• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume II
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• pp.1027-1030
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• 2006

Development of diurnal warming in the open Okhotsk Sea during the daytime and calm conditions was studied using sea surface temperature (SST) fields retrieved from NOAA AVHRR, Terra and Aqua MODIS, Aqua AMSR-E and ADEOS-II AMSR data. Sea surface wind fields were estimated from AMSR-E/AMSR measurements as well as were obtained from QuikSCAT scatterometer. Weak winds and cloudless conditions were observed in the central area of anticyclone, which moved slowly on 28-30 June 2003 east off Sakhalin. The area where the amplitude of the diurnal SST signal ${\Delta}T$ was significant also shifted slowly and had or circular or elongated shape. The ${\Delta}T$ was estimated relative to the SST values in the areas surrounding the centre of anticyclone where wind speed W exceeded 5- 6 m/s. The diurnal variations of SST, day-night differences were computed using NOAA-12 and NOAA-16 AVHRRderived data. Analysis of simultaneous SST and W fields showed that the increase of W from 0 to 5-6 m/s causes the decrease of ${\Delta}T$ to zero. Maximum warming exceeded $8^{\circ}C$ and was observed in the centre of anticyclone where W = 0 m/s. So strong heating was likely due to the increased chlorophyll a concentration in the area under study that follows from analysis of satellite ocean colour data.

• 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.

• Environmental Engineering Research
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• 제25권2호
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• pp.147-162
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• 2020

The main objective of this study is to estimate the levels of pollution to which the community is presently exposed and to model the regimes of local air quality. Diurnal, daily, and monthly variations of NO, NO₂, SO₂, and O₃ were thoroughly investigated in three areas; namely, residential, industrial, and terminal in Ras Al-Khafji. There is obvious diurnal variation in the concentration of these pollutants that clearly follows the diurnal variation of atmospheric temperature and main anthropogenic and industrial activities. Correlation analysis showed that meteorological conditions play a vital role in shaping the pattern and transportation of air pollutants and photochemical processes affecting O₃ formation and destruction. Bivariate polar plots, an effective graphical tool that utilizes air pollutant concentrations' dependence on wind speed and wind direction, were used to identify prevailing emission sources. Non-buoyant ground-level sources like domestic heating and street transport emissions, various industrial stacks, and airport-related activities were considered dominant emission sources in observatory sites. This study offers valuable and detailed information on the status of air quality, which has considerable, quantifiable, and important public health benefits.

• 보존과학연구
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• 통권24호
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• pp.169-184
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• 2003

Yearly mean temperature and relative-humidity of the Seokguram Grotto was measured $19~23^{\circ}C$, 40~44% from May, 1998 to December,2002. The measurement has little differences comparing to the optimum guideline (temperature : $20^{\circ}\pm2^{\circ}C$, relative-humidity : $50^{\circ}\pm5%$). It is necessary to increase humidity in the Seokguram Grotto during winter because of heating and decrease the temperature during summer because of a higher temperature of outside. In addition, the diurnal range keep in $4^{\circ}C$ of temperature and in 10% of relative-humidity. Yearly mean concentration of $CO_2$(carbon dioxide) was measured538~658ppm that is higher than concentration of normal atmosphere(360 ppm). The $CO_2$ has an cumulative effect on the surface of stone cultural properties as a form of carbonic acid($H_2CO_3$) after reaction with water. HVAC (Heating, Ventilation and Air Conditioning) system should be operated to maintain ideal state for the preservation according to the optimum guideline. Also, the entrance into the Seokguram Grotto should be controlled to prevent a sudden fluctuation of humidity and temperature. Human could carry small particles like a microdust, microbe, etc., into the Seokguram Grotto and also could damage the surface by a direct touch.

• 지역연구
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• 제40권2호
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• pp.107-130
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• 2024

도시의 지표면 기온 변화는 도시민의 열 쾌적성, 에너지 소비, 나아가 건강에 영향을 미치는 주요한 환경요인이다. 많은 연구가 도시 지표면 기온과 도시 건조환경(built-environment) 형태 간의 관계를 탐색해 왔으나 대부분 극궤도위성 자료를 사용해 정오 시간대 기온만을 분석하였다. 본 연구는 다양한 시간대 지표면 기온을 관측하는 ECOSTRESS 위성 자료를 활용하여 서울시 여름철 지표면 기온의 주간 변동을 탐색하였으며 기온 변동이 건조환경 유형별로 차별적으로 나타나는지 분석하였다. ECOSTRESS는 2018년 발사된 NASA 위성으로 점진 변화 궤도를 운항하며 다양한 시간대 지표면 온도를 70m 고해상도로 관찰한다. 본 연구는 2019~2022년 이른 오전(6:25AM)과 늦은 오후(5:26PM)에 걸친 자료를 수집하여 서울시 지표면 온도의 시계열 자료를 구축하였다. 환경 특성을 반영하는 녹지, 수면, 건축 형태(건폐율, 용적률, 높이) 데이터를 기반으로 계층적 군집분석을 실시해 8가지 건조환경 유형을 도출하였으며, 유형별 온도변동 특성을 비교하였다. 각 유형은 저층고밀거주지(low-rise compact), 저밀아파트단지(low-BCR Apt.), 강변 중고층 주거단지(Riverside Mid-rise Apt.), 중고층 용도혼합지역(mid-to-high-rise mixed use), 고층고밀지역(high-rise compact), 초고층빌딩(skyscrapers), 산림, 수면(하천)을 나타내었다. 분석 결과, 지표 기온의 공간적 격차는 새벽 이후 증가하여 정오(12:04)에 극대화된 뒤 다시 감소하였으며, 기온 변화가 급격한 지역과 안정적인 지역이 구분되었다. 저층 고밀 거주지와 고층 고밀지역의 경우 기온이 빠르고 높게 증가하여 기온변동성이 높았고, 저밀 아파트단지는 기온이 온화하고 완만하게 증가하며 기온 변동성이 낮았다. 건조환경 유형 간 평균기온의 서열은 시간별로 변화하지 않고 유지되었다. 이러한 결과는 폭염과 일교차 증가에 적응할 수 있는 도시형태에 시사점을 제공한다.

• International Union of Geodesy and Geophysics Korean Journal of Geophysical Research
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• 제24권1호
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• pp.29-45
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• 1996

Before (March 26, 1994) or after the occurrence of a downslope windstorm (March 29), the NO, $NO_2$, and $SO_2$ at the ground level of Kangnung city were monitored with high concentrations in the afternoon, due to a large amount of gases emitted from combustion of motor vehicle and heating apparatus, especially near 1600-1800 LST and 2000-2100 LST, but at night, they had low concentrations, resulting from small consumptions of vehicle and heating fuels. When both moderate westerly synoptic-scale winds flow over Mt. Taegwallyang and easterly meso-scale sea breeze during the day, atmospheric pollutants should be trapped by two different wind systems, resulting in higher concentration at Kangnung city in the afternoon. At night, the association of westerly synoptic wind and land breeze can produce relatively strong winds and the dissipation by the winds cause these low concentrations to lower and lower, as nightime goes on. From March 27 through 28, an enforced localized windstorm could be produced along the lee side of the mountain near Kangnung, generating westerly internal gravity waves with hydraulic jump motions. Sea breeze toward inland appartantly confines to the bottom of the eastern side of the mountain, due to the interruption of eastward violent internal gravity waves. As the windstorm moves down toward the ground, an encountering point of two opposite winds approaches Kangnung, and a great amount of NO and $NO_2$ were removed by the strong surface winds. Thus, their maximum concentrations are found to be near 18 and 20 LST, 17 and 21 LST. In the nighttime, the more developed storm should produce very strong surface winds and the NO and $NO_2$ could be easily dissipated into other place. The $SO_2$ concentration had no maximum value, that is, almost constant one all day long, due to its removal by the strong surface winds. Especially, the CO concentrations were slightly lower during the strom period than both before or after the strom, but they were nearly constant without much changes during the during the daytime and nighttime.

• Wind and Structures
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• 제24권6호
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• pp.565-578
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• 2017

The meteorological model WRF is used to investigate the wind circulation in Valle Camonica, Italy, an alpine valley that includes a large subalpine lake. The aim was to obtain the information necessary to evaluate the wind potential of this area and, from a methodological point of view, to suggest how numerical modeling can be used to locate the most interesting spots for wind exploitation. Two simulations are carried out in order to analyze typical scenarios occurring in the valley. In the first one, the diurnal cycle of thermally-induced winds generated by the heating-cooling of the mountain range encircling the valley is analyzed. The results show that the mountain slopes strongly affect the low-level winds during both daytime and nighttime, and that the correct setting of the lake temperature improves the quality of the meteorological fields provided by WRF significantly. The second simulation deals with an event of strong downslope winds caused by the passage of a cold front. Comparisons between simulated and measured wind speed, direction and air temperature are also shown.

• 해양환경안전학회지
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• 제18권6호
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• pp.514-519
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• 2012

전라남도 완도 연안 해역은 전복양식이 중요하고 최근 해상가두리 양식이 보편화되어 전복사육과 폐사에 중요한 수온의 변동을 이해할 필요가 있다. 완도해역에 위치한 신지도, 청산도의 2005년부터 2009년까지 연속자동관측 수온자료를 이용하여 완도 양식장 해역의 수온 변동 특성을 분석하였다. 연안에 가까운 신지도의 연간 수온변동 범위와 수온증가율이 청산도에 비해 크게 나타났으며, 수심이 낮은 연안 해역에서 하계 태양복사열에 의한 가열과 동계의 냉각에 기인한 것으로 판단된다. 또한 추계의 수온 감소율이 춘계의 상승률보다 컸고, 하계에 조석 주기의 단주기 수온변동이 뚜렷하게 나타났다. 급격한 수온변화에 해당하는 큰 수온일교차는 청산도에서 크게 나타났다. 수온 자료로 판단한 전복양식장은 외해에 위치한 청산도가 연안보다 더 적절한 해역으로 판단된다.

• 생물환경조절학회지
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• 제6권4호
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• pp.235-241
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• 1997

거봉과 같은 대립계 4배체 포도의 근역제한 재배에서 품질향상과 수량을 증대시키려면 포도수체 지상부의 기온과 상대습도 뿐만 아니라 근권부의 지온과 토양수분을 적정하게 관리하는 것이 중요하다. 거봉의 2기작을 위한 근역 제한 재배에서 지중가온과 토양수분을 조절하면서 근권부의 지온과 토양수분 홉인합의 변화 특성을 살펴보고자 시도된 본 연구에서 나타난 결과를 요약하면 다음과 같다. 1. 가온 시기에 주간의 최고 기온과 야간 기온의 평균치는 각각 25.1~32.7$^{\circ}C$, 18$^{\circ}C$ 이고, 상대습도는 주간 최저치와 야간 최고치가 각각 50~55%, 84~87%로 나타났다. 2. 지중 15cm 깊이에서 지중 가온구와 지중 무가온구 지온의 평균치는 각각 25.6$^{\circ}C$, 17.4$^{\circ}C$로서 지온의 적정 범위에 해당되어 본 실험에서 적용된 온수보일러에 의한 지중 가온이 효과적인 것으로 나타났다. 3. 15cm 깊이에서 토양수분 흡인압의 목표치를 pF 2.2로 설정하였을 때 관수 개시와 함께 15cm 깊이에서의 흡인압은 pF 1.5 정도까지 하강하였으나, 이후에는 흡인압이 상승하면서 pF 2.0~2.2를 유지하여 토양수분 흡인압의 조절이 효과적으로 이루어졌다. 그러므로 근역 제한 재배에서 관수 개시점을 결정하기 위한 지표로서 지중 15cm 깊이에서 측정된 토양수분 홉인압을 이용하는 것이 바람직하다. 4. 거봉의 근역 제한 재배에서 신초의 도장을 방지하려면 근권부의 효과적인 배수 대책이 요구된다.

• 한국환경과학회지
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• 제18권5호
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• pp.489-499
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• 2009

In an effort to examine the Regional Atmospheric Modeling System (RAMS ver. 4.3) to the initial meteorological input data, detailed observational data of NOAA satellite SST (Sea Surface Temperature) was employed. The NOAA satellite SST which is currently provided daily as a seven-day mean value with resolution of 0.1 $^{\circ}$ grid spacing was used instead of the climatologically derived monthly mean SST using in RAMS. In addition, the RAMS SST data must be changed new one because it was constructed in 1993. For more realistic initial meteorological fields, the NOAA satellite SST was incorporated into the RAMS-preprocess package named ISentropic Analysis package (ISAN). When the NOAA SST data was imposed to the initial condition of prognostic RAMS model, the resultant performance of near surface atmospheric fields was discussed and compared with that of default option of SST. We got the good results that the new SST data was made in a standard RAMS format and showed the detailed variation of SST. As the modeling grid became smaller, the SST differences of the NOAA SST run and the RAMS SST43 (default) run in diurnal variation were very minor but this research can apply to further study for the realistic SST situation and the development in predicting regional atmospheric field which imply the regional circulation due to differential surface heating between sea and land or climatological phenomenon.