• 대한원격탐사학회지
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• 제20권1호
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• pp.1-11
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• 2004

Based on surface energy balance climatology, surface temperatures should respond to drying conditions well before plant response. To test this hypothesis, land surface temperatures (LST) derived from MODIS data were analyzed to determine how the data were correlated with climatic water balance variables and NDVI anomalies during a growing season in Western and Central Kansas. Daily MODIS data were integrated into weekly composites so that each composite data set included the maximum temperature recorded at each pixel during each composite period. Time-integrated, or cumulative values of the LST deviation standardized with mean air temperatures had significantly high correlation coefficients with SM, AE/PE, and MD/PE, ranging from 0.65 to 0.89. The Standardized Thermal Index (STI) is proposed in this study to accomplish the objective. The STI, based on surface temperatures standardized with observed mean air temperatures, had significant temporal relationships with the hydroclimatological factors. STI classes in all the composite periods also had a strong correlation with NDVI declines during a drought episode. Results showed that, based on LST, air temperature observations, and water budget analysis, NDVI declines below normal could be predicted as early as 8 weeks in advance in this study area.

• 한국환경과학회지
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• 제28권2호
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• pp.277-285
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• 2019

Heat watch warning systems are operating in Korea and several other countries (China, the United Kingdom, France, the United States, Germany, Australia, and Japan). The heat wave indices used in this system are the heat index, perceived temperature, the wet bulb globe temperature, and the daily maximum temperature. To improve the heat wave advisory and warning system, some suggestions have been made. The meteorological-health index (i.e., indirect index), has especially been proposed in previous studies. This information should be provided not only to vulnerable groups (seniors, infants, and children), but also to outdoor workers who may be particularly exposed to heat waves. In addition, to have sufficient preemptive response times, the need for an extension of the heat watch warning period was suggested. Finally, the subdivision of administrative units and risk stages was proposed.

• 한국지리정보학회지
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• 제19권4호
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• pp.199-217
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• 2016

본 연구는 부산광역시 13개 기상관측지점을 대상으로 1997~2014년 동안의 기온상승율과 하강율의 계절적 특성이 연간 기온변화 특징에 미치는 영향을 분석하였다. 일별 기온 자료를 시계열적으로 단순화하기 위해 푸리에분석법을 적용하였는데, 이는 기상 자료와 같이 연속적으로 수집되는 시계열자료를 몇 개의 한정된 주요 파형으로 환원하여 자료를 단순화하는 수학적 기법이다. 부산광역시의 국지적 기온변화율은 대륙도에 의해 공간적으로 큰 영향을 받는 것으로 조사되었다. 계절적으로는 3월에 가장 높은 기온상승율(평균 $1.121^{\circ}C/month$)을 보였고, 11월에 가장 가파른 기온하강율(평균 -$1.564^{\circ}C/month$)을 나타냈다. 지역적으로 최난월인 8월 평균기온에 지배적인 영향을 주는 7월 평균기온상승율과 대륙도가 높은 지역일수록 최난일이 일찍 출현한 것으로 보아, 해양의 영향이 적은 지역일수록 기온상승률이 높고 해양 인접 지역에 비해 연중최고기온에 도달하는 시기가 앞당겨지는 것으로 분석되었다. 연구 지역 관측 지점 전체를 평균한 연도별 분석 결과도 7월 평균기온이 높은 해일수록 최난일 출현은 시기적으로 앞당겨지는 경향을 나타냈다. 도시화 정도를 나타내는 불투수면의 면적 비율 역시 기온의 연 변화와 통계적으로 상관관계를 갖는 것으로 나타났다. 관측지점의 불투수면 면적비율이 증가할수록 연평균기온이 높게 나타났고, 연평균 기온상승율과 하강율의 장기적 변동 폭도 크게 나타났다.

• 한국환경과학회지
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• 제26권5호
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• pp.621-638
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• 2017

Meteorological characteristics related to variations in ozone ($O_3$) concentrations in the Korean peninsula before, during, and after Typhoon Talas (1112) were analyzed using both observation data and numerical modeling. This case study takes into account a high $O_3$ episode (e.g., a daily maximum of ${\geq}90ppb$) without rainfall. Before the typhoon period, high $O_3$ concentrations in the study areas (e.g., Daejeon, Daegu, and Busan) resulted from the combined effects of stable atmospheric conditions with high temperature under a migratory anticyclone (including subsiding air), and wind convergence due to a change in direction caused by the typhoon. The $O_3$ concentrations during the typhoon period decreased around the study area due to very weak photochemical activity under increased cloud cover and active vertical dispersion under a low pressure system. However, the maximum $O_3$ concentrations during this period were somewhat high (similar to those in the normal period extraneous to the typhoon), possibly because of the relatively slow photochemical loss of $O_3$ by a $H_2O+O(^1D)$ reaction resulting from the low air temperature and low relative humidity. The lowest $O_3$ concentrations during the typhoon period were relatively high compared to the period before and after the typhoon, mainly due to the transport effect resulting from the strong nocturnal winds caused by the typhoon. In addition, the $O_3$ increase observed at night in Daegu and Busan was primarily caused by local wind conditions (e.g., mountain winds) and atmospheric stagnation in the wind convergence zone around inland mountains and valleys.

• Asian-Australasian Journal of Animal Sciences
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• 제22권3호
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• pp.416-420
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• 2009

An experiment of one-year duration was conducted on sixteen adult male German Angora rabbits under sub-temperate Himalayan conditions, to assess the effect of seasons on their body weight, wool production and quality, plane of nutrition and the digestibilities of nutrients. The daily meteorological attribute viz. minimum and maximum temperature; relative humidity and rainfall were recorded during winter (October to March), summer (April to June) and rainy (July to September) seasons. Biological parameters viz. body weight at the time of shearing, wool yield of individual rabbit, quality attributes of wool, fortnightly dry matter intake, chemical composition of feed and fodder and digestibilities of nutrients were recorded. Average minimum and maximum ambient temperature during winter, summer and rainy seasons were 4.6${\pm}$1.9 and 21.4${\pm}$2.8; 13.6${\pm}$2 and 30.3${\pm}$2; and 20.0${\pm}$1.4 and $31.0{\pm}1.8^{\circ}C$, respectively. The average relative humidity and total rainfall during winter, summer and rainy season were 69.5${\pm}$2.9% and 74.7${\pm}$21.8 mm; 58.6${\pm}$2.2% and 38.1${\pm}$18.1 mm; and 69${\pm}$4.2% and 104.0${\pm}$43.7 mm, respectively. The body weight of rabbits increased during all seasons, however, the maximum average daily weight gain of 3.47${\pm}$0.1 g was observed during the rainy season. The wool yield differed significantly (p$\leq$0.05) among different seasons with highest (140.4${\pm}$10 g) and lowest (108.5${\pm}$6.9 g) during winter and summer, respectively. The wool yield during the rainy season was 123.3${\pm}$5.2 g. The wool quality attributes revealed non-significant differences for staple length, fiber diameter, medulation percent, percent pure fibers and percent guard hairs. Plane of nutrition revealed significant (p$\leq$0.05) differences for concentrate intake. The concentrate intake was highest during winter (124.4${\pm}$2.6 g) followed by summer (86.8${\pm}$8.9 g) and rainy (80.7${\pm}$11.8 g) seasons. The reverse trend was observed in roughage intake with significantly (p${\leq}$0.05) lower intake during winter and highest during summer months. As a result total dry matter intake during different seasons was similar. Significant differences (p${\leq}$0.05) were observed for digestibilities of crude protein, crude fiber, ether extract, acid detergent fiber and cellulose. Digestibility of crude protein was highest during winter whereas the digestibilities of crude fiber, ether extract, acid detergent fiber and cellulose remained higher during the rainy season. During the winter season, the dry matter used for producing 100 g of wool was substantially lower than during other seasons and was concluded to be the best season for production of Angora wool under subtemperate Himalayan conditions.

• 한국약용작물학회지
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• 제28권6호
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• pp.463-470
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• 2020

Background: Evaluation of transpiration is required for agricultural and environmental management applications, as crop yields and plant growth are primarily water limited. This study aimed to determine the transpiration and carbon accumulation of Cnidium officinale. Methods and Results: The transpiration of C. officinale was evaluated using weighing lysimeter. The relationship between transpiration and factors such as solar radiation, air temperature, and leaf area was assessed. Transpiration increased as the leaf area increased with the growth stage. Furthermore, daily transpiration per unit leaf area was 0.69 ± 0.16 g·cm-2·day-1 and there were no significant differences in daily transpiration during the cultivation period. The maximum transpiration was 620.6 g m-2·h-1 and diurnal changes in transpiration were highly correlated with solar radiation although the maximum transpiration was observed at the air temperatures of 20℃ - 26℃. The ratio of carbon accumulation to transpiration was 0.12%. Conclusions: Our results indicated that the transpiration of C. officinale is primarily regulated by solar radiation energy on clear days and that 97% of the water is discharged through transpiration for heat dissipation. Therefore, weighing lysimeters can measure transpiration accurately and may be useful in interpreting plant growth.

• 대한지리학회지
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• 제50권1호
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• pp.1-21
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• 2015

본 연구에서는 지난 40년 동안(1973~2012)의 우리나라 기상청 산하 61개 지점 일기온 자료와 NCEP/NCAR 재분석 자료를 바탕으로 우리나라 지역별 겨울철 극한저온현상 발생 시 동아시아 영역의 종관 기후 패턴의 특징을 밝히고자 하였다. 일최고기온과 일최저기온 하위 10 퍼센타일 기준으로 정의된 겨울철 극한저온현상은 주로 겨울철 전반기(12월 초순~1월 중순)에 2~7일 간격으로 우리나라 전역 또는 주요 산맥 기준 동서지역으로 구분되어 발생함을 알 수 있다. 해수면기압과 바람벡터 등의 지상 종관 자료 합성장 분석에 따르면 총 13개로 구분되는 우리나라 겨울철 극한저온현상 발생 공간 패턴은 산맥뿐만 아니라 시베리아 고기압과 알류샨 저기압의 상대적인 확장 범위와 강도와 밀접한 관련성이 있음을 알 수 있다. 대류권 중층(500 hPa) 종관기후도 분석에 따르면, 블러킹 형태의 저기압이 상층 찬 공기를 고위도 지역에서 한반도로 이류시킬 때 우리나라에 겨울철 극한저온현상이 발생하기에 적합한 조건이 형성됨을 알 수 있다. 이러한 결과들은 지역규모 이상의 동아시아 겨울철 극한저온현상 예보를 향상시키기 위해 시베리아 고기압, 알류샨 저기압, 상층 블러킹 등의 종관 기후 요소를 모니터링하는 것이 중요함을 가리킨다.

• 대기
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• 제24권4호
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• pp.541-554
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• 2014

Historical, RCP4.5 and RCP8.5 scenarios from HadGEM2-AO are dynamically downscaled over the northeast East Asia with WRFV3.4. The horizontal resolution of the produced data is 12.5 km and the periods of integration are 1979~2010 for historical and 2019~2100 for both RCP4.5 and RCP8.5. We analyze the time series, climatology, EOF and extreme climate in terms of 2 m-temperature and precipitation during 30-year for the Historical (1981~2010) and RCP4.5 and RCP8.5 (2071~2100) scenarios. According to the result, the temperature of the northeast Asia centered at the Korean Peninsula increase 2.9 and $4.6^{\circ}C$ in the RCP4.5 and RCP8.5 scenarios, respectively, by the end of the 21st century. The temperature increases with latitude and the increase is larger in winter rather than in summer. The annual mean precipitation is expected to increase by about $0.3mm\;day^{-1}$ in RCP4.5 scenario and $0.5mm\;day^{-1}$ in RCP8.5 scenario. The EOF analysis is also performed for both temperature and precipitation. For temperature, the EOF $1^{st}$ modes of all scenarios in summer and winter show that temperature increase with latitude. The $2^{nd}$ mode of EOF of each scenario shows the natural variability, exclusive of the global warming. The summer precipitation over the Korean Peninsula projected increases in EOF $1^{st}$ modes of all scenarios. For extreme climate, the increment of the number of days with daily maximum temperature above $30^{\circ}C$ per year ($DAY_{TX30}$) is 25.3 and 49.7 days in RCP4.5 and RCP8.5 respectively over the Korean Peninsula. The number of days with daily precipitation above $20mm\;day^{-1}$ per year ($DAY_{PR20}$) also increases 3.1 and 3.5 days in RCP4.5 and RCP8.5 respectively.

• 한국환경복원기술학회지
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• 제24권6호
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• pp.109-119
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• 2021

Thermal environment of city is getting worse due to severe urban heat island caused by climate change and urbanization. Green roof improves the urban thermal environment and save the cooling energy in buildings. This study presented a green roof combined with a storage system that stores rain-water and supplies water through a wick and evaluated the temperature reduction effect as surface temperature and amount of evapotranspiration. For about a week, the surface temperature using a infrared thermal imager and the evapotranspiration by recording change of module weight were measured at intervals of 30 minutes from sunrise to sunset. The results show that the mean surface temperature of the green roof was 15.4 degrees lower than that of the non-green roof from 12:00 P.M. to 14:00 P.M. There was no significant difference between mean surface temperature of green roof with and without storage system immediately after rain, but more than a week after rain, there was a difference with average of 2.49 degrees and maximum of 4.72 degrees. The difference in daily amount of evapotranspiration was measured to be 1.66 times on average. As drought stress increased over time, the difference in daily amount of evapotranspiration and surface temperature between with/without storage system increased simultaneously. The results of the study show a more excellent cooling effect of green roof combined with the rainwater storage system.

• 환경생물
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• 제40권3호
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• pp.352-362
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• 2022

우리나라 동해와 남해 연안에 주로 분포하는 게바다말의 수온 상승에 따른 탄소수지 변화를 예측하기 위하여 5℃에서 30℃까지의 수온에서 5℃ 간격으로 광합성과 호흡률을 측정하였다. 광합성 매개변수 중 광합성 효율(α)을 제외한 최대광합성률(P_max)과 보상광도(I_c), 포화광도(I_k)가 수온이 상승함에 따라 증가하였으며, 호흡률(R) 또한 수온 상승에 따라 증가하였다. 가장 높은 수온(30℃)에서 P_max와 I_k는 급격히 감소하였으나, 반면에 I_c와 호흡률은 지속적으로 증가하였다. P_max :R ratio는 가장 높은 수온(30℃)에서 최소값을, 가장 낮은 수온(5℃)에서 최대값을 보였다. 이러한 결과를 토대로 게바다말이 양의 탄소수지를 유지하기 위해 필요한 일일 포화광도 시간(H_sat)을 계산한 결과, 5℃에서는 2.50시간 이상, 30℃에서는 10.61시간 이상이 요구되어, 수온이 상승할수록 더 많은 시간의 포화광도(H_sat)가 요구되는 것으로 나타났다. 따라서 수온이 꾸준히 상승되어 여름철 고수온이 장기간 지속되면 우리 연안 게바다말 생육지의 분포에 부정적인 영향을 미칠 것으로 판단되었다.