• 제목/요약/키워드: Minimum Temperature

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제주지역 기온과 강수량의 기후 변동 특성 (Climatological Variability of Temperature and Precipitation in Jeju)

  • 김성수;장승민;백희정;최흥연;권원태
    • 한국지구과학회지
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    • 제27권2호
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    • pp.188-197
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    • 2006
  • 1924년부터 2004년까지 제주관측지점 자료를 이용하여 제주의 기온과 강수량의 변동 특성을 조사하였다. 지난 81년 동안 연평균 기온은 $0.02^{\circ}C/year$ 정도로 증가하였으며 1980년 이후에는 $0.05^{\circ}C/year$로 이전보다 큰 폭으로 증가하였다. 최저기온의 증가가 최고기온 증가보다 크게 나타나 결과적으로 최저기온의 상승이 평균기온의 상승을 유발한 것으로 보인다. 기온과 강수의 특이기후 발생빈도 또한 조사하였다. 최고기온 특이값 빈도에 대한 기온편차는 지구온난화경향과 더불어 1980년대에 증가하였으며, 최저기온 특이값은 여름과 겨울 동안 감소하는 것으로 나타났다. 강수일수는 감소하고 일강수량이 80 mm 이상인 호우일수의 빈도는 증가하여 강수강도가 강화되는 것으로 나타났다.

PRISM과 GEV 방법을 활용한 30 m 해상도의 격자형 기온 극값 추정 방법 연구 (A Study on the Method for Estimating the 30 m-Resolution Daily Temperature Extreme Value Using PRISM and GEV Method)

  • 이준리;안중배;정하규
    • 대기
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    • 제26권4호
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    • pp.697-709
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    • 2016
  • This study estimates and evaluates the extreme value of 30 m-resolution daily maximum and minimum temperatures over South Korea, using inverse distance weighting (IDW), parameter-elevation regression on independent slopes model (PRISM) and generalized extreme value (GEV) method. The three experiments are designed and performed to find the optimal estimation strategy to obtain extreme value. First experiment (EXP1) applies GEV firstly to automated surface observing system (ASOS) to estimate extreme value and then applies IDW to produce high-resolution extreme values. Second experiment (EXP2) is same as EXP1, but using PRISM to make the high-resolution extreme value instead of IDW. Third experiment (EXP3) firstly applies PRISM to ASOS to produce the high-resolution temperature field, and then applies GEV method to make high resolution extreme value data. By comparing these 3 experiments with extreme values obtained from observation data, we find that EXP3 shows the best performance to estimate extreme values of maximum and minimum temperatures, followed by EXP1 and EXP2. It is revealed that EXP1 and EXP2 have a limitation to estimate the extreme value at each grid point correctly because the extreme values of these experiments with 30 m-resolution are calculated from only 60 extreme values obtained from ASOS. On the other hand, the extreme value of EXP3 is similar to observation compared to others, since EXP3 produces 30m-resolution daily temperature through PRISM, and then applies GEV to that result at each grid point. This result indicates that the quality of statistically produced high-resolution extreme values which are estimated from observation data is different depending on the combination and procedure order of statistical methods.

수도권지역 미래 도시성장에 따른 기온변화 추정 (Estimation of Air Temperature Changes due to Future Urban Growth in the Seoul Metropolitan Area)

  • 김유근;김현수;정주희;송상근
    • 한국환경과학회지
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    • 제19권2호
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    • pp.237-245
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    • 2010
  • The relationship between air temperatures and the fraction of urban areas (FUA) and their linear regression equation were estimated using land-use data provided by the water management information system (WAMIS) and air temperatures by the Korea Meteorology Administration (KMA) in the Seoul metropolitan area (SMA) during 1975 through 2000. The future FUA in the SMA (from 2000 to 2030) was also predicted by the urban growth model (i.e., SLEUTH) in conjunction with several dataset (e.g., urban, roads, etc.) in the WAMIS. The estimated future FUA was then used as input data for the linear regression equation to estimate an annual mean minimum air temperature in the future (e.g., 2025 and 2030). The FUA in the SMA in 2000 simulated by the SLEUTH showed good agreement with the observations (a high accuracy (73%) between them). The urban growth in the SMA was predicted to increase by 16% of the total areas in 2025 and by 24% in 2030. From the linear regression equation, the annual mean minimum air temperature in the SMA increased about $0.02^{\circ}C$/yr and it was expected to increase up to $8.3^{\circ}C$ in 2025 and $8.7^{\circ}C$ in 2030.

n-Propanol과 Formic acid계의 최소자연발화온도의 측정 (Measurement of Autoignition Temperature of n-Propanol and Formic acid System)

  • 조영세;하동명
    • 한국화재소방학회논문지
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    • 제27권5호
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    • pp.64-69
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    • 2013
  • 가연성 혼합물의 최소자연발화온도는 가연성액체의 안전한 취급을 위해서 중요한 지표가 된다. 본 연구에서는 ASTM E659 장치를 이용하여 가연성 혼합물인 n-Propanol과 Formic acid 계의 최소자연발화온도와 발화지연시간을 측정하였다. 2성분계를 구성하는 순수물질인 n-Propanol과 Formic acid의 최소자연발화온도는 각 각 $435^{\circ}C$$498^{\circ}C$로 측정되었다. 그리고 측정된 n-Propanol과 Formic acid 계의 최소자연발화온도는 제시된 식에 의한 예측값과 작은 평균절대오차에서 일치하였다. 그리고 n-Propanol과 Formic acid 계는 일부 혼합 조성에서 두 개의 순수물질 가운데 낮은 AIT보다 낮게 측정된 최소자연발화온도거동(MAITB, Minimum Autoignition Temperature Behavior)을 보이고 있다.

일 최저 기온을 이용한 한국의 폭염사상 추세 (Trend of heat wave events in South Korea using daily minimum air temperature)

  • 김령은;원정은;이정민;최정현;김상단
    • 한국습지학회지
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    • 제21권4호
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    • pp.344-353
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    • 2019
  • 폭염은 전 세계에서 나타나고 있는 현상으로 열 노출과 관련된 위험을 악화시키고, 치명적인 인명피해를 초래한다. 본 연구에서는 폭염의 한 가지 형태 중 하나인 열대야를 대상으로 한국의 열대야 추세가 어떻게 변화하고 있는 지를 살펴보았다. 1973년부터 2018년까지 한국 기상청 ASOS 60개 지점의 일 최저 기온을 이용하여 여섯 개의 열대야 특성의 시간적인 변화를 분석하였다. 이러한 분석으로부터 열대야 관심지역은 인천, 강릉, 청주, 전주, 광주, 장흥, 여수, 거제, 구미, 영덕 등 10개 지역, 열대야 우심지역은 홍천, 양평, 수원, 원주, 보령, 대전, 부안, 정읍, 목포, 거창, 밀양, 포항, 제주, 서귀포 등 14개 지역이 식별되었다. 제안된 열대야 우심지역에는 특별한 열대야 대책이 수립될 필요가 있을 것이다.

온도에 따른 사질토의 다짐 특성 (Temperature Effect on the Compaction Characteristic of Cohesionless Soil)

  • 이기철;지수빈;김호비;김동욱
    • 한국지반공학회논문집
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    • 제32권2호
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    • pp.53-62
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    • 2016
  • 흙의 다짐 특성에 영향을 주는 주요인자 중 하나인 온도는 지역과 계절에 따라 다양하게 변화하는 특성을 가진다. 최근 동토지방에서 많은 토목공사가 시행되고 있지만, 온도와 관련된 흙의 다짐기준 및 지침을 정량화할 수 있는 문헌은 미비한 실정이다. 따라서 본 연구는 온도에 따른 흙의 다짐특성을 시험을 통해 평가하고자 하였다. 시험을 위해 러시아 시베리아, 캐나다 앨버타 주 오일 샌드 지역 등에서 자주 쓰이는 성토재료인 모래의 온도별 다짐특성을 나타낼 수 있는 주문진 모래를 사용하였으며, 표준다짐시험을 흙의 다양한 온도조건($-10^{\circ}C$에서 $17^{\circ}C$)에서 수행하였다. 시험 결과 영상 온도에서는 다짐 시 벌킹 효과로 인해 흙 공시체의 부피 팽창이 발생하였으며, 그 범위는 0%~6%이였다. $0^{\circ}C$에서 $17^{\circ}C$까지 온도가 증가하면서 최대 부피(최소 건조단위중량)에 해당하는 함수비는 감소하였고, 최소 부피(최대 건조단위중량)에 해당하는 함수비는 온도가 증가함에 따라 약간 증가하였다. 영하 온도의 경우 함수비가 추가됨에 따라 건조단위중량은 지속적으로 감소하였다. 영하 온도에서는 벌킹이 발생하지 않았으며 물의 단위부피보다 얼음의 단위부피가 더 크기 때문에 흙 공시체의 부피가 증가하였다.

The Optimum Condition of Anisotropic Bulk(10) Si Etching with KOH for High Selectivity and Low Surface Roughness

  • Lim, Hyung-Teak;Kim, Yong-Kweon;Lee, Seung-Ki
    • Journal of Electrical Engineering and information Science
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    • 제2권5호
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    • pp.108-113
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    • 1997
  • In this paper, the optimum condition of (110) Si etching with the potassium hydroxide(KOH) etchant is presented. Although several researches on (110) Si anisotropic etching have been studied, there has been lack of effects of mask quality and etching conditions on the selectivity and the roughness o the etched surface. Three kinds of masks (film, emulsion and E-beam mask) were used in order to verify the effect of etching properties. Anisotropic bulk etching depends on the crystalline orientation and the concentration and temperature of the etchant. In order to investigate the effect of etching conditions on selectivity and the roughness of the etched surface, the concentration of the etchant was varied from 35 to 45 per cent in weight with increments by 5 per cent and the temperature was changed from 70 to 90$^{\circ}C$ with increments by 10$^{\circ}C$. The combination of the temperature of 70$^{\circ}C$ and the concentration of 40wt.% was found to be the optimum etching condition for high selectivity. Etched surfaces show minimum surfaces show minimum surface roughness at a temperature of 80$^{\circ}C$ and a concentation of 40wt.%. Comb structures with various comb widths were fabricated and the lengths of the combs wree measured with several etching time durations. A micro comb structure 525$\mu\textrm{m}$ high was fabricated for MEMS application.

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Variation of Hydro-Meteorological Variables in Korea

  • Nkomozepi, Temba;Chung, Sang-Ok;Kim, Hyun-Ki
    • Current Research on Agriculture and Life Sciences
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    • 제32권3호
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    • pp.135-143
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    • 2014
  • The variability and temporal trends of the annual and seasonal minimum and maximum temperature, rainfall, relative humidity, wind speed, sunshine hours, and runoff were analyzed for 5 major rivers in Korea from 1960 to 2010. A simple regression and non-parametric methods (Mann-Kendall test and Sen's estimator) were used in this study. The analysis results show that the minimum temperature ($T_{min}$) had a higher increasing trend than the maximum temperature ($T_{max}$), and the average temperature increased by about $0.03^{\circ}C\;yr.^{-1}$. The relative humidity and wind speed decreased by $0.02%\;yr^{-1}$ and $0.01m\;s^{-1}yr^{-1}$, respectively. With the exception of the Han River basin, the regression analysis and Mann-Kendall and Sen results failed to detect trends for the runoff and rainfall over the study period. Rapid land use changes were linked to the increase in the runoff in the Han River basin. The sensitivity of the evapotranspiration and ultimately the runoff to the meteorological variables was in the order of relative humidity > sunshine duration > wind speed > $T_{max}$ > $T_{min}$. Future studies should investigate the interaction of the variables analyzed herein, and their relative contributions to the runoff trends.

1904년 이래의 부산 기후 변동성 및 생활기상지수들의 기후변화 특성 연구 (A Study on Characteristics of Climate Variability and Changes in Weather Indexes in Busan Since 1904)

  • 전하은;하경자;김혜렴
    • 대기
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    • 제33권1호
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    • pp.1-20
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    • 2023
  • Holding the longest observation data from April 1904, Busan is one of the essential points to understand the climate variability of the Korean Peninsula without missing data since implementing the modern weather observation of the South Korea. Busan is featured by coastal areas and affected by various climate factors and fluctuations. This study aims to investigate climate variability and changes in climatic variables, extremes, and several weather indexes. The statistically significant change points in daily mean rainfall intensity and temperature were found in 1964 and 1965. Based on the change point detection, 117 years were divided into two periods for daily mean rainfall intensity and temperature, respectively. In the long-term temperature analysis of Busan, the increasing trend of the daily maximum temperature during the period of 1965~2021 was larger than the daily mean temperature and the daily minimum temperature. Applying Ensemble Empirical Mode Decomposition, daily maximum temperature is largely affected by the decadal variability compared to the daily mean and minimum temperature. In addition, the trend of daily precipitation intensity from 1964~2021 shows a value of about 0.50 mm day-1, suggesting that the rainfall intensity has increased compared to the preceding period. The results in extremes analysis demonstrate that return values of both extreme temperatures and precipitation show higher values in the latter than in the former period, indicating that the intensity of the current extreme phenomenon increases. For Wet-Bulb Globe Temperature (effective humidity), increasing (decreasing) trend is significant in Busan with the second (third)-largest change among four stations.

Normalized Cross-Correlations of Solar Cycle and Physical Characteristics of Cloud

  • Chang, Heon-Young
    • Journal of Astronomy and Space Sciences
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    • 제36권4호
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    • pp.225-234
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    • 2019
  • We explore the associations between the total sunspot area, solar north-south asymmetry, and Southern Oscillation Index and the physical characteristics of clouds by calculating normalized cross-correlations, motivated by the idea that the galactic cosmic ray influx modulated by solar activity may cause changes in cloud coverage, and in turn the Earth's climate. Unlike previous studies based on the relative difference, we have employed cloud data as a whole time-series without detrending. We found that the coverage of high-level and low-level cloud is at a maximum when the solar north-south asymmetry is close to the minimum, and one or two years after the solar north-south asymmetry is at a maximum, respectively. The global surface air temperature is at a maximum five years after the solar north-south asymmetry is at a maximum, and the optical depth is at a minimum when the solar north-south asymmetry is at a maximum. We also found that during the descending period of solar activity, the coverage of low-level cloud is at a maximum, and global surface air temperature and cloud optical depth are at a minimum, and that the total column water vapor is at a maximum one or two years after the solar maximum.