteristics and the drying rate model equation of garlic(allium sativum L.) using computer aided convective drying. The drying chanacteristic curve of garlic divided into constant rate drying period and 2 stage of falling rate drying period. The drying rate was fairly affected by hot air temperatures during the total drying period, but air flow rates has nearly no effect on the drying rate except initial drying period. Of the several model equation, r2 values of page model equation was the highest, and the estimated drying profiles were comparatively coincided with the observed drying profiles. Page model equation was suitable to predict the drying rate and moisture content during drying of sliced garlic.

To convert the analog signal from the drying process into the digital signal, the interface circuit was designed and built. To measure the weight and temperature during drying process, strain gauge type load cell and temperature transducer composed of pt 100 thermometers and wheatstone bridge circuits were built and used. The temperature control device was composed of photocoupler and triac. Microcomputer aided experimental convective drying system was built with above cricuits and devices. Drying characteristics of onions can be estimated using this system.