• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume II
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• pp.1001-1002
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• 2006

Special problem emphasized by specialists in the field of analyzing the heat interchanges in the system ocean-atmosphere (SOA) is a necessity of determination of the near-surface atmospheric temperature, which can be only indirectly connected with characteristics of the SOA natural microwave radiation measured from satellites. That is why, the following dilemma is not obvious, but interesting and promised: what is better - to use the satellite methods for retrieving the partial parameters of the SOA or for analysis its state as a whole. To our opinion, this task is similar to the idea recognized by specialists engaged in the heat infrared region (8-12 mcm) of electromagnetic spectrum and its applications, where an intensity of natural infrared radiation (effective radiation) is used as the inherent property (the attribute) of the SOA heat balance. Here we studied important aspects of this problem: a) what medium initiates a heat transfer in the SOA and disturbs its heat balance - the ocean or the atmosphere b) what SOA parameters directly influence on its natural microwave radiation intensity (brightness temperature) measured from satellites? We relate these processes mainly to the synoptic range of time scales enriched by various events in the SOA interface such as the mid-latitude and tropical cyclones.

• 대기
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• 제24권4호
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• pp.471-479
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• 2014

A road surface temperature prediction model (UM-Road) using input data of the Unified Model (UM) output and road physical properties is developed and verified with the use of the observed data at road weather information system. The UM outputs of air temperature, relative humidity, wind speed, downward shortwave radiation, net longwave radiation, precipitation and the road properties such as slope angles, albedo, thermal conductivity, heat capacity at maximum 7 depth are used. The net radiation is computed by a surface radiation energy balance, the ground heat flux at surface is estimated by a surface energy balance based on the Monin-Obukhov similarity, the ground heat transfer process is applied to predict the road surface temperature. If the observed road surface temperature exists, the simulated road surface temperature is corrected by mean bias during the last 24 hours. The developed UM-Road is verified using the observed data at road side for the period from 21 to 31 March 2013. It is found that the UM-Road simulates the diurnal trend and peak values of road surface temperature very well and the 50% (90%) of temperature difference lies within ${\pm}1.5^{\circ}C$ (${\pm}2.5^{\circ}C$) except for precipitation case.

• Journal of Radiation Protection and Research
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• 제9권1호
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• pp.11-18
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• 1984

Well type 전리함과 미세전류 측정희로를 사용하여 표준 감마선 전리함 장치를 개발하였다. 미세전류는 automatic Townsend balance with stepwise compensation방법을 사용하여 측정하였다. $^{226}Ra$을 기준 선원으로 택하여 감마 방출핵종인 $^{241}Am,\;^{133}Ba,\;^{60}Co,\;^{134}Cs,\;^{137}Cs^{22}Na$에 대한 비교 교정인자를 산출하였으며, 감마에너지의 함수로서 검출 효율 곡선을 구하였다.

• 한국환경과학회지
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• 제4권3호
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• pp.197-206
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• 1995

Surface heat balance of the northern sea of Cheju Island for summer in 1993 and 1994 is analyzed using the observation data obtained by Marine Research Institute, Cheju National University. Each flux elements at the sea surface is derived from the marine meteorological reports with application of an aerodynamical bulk method for the turbulent heat fluxes, and empirical formulae for the long-wave radiation heat fluxes. The flux divergence of oceanic heat transport and the rate of heat storage in the ocean are estimated as residual. The features of the surface heat balance are mainly decided by the solar radiation flux and the latent heat flux for 199B. But the Bowen Ratios were large for 1993. This means that the sensible heat fluxes were nearly equal to the latent heat fluxes for 1993. In this period, mean flux divergence of oceanic heat transport is about 130 W/$m^2$.

• 한국추진공학회:학술대회논문집
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• 한국추진공학회 2010년도 제34회 춘계학술대회논문집
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• pp.450-459
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• 2010

고체추진제의 첨가제 또는 연료로써 주로 사용되는 알루미늄 단일 입자 연소시험 장비를 제작하고 연소 실험을 수행하였다. 산화 알루미늄으로 피복된 금속입자는 약 30~100 ${\mu}m$의 크기를 사용하였다. 단일 입자는 Electrodynamic Balance (EDB) 방법에 의해 공중 부양된 상태로, 중력에 의한 영향이 배제되어 금속입자 고정용 또는 측정용 장치들의 접촉에 의한 열손실을 제거시켜 실험 정확도를 높였다. Standard Hyperbolic Electrodynamic Levitator (SHEL) 내에서 부양된 입자에 $CO_2$ 레이저를 사용하여 점화시킨 후, 입자로부터 방사되는 열복사를 이용한 two wavelength pyrometry를 적용하여 알루미늄 입자 크기에 따른 연소시간, 평균 화염온도, 점화온도, 점화시간을 획득하였으며, 단일 알루미늄 입자의 점화-연소특성을 평가하였다.

• 태양에너지
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• 제20권3호
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• pp.61-73
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• 2000

Heat losses from receivers for a dish-type solar energy collecting system are numerically investigated. The analytical method for predicting conductive heat loss from a cavity receiver is used. The Stine and McDonald Model is used to estimate convective heat loss. Two kinds of techniques for the radiation analysis are used. The Net Radiation Method that is based on the radiation heat balance on the surface is used to calculate the radiation heat transfer rate from the inside surface of the cavity receiver to the environment. The Monte-Carlo Method that is the statistical approach is adopted to predict the radiation heat transfer rate from the reflector to the receiver. Based on the heat loss analysis, the performance of two different receivers for multifaceted parabolic solar collectors with several flat facets can be estimated, and the optimal facet size is obtained.

• 한국토양비료학회지
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• 제23권2호
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• pp.94-99
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• 1990

콩군낙(群落)(팔달(八達)콩 ; 재식밀도(栽植密度) $45{\times}10cm$)에서의 열수지성분(熱收支成分) 변화(變化)를 계절별(季節別)로 관측(觀測)하고 열수지법(熱收支法)으로 증발산량(蒸發散量)을 계산(計算)하여 건물생산량(乾物生産量)과의 관계(關係)를 구한 결과(結果)는 다음과 같다. 1. 맑은날의 전단파복사량(全短波輻射量)에 대한 순복사량(純輻射量)의 비율(比率)은 59~76%로 흐린날의 63~83%보다 낮았다. 2. 순복사량(純輻射量)에 대한 잠열전달량(潛熱傳達量)의 비율(比率)은 흐린날에 100%를 넘는 경우가 있어 때때로 이류(移流)에 의한 열복사(熱輻射)의 수평전도(水平傳導)가 있었다. 3. 1시간(時間)마다 적산(積算)한 일적산순복사량(日積算純輻射量)(Rn)과 증발잠열(蒸發潛熱)($LE_{(+)}$) 및 화간순복사량(畵間純輻射量)($Rn_{(+)}$)과 증발잠열(蒸發潛熱)과의 관계(關係)는 각각(各各) 다음과 같은 직선관계(直線關係)가 성립(成立)하였다. $$LE_{(+)}=0.971\;Rn+1.122\;R^2=0.9017$$ $$LE_{(+)}=0.882\;Rn_{(+)}+1.945\;R^2=0.8836$$ 4. 열수지계산(熱收支計算)에 의한 군낙증발산량(群落蒸發散量)(ETa)과 대형(大型) pan 증발량(蒸發量)(Epan)과의 관계(關係)는 다음과 같았다. ETa = 1.049 Epan + 1.657 $$R^2=0.6589$$ 5. 생육초기(生育初期)를 제외(除外)한 생육기간중(生育期間中) 건물(乾物)로의 물이용효율(利用效率)은 $2.31g{\cdot}DM{\cdot}kg^{-1}\;H_2O$이었으며, 평균일증발산량(平均日蒸發散量)은 5.29mm, 일사량중(日射量中) 군낙(群落)의 증발산(蒸發散)으로 소비(消費)된 열량(熱量)의 비율(比率)은 85%이었다.

• 천문학회보
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• 제36권1호
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• pp.54.2-54.2
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• 2011

It is the conventional wisdom that the Poynting-Robertson effect is essentially the outcome of the interplay between absorption and reemission processes. For a better understanding of the motion of charged particles around a compact star with strong radiation, we reached an alternative interpretation for the Poynting-Robertson effect based on the covariant formalism and found that it is attributed to the combination of the aberration and the Lorentz transformation of the radiation stress-energy tensor. As a general relativistic application of the Poynting-Robertson effect, we studied the dynamics of test particles around the spinning relativistic star with strong radiation. We discovered that the combination of the angular momentum and the finite size of the star generates "radiation counter drag" which exerts on the test particle to enhance its specific angular momentum, contrary to the radiation drag. The balance of the radiation drag and the radiation counter drag renders the particle to hover around the spinning luminous star at the "suspension orbit". The radial position and the angular velocity of the particle on the "suspension orbit" are determined by the angular momentum, the luminosity, and the size of the central star only, and they are independent of the initial position and velocity of the particle.

• 한국농림기상학회지
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• 제11권2호
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• pp.79-85
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• 2009

순복사는 지표와 대기간의 생물학적/물리적 과정을 일으키는 주요 원인이며 순복사에 대한 정확한 정보는 기후 예측뿐만 아니라 수자원관리에 중요한 역할을 한다. 그러나 실제 순복사 관측을 하는 지점은 매우 적으며 일반적으로 순복사는 단순 경험방정식으로부터 추정된다. 이 연구에서는 한국의 세 개의 다른 식생기능형태(예, 혼합림, 침엽수림, 그리고 농경지)에서 순복사를 추정하는 두 방법을 제시하였다. 첫번째 방법은 순복사와 전천일사의 관계를 선형회귀식으로 나타낸 방법이고 두번째 방법은 복사수지방정식을 사용한 방법이다. 세 개의 다른 식생기능형태에서 관측된 2008년 자료를 두 방법에 적용하여 순복사를 추정하였다. 일년 자료를 사용하여 선형회귀식을 적용한 결과, 전천일사에 대한 순복사의 비율은 혼합림에서는 70%, 침엽수림에서는 79%, 그리고 농경지에서는 64%를 보였다. 이는 다른 식생기능형태에 따라 순복사와 전천일사의 관계가 달라짐을 보였다. 장파복사를 고려한 복사수지 방정식의 경우, 순복사 추정이 다소 향상되었다. 두 방법 모두 관측된 순복사와 추정된 순복사가 잘 일치함을 보였으며 이는 두 방법을 사용하여 순복사를 추정할 수 있음을 보여준다.

• 한국대기환경학회지
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• 제19권3호
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• pp.285-296
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• 2003

The measurement of the radiation energy, trunk temperature, leaf area index (LAI), air temperature, vapor pres-sure, and precipitation has been conducted under a mixed forest at Kwangneung Arboretum during the period of 2001. Characteristics of the diurnal and seasonal variation of the radiative energy were investigated. The aerodynamic roughness length was determined as about 1.6 m and the mean albedo was about 0.1 The downward short-wave radiation was linearly correlated with the net radiation and its correlation coefficient was about 0.96. From this linear relation, the heating coefficient was calculated and its annual mean value was about 0.21 The albedo and heating coefficient was varied with season, surface characteristics, and meteorological conditions. The diurnal and seasonal variations of radiation energy were discussed in terms of the surface characteristics and meteorological conditions. In the daytime, during clear skies, net radiation was dominated by the shortwave radiation. In presence of clouds and fog, the radiation energy was diminished. At night, the net radiation was entirely dominated due to the net longwave radiation. There was no distinct diurnal variation in net radiation flux during the overcast or rainy days. The net radiation was strongest in spring and weakest in winter. The seasonal development in leaf area was also reflected in a strong seasonal pattern of the radiation energy balance. The timing, duration, and maximum leaf area and trunk temperature were found to be an important control on radiation energy budget. The trunk temperature was either equal or warmer than air temperature during most of the growing season because the canopy could absorb a substantial amount of sunlight. After autumn (after the middle of October), the trunk temperature was consistently cooler than air temperature.