• 한국환경과학회지
• /
• 제8권3호
• /
• pp.293-297
• /
• 1999

Based on the monthly weather report of Korea Meteorological Administration (KMA) and daily sea surface temperature (SST) in Incheon harbor of National Fisheries Research and Development Institute, heat budget in Incheon coastal area was estimated. The temperature differences between the sea surface and near bottom were nearly within 1$^{\circ}C$. This indicate the mixing from the sea surface and the bottom. The net heat flux through the sea surface and the advection through the inner and outer bay was affected uniformly to the water body in Incheon coastal area. The net heat flux was about 110W/$m^2$ in maximum value on May, about -80W/$m^2$ in minimum on January. The net heat flux through the sea surface from the solar radiation was about 2.35$\times$${10}^5$W during the year. This heat flux flew out the bay through the advection by the same flux.

• 한국환경과학회지
• /
• 제3권2호
• /
• pp.89-100
• /
• 1994

It is very important to assess accurately the terms which are included in the heat budget equation of soil surface because they are used in the UM and miso-scale circulation modeling as well as in the micrometeorological studies. Each terms in the heat budget equation change according to the soil moisture content. So, it is necessary to specify clearly the relations between soil moisture content and these terms. Special experiment with micrometeorological measurements was executed to study these relations at Environmental Research Center of Tsukuba University, Japan. The results are as follow: 1. The soil moisture contents of 1 cm and 4 cm depth are oscillated with one day Period in drying process and the amplitude of variation of 1 cm depth is greater than that of 4 cm. 2. Increase in soil moisture contents due to precipitation result in decrease of albedo with step function. 3. Sensible heat is in reverse proportion to the soil moisture content and latent heat is in direct proportion to it. Latent heat is more sensitive than sensible heat according to the soil moisture variation. Net long wave radiation have high correlation with soil moisture. 4. Comparing with the radiative term with the flux term in wetting process due to precipitation, the energy transfer of the aero and thermodynamic flux is greater than that of the radiative heat flux.

• 한국환경과학회지
• /
• 제25권8호
• /
• pp.1057-1063
• /
• 2016

The heat budget is investigated in the Gumi Reservoir of the Nakdong river. In warm climate season, solar radiation effects play a important role in the change of water temperature. The features of the surface heat balance are almost derived by the latent heat flux and the solar radiation flux. On the other hand, in cold climate season, change of heat stored in the water is mainly dominated by latent and sensible heat transfer between water and air, since flux of solar radiation and loss of outgoing long wave radiation balance approximately. For the annual averages, net flux of radiation, evaporation(latent heat) loss are dominant in the Gumi reservoir. The evaporation losses are dominant from spring to early winter. This means that the Gumi reservoir rolls like a lake of thermal medium or deep depth.

• 한국환경과학회지
• /
• 제4권3호
• /
• pp.197-206
• /
• 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/$m^2$.

• 한국환경과학회지
• /
• 제7권1호
• /
• pp.67-73
• /
• 1998

Surface heat budget of the Deukryang Bay from July 1, 1992 to September 12, 1993 is analyzed by us- ing the meteorological data (by Changhung Observatory and Mokpo Meteorological Station) and oceanogaphical data (by Research Center for Ocean Industrial Development. Pukyong National University). Each flux element at the sea surface which has annual variation Is derived with application of an aerodynamical bulk method and empirical formulae. The solar radiation Is the maximum In spring and sensible heat are the maximum in autumn and water. and minimum in summer The heat .storage rate is calclilated by using the rate of water temperature variation according to the depth. The oceanic transport heat is estimated as a residual. The net heat flux, the heat storage rate are positive In spring and summer, while they are negative in autumn and winter. The oceanic transport heat Is convergence In winter and divergence In the rest of seasons.

• 한국조경학회지
• /
• 제40권6호
• /
• pp.190-197
• /
• 2012

본 연구는 저관리 경량형 옥상녹화의 열수지를 정량화하기 위하여 모의실험을 수행하였다. 콘크리트블록을 이용하여 가로 $1.2m{\times}$세로 $1.2m{\times}$높이 1m의 모의실험구 2개를 제작하여 하나는 한국잔디를 식재한 토심 10cm의 옥상녹화 실험구로 하였으며, 옥상녹화를 실시하지 않은 나머지 하나는 대조구로 하였다. 2012년 6월 6일~7일에 기온, 상대습도, 풍향, 풍속 등 외부 기상환경, 증발산량, 옥상녹화와 대조구인 콘크리트의 표면과 천장면의 온도, 열류량, 열수지를 측정하였다. 6일과 7일의 일최고기온은 각각 $29.4^{\circ}C$와 $30^{\circ}C$로 초여름 날씨로는 매우 무더웠다. 6일과 7일의 일증발산량은 각각 $2,686.1g/m^2$과 $3,312.8g/m^2$이었으며, 일사량이 증가함에 따라 증발산량도 증가하였다. 외부 기온이 가장 높은 시간일 때의 옥상녹화 표면과 대조구 표면의 온도차이를 비교해 보면 대조구 표면이 $5.5^{\circ}C$(6일)와 $2.2^{\circ}C$(7일) 더 높은 것으로 나타났다. 옥상녹화 천장과 대조구 천장의 온도차이를 비교해 보면 $13.1^{\circ}C$(6일)와 $14.2^{\circ}C$(7일)로 나타나 옥상녹화에 의한 실내온도저감효과가 매우 큰 것으로 나타났다. 옥상녹화와 대조구인 콘크리트 표면의 열수지를 분석한 결과, 옥상녹화는 순복사량과 잠열량이 많은 비율을 차지하고 있었으나 대조구는 현열량과 전도열량의 비율이 높았다. 즉, 옥상녹화는 한국잔디와 식재토양에 의한 증발산으로 열을 식혀주는 잠열의 비율이 높은 반면에 대조구인 콘크리트 표면은 식물이 식재되어 있지 않기 때문에 열을 식혀주는 잠열은 $0W/m^2$인 반면에 주위 온도를 증가시키는 현열량과 건물내로 전달되는 전도열량의 비율이 높아 표면과 천장면의 온도를 상승시켰다. 본 연구는 옥상녹화의 온도저감과 열수지 해석을 시도했다는 점에서는 매우 의의가 크다고 할 수 있지만, 옥상녹화는 토심과 토양배합비, 식물종, 계절 등 여러 변수에 따라 온도저감효과가 다르게 나타날 수 있기 때문에 이에 대한 후속연구가 필요하다.

• 한국대기환경학회지
• /
• 제13권2호
• /
• pp.103-113
• /
• 1997

The research described in this paper was conducted to estimate the stability and heat budget in planetary boundary layer (PBL) at Kimhae. The upper air observation was carried out during period from 3 Februsry 1993 to 5 February 1993 at Kimhae. The surface observation data used the one during period from 1 April 1994 to 31 March 1995. The maximum height of inversion layer observed at Kimhae was 310 m. Destruction of the inversion was simultaneously occurred at the surface and the mid-layer (200 $\sim$ 300 m), however the origin of destruction is different each other. The surface inversion is destructed by surface heating owing to growing radiation in surface but disappearance of the mid-layer inversion is related to the upper cold air movement.

• 한국환경과학회지
• /
• 제5권6호
• /
• pp.727-738
• /
• 1996

An one dimensional atmosphere-canopy-soil interaction model is developed to estimate of the heat budget parameter in the atmospheric boundary layer. The canopy model is composed of the three balance equations of energy, temperature, moisture at ground surface and canopy layer with three independent variables of Tf(foliage temperature), Tg(ground temperature), and qg(ground specific humidity). The model was verilied by comparative study with OSUID(Oregon State University One Dimensional Model) proved in HAPEX-MOBILHY experiment. Also we applied this model in two dimensional land-sea breeze circulation. According to the results of this study, surface characteristics considering canopy acted importantly upon the simulation of meso-scale circulation. The factors which used in the numerical experiment are as follows ; the change for a sort of soil(sand and peat), the change for shielding factor, and the change for a kind of vegetation.

• 한국지열·수열에너지학회논문집
• /
• 제18권1호
• /
• pp.1-11
• /
• 2022

As abnormal climates occur due to the increase in greenhouse gases at home and abroad, various problems such as human casualties, crop damage, energy depletion, and economic loss due to heat diseases, which are one of the extreme climate phenomena, are following one after another. In response, the government has established the 'Climate Crisis Response Special Committee' since 2018, when it recorded the greatest damage in history due to heat waves, and has been carrying out budget formation and reform of laws and systems every year to respond to heat waves. However, in relation to the heat wave damage reduction facility that is being expanded with a large budget, there is no prior research related to the degree of heat loss due to the use of the facility, the difference in effects between specific groups, and the economic effect that comes back compared to the invested budget. Therefore, from a midto long-term perspective, it is expected that it will be difficult to establish a clear direction for policy making. Therefore, in this study, representative facilities were selected according to the principle of heat reduction among the currently expanded heat damage reduction facilities, and a questionnaire survey was conducted for users of each reduction facility (waterfall, awning, pond, and elastic pavement). Accordingly, the change in the sense of heat according to the use of the heat damage reduction facility was checked, and the change in the sense of heat according to the group characteristics (gender, age, metabolic rate) was analyzed to examine the characteristics of the relationship between the facility and the users.

• 한국환경과학회지
• /
• 제10권5호
• /
• pp.329-336
• /
• 2001

Characgcteristics of nocturnal boundary layer(NBL) were analyzed by the upper-air observations data using with the airsonde and pilot balloons from 1994 to 1999 in Kyungpook province. The automate weather boundary layer can become stably stratified when the surface is cooler than the air. Stable nocturnal boundary layer height were estimated from the top of surface stable layer where the vertical gradient of temperature and mixing ratio tend to zero or negative. The depth of the stable nocturnal boundary layer depended largely on the thermal effect rather than the wind effect at nighttime. The NBL was more developed on the land than on the coastal region. The stability index (bulk Richardson number) showed that the NBL was stable when the wind was weak and the vertical gradient of the temperature was strong. The heat budget in the NBL was studied by considering the effect of the radiative and the cooled by both the longwave radiative flux and the divergence of the heat flux, while NBL under the cloudy sky the longwave radiative flux played a role of the warming. It was noted that the heat was not conserved in both cases. To complete the heat budget in the NBL the warming/cooling by advection and subsidence must be considered.