• 제목/요약/키워드: Annual mean minimum air temperature

검색결과 15건 처리시간 0.022초

감 재배지 간 과실 품질 차이에 관계한 기온요인 분석 (Analysis of Air Temperature Factors Related to Difference of Fruit Characteristics According to Cultivating Areas of Persimmon (Diospyros kaki Thunb.))

  • 김호철;전경수;김태춘
    • 생물환경조절학회지
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    • 제17권2호
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    • pp.124-131
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    • 2008
  • 본 연구에서는 감 재배지 간 과실 특성 차이에 관계한 기온 요인을 분석하고자 8개 단감 '부유' 재배지의 16개 기온요인과 과실 특성을 조사하여 주성분 및 다중회귀 분석을 실시하였다. 16개 기온요인 중 제1주성분은 12개 요인으로 이중 연 평균최저기온, 10월 평균기온, 연 평균최저극온, 생육기 평균기온의 영향력이 아주 높았다. 그리고 제2주성분은 4개 요인으로 4월에서 7월까지의 월 평균기온이었고 5월과 6월 평균기온의 영향력이 높았다. 이에 제2주성분까지 누적기여율은 91.4%로 재배지 간 기온 차이에 관여하는 기온 요인을 분석하는 데에는 충분하였다. 8개 재배지 중 5 재배지은 주요 기온요인이나 그 영향력에서 뚜렷한 차이를 나타내었다. 기온요인과 과실 특성 간 다중회귀분석에서 과고는 생육기 평균기온($X_8$) 겨울철 적산온도($X_6$) 영향을 뚜렷이 받으며 회귀식 $Y=150.55-5.375X_8+0.014X_6$을 나타내었고, 이 회귀식에 대하여 생육기 평균최저기온($X_9$), 적산온도($X_5$), 8월 평균기온($X_{12}$) 등이 영향을 주었다. 과경은 생육기 평균기온($X_8$, 부의 상관), 과육갈반정도는 생육기 평균최저기온($X_9$, 정의 상관), 과피색 $a^*$값은 연 평균최저기온($X_2$, 정의 상관)의 영향을 받는 것으로 나타났다.

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.

제주도 감귤 재배지역에 대한 환경특성의 정량화 (Quantification of Environmental Characteristics on Citrus Production Area of Jeju Island in Korea)

  • 문경환;손인창;송은영;오순자;박교선;현해남
    • 한국농림기상학회지
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    • 제17권1호
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    • pp.69-74
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    • 2015
  • 제주지역에서 재배되고 있는 감귤류의 일종인 온주밀감을 대상으로 지형, 기후 등 현재의 재배환경을 공간기술을 이용하여 정량화하여 환경특성 범위를 분석하고, 앞으로 기후변화에 대비하여 온주밀감의 재배가 가능한 지역을 판단할 수 있는 환경 기준을 도출하고자 하였다. 해발고도, 경사도, 경사향, 연평균기온, 1월 평균기온, 일최저기온의 극 값, $-5^{\circ}C$ 이하 일수, 강수량 등 8종의 기후요소에 대하여 지리정보시스템(GIS) 기술을 이용하여 분포지도의 형태로 제작하였고, 이 분포도에서 감귤원이 분포하는 지역에 포함되는 격자 값을 추출하여 환경요소의 분포를 분석할 수 있었다. 온주밀감의 재배 가능 여부를 판단할 수 있도록 $14.5^{\circ}C$ 이상의 연평균기온, $-10.0^{\circ}C$ 이상의 일 최저기온의 극 값, 연중 $-5^{\circ}C$ 이하 저온일수가 5일 이상일 것 등 3 가지 기후학적 환경요소에 대한 기준을 설정하였다.

한국 남부지방 난온대성 상록활엽수의 동해피해 -전라남도 광양시 중마동의 후박나무를 중심으로- (Freezing Injury of Evergreen Broad-Leaved Trees in Warm-Temperature in the Southern Region in Korea -A Case of Machilus Thunbergii Siebold & Zucc. on the Jungma-dong, Gwangyang-city, Jeollanam Province-)

  • 이기원;김도균
    • 한국환경복원기술학회지
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    • 제20권1호
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    • pp.77-96
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    • 2017
  • This study was carried out to clarify the climatic factors of the freezing injury for the judgement on the adaptation areas of evergreen broad-leaved trees. We surveyed and analyzed the climatic factors of the freezing injury to Machilus thunbergii Siebold & Zucc. on the streets with the analyzation of planting grounds, soil conditions and the surrounding buildings. This study showed that only the minimum air temperature factor out of the other climate elements, which were the annual precipitation; the average annual temperature; the average monthly temperature of january; the average monthly minimum temperature of January; the average temperature of the coldest month; the warmth index and the coldness index, was matched up with the previous theories and reports on the freezing damages on the evergreen broad leaved trees and Machilus thunbergii Siebold & Zucc. The freezing injury of Machilus thunbergii Siebold & Zucc was occurred when the mean minimum temperature of the coldest month(TMC) in winter season fell down below $-4.1^{\circ}C$ and the temperature fell down below $-9.2^{\circ}C$. The freezing damage on Machilus thunbergii Siebold & Zucc surrounded by high buildings were less than those surrounded by low buildings or at non buildings.

한국 근해 수온의 주기적 변화(I) 남해의 거문도해역 표면수온 년주변화 및 영년변화 (Periodic Variations of Water Temperature in the Seas Around Korea(I) Annual and Secular Variations of Surface Water Temperature, Kumun-Do Region, Southern Sea of Korea)

  • 한상복
    • 한국해양학회지
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    • 제5권1호
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    • pp.6-13
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    • 1970
  • Ten days and monthly mean temperatures were analysed daily data observed during July, 1916 to March, 1970 statistically. Periodic characters were calculated by Δn, new method of approximate solution of Schuster Method. According to ten days mean temperatures, annual variation function is F($\theta_d$)=16.29-5.27 cos $\theta_d$+0.75 cos2 $\theta_d$-3.14 sin $\theta_d$+1.16 sin2 $\theta_d$-0.63 sin $\3{theta}_d$, where $\theta_d$=$-\frac{\pi}{18}$(d-3), d is the order of ten days period, 1 to 36. Annual mean water temperature is 16.3$^{\circ}C$, minimum in the last ten days of February 10.9$^{\circ}C$, maximum in the last ten days of August 24.5$^{\circ}C$. Periodic character of secular variation shows 11 year and its curve is F($\theta_y$)=16.29+0.53 cos $\theta_y$ -0.16cos $2{\theta}_y$+0.10 cos$3{\theta}_y$-0.10 sin $\theta_y$, where $\theta_y$=2$-\frac{2\pi}{11}$(y-1920), y is calendar year. And the relation between air temperature x and water temprature y is following. y=9.67 1.035$\^x$

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2006년 동해안 감포의 열수지 (Heat Budget at Gampo in the Eastern Coast of Korea in 2006)

  • 최용규;한인성;서영상;고우진;김상우
    • 한국환경과학회지
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    • 제18권1호
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    • pp.33-39
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    • 2009
  • Based on the monthly weather report of Korea Meteorological Administration (KMA) and daily sea surface temperature (SST) data from National Fisheries Research and Development Institute (NFRDI) in 2006, heat budget was estimated at Gampo in the eastern coast of Korea, the region occuring the cold water known as upwelling in summer. Net heat flux was transported from the air to the sea surface during February to November, and it amounts to $345Wm^{-2}$ in monthly mean value. During December to January, the transfer of net heat flux was conversed from the sea surface to the air with $-56Wm^{-2}$ in minimum of monthly mean value in January. Long wave radiation was ranged from $6Wm^{-2}\;to\;106Wm^{-2}$. Sensible heat was varied from $-36Wm^{-2}$(June) to $61Wm^{-2}$(February) and showed negative values from April to August. Latent heat showed $20Wm^{-2}$(July) with its minimum in July and $49Wm^{-2}$ with its maximum in March in monthly mean value. The annual mean of net heat flux is $129Wm^{-2}$, giving an annual heat surplus of $22Wm^{-2}$. Thus, during summer, the upwelled cold water at Gampo, appears to compensate the heat gain. However the ways in which these compensations are accomplished remains to be clarified.

제주한란의 자생환경 특성 및 분포에 관한 연구 (Habitat Characteristics and Distribution of Cymbidium kanran Native to Jejudo, Korea)

  • 이종석
    • 한국환경복원기술학회지
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    • 제7권1호
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    • pp.40-49
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    • 2004
  • This work carried out to define the characteristic of Cymbidium kanran habitat at Mt. Halla in Jejudo, Korea from the ecological point of view including geological and topographical features, air and soil temperature, relative humidity, fluctuations of light intensity, habitat vegetation, distribution altitude, area limit, and etc. And another goal of this study consider the conservation counterplan of the cymbidium habitat. Natural distribution areas of the cymbidium were observed more abundantly on the well drained south and east-facing slopes. Soil acidity was ranged from pH 4.1 to 5.3, and electric conductivity was ranged from 176.4 to 299.9 us/cm (average 215.3 us/cm). Base-saturation percentage of the habitat soil was below 50%, bulk density 0.42g/$cm^2$, particle density 2.05g/$cm^2$, humus content 26%, total nitrogen 0.82%, available phosphate 4.2 mg/kg, exchangeable potassium 0.63 Cmol/kg, calcium 0.44 Cmol/kg and magnesium 0.67 Cmol/kg. Annual mean air temperature was $15.4^{\circ}C$, however, air temperature was ranged $11.7{\sim}18.2^{\circ}C$ in spring, $21.2{\sim}23.8^{\circ}C$ in summer, $12.8{\sim}22.0^{\circ}C$ in fall and $5.5{\sim}7.8^{\circ}C$ in winter season. Annual mean soil temperature at depth of 10cm was $13.2^{\circ}C$ And minimum value was recorded $4.7^{\circ}C$ on January, and maximum value $22.5^{\circ}C$ on August. Relative humidity was ranged 90.8~94.7% in summer, 80.8~91.5% in fall and 77.6~84.2% in winter season. Minimum value was 56.5% on December, and maximum value was 100% on July and August. Light intensities were ranged from 400 to 1,800 lux at the greater part of Cymbidium kanran sites in Jejudo. Summer regarded as an lower light intensities was recorded to be range of 500~600 lux; however, autumn and winter were shown higher light regimes ranged from 3,500 to 3,800 lux. Therefore, one must be suprised that the cymbidium grow at the light condition of 6 lux (minimum) or 10,000 lux (maximum). Tree species keeping higher frequency rate and density were Eurya japonica, Camellia japonica, Castanopsis cuspidata, Carpinus laxiflora and Pinus densiflora. Number of trees growing in a 5${\times}$5m quardrat was 35 as an average, and proportion of evergreen versus deciduous was 5:1. Distribution altitude of the orchid habitat was ranged from 120m (low) to 840m (high) from sea level on the south facing slope of Mt. Halla, and was ranged eastern borderline of Gujwaup, Bukjejugun to western boundaries of Jungmundong, Seogwipo city. For the stable conservation of Cymbidium kanran habitat, sunlight regimes must be increased more by means of cutting trees or twigs in the site.

Characteristics of atmospheric environment over Korean peninsula for the optical remote sensing

  • Lee, Jung-Lim;Suh, Myoung-Seok;Kwak, Chong-Heum;Jeong, Jae-Joon
    • 대한원격탐사학회:학술대회논문집
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    • 대한원격탐사학회 2002년도 Proceedings of International Symposium on Remote Sensing
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    • pp.3-6
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    • 2002
  • In this study, we investigate the atmospheric environment changes in the aspect of optical remote sensing using surface observation data from 1971 to 2000 of Korea Meteorological Administration. Visibility, spatially averaged over Korean peninsula, is systematically reduced from about 28km to 18km during the last 30 years. It means that atmospheric conditions for the optical remote sensing over Korean peninsula are growing worse and worse due to the degradation of air quality. The 30-year average of cloud amount shows a strong seasonal variation, maximum(75%) in summer and minimum (35%) in autumn. Precipitation also shows a very similar variation pattern with cloud. The temperature and sea level pressure show a opposite seasonal change pattern, maximum(minimum in SLP) in summer and minimum(maximum in SLP) in winter, respectively. Relative humidiy(RH) is one of the variables mostly affected by urbanization or urban heat island. As a results, annual mean RH is decreased from 73% to 68% during last 30 years. When we take into account the favorable and unfavorable factors all together, summer and autumn are the worst and the best season for optical remote sensing in Korea.

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한국(韓國)과 일본(日本)의 기온조건(氣溫條件)의 차이(差異)와 수도작(水稻作)에의 의미(意味) (Differences in Temperature between Korea and Japan, and its Inference in Rice Planting)

  • 곡신휘;정영상
    • 한국토양비료학회지
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    • 제18권4호
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    • pp.348-351
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    • 1985
  • 한국(韓國)과 일본(日本)의 농업기후조건(農業氣候條件)을 비교(比較)하기 위하여 기온(氣溫)을 분석(分析)하고 수도작(水稻作)에의 의미(意味)를 조사(調査)한 결과(結果)는 다음과 같다. 1. 평균기온(平均氣溫)은 최난월(最暖月)인 8월(月)에는 비슷하나 최한월(最寒月)인 1월(月)에는 큰 차이(差異)가 있어 한국(韓國)의 연교차(年較差)가 매우 크다. 2. 한국(韓國)에서 봄 가을에 기온변동(氣溫變動)이 심(甚)하여 특(特)히 등열기간중(登熱期間中)에 최저기온(最低氣溫)의 강하(降下)가 심(甚)하다. 따라서 같은 등열기간(登熱期間)의 적산온도(積算溫度)라 하더라도 한계온도(限界溫度) 이하(以下)로 떨어지는 한랭시간(寒冷時間) 적산온도(積算溫度)가 한국(韓國)에서 높으므로 등열(登熱)과 기온(氣溫)의 해석(解析)에 있어서 이 점(點)을 고려(考慮)하여야 한다.

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2013~2017년 연안해역별 해양기상요소의 시·공간 변화 및 해무발생시 특성 분석 (Temporal and Spatial Variations of Marine Meteorological Elements and Characteristics of Sea Fog Occurrence in Korean Coastal Waters during 2013-2017)

  • 박소희;송상근;박형식
    • 한국환경과학회지
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    • 제29권3호
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    • pp.257-272
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    • 2020
  • This study investigates the temporal and spatial variations of marine meterological elements (air temperature (Temp), Sea Surface Temperature (SST), and Significant Wave Height (SWH)) in seven coastal waters of South Korea, using hourly data observed at marine meteorological buoys (10 sites), Automatic Weather System on lighthouse (lighthouse AWS) (9 sites), and AWS (20 sites) during 2013-2017. We also compared the characteristics of Temp, SST, and air-sea temperature difference (Temp-SST) between sea fog and non-sea-fog events. In general, annual mean values of Temp and SST in most of the coastal waters were highest (especially in the southern part of Jeju Island) in 2016, due to heat waves, and lowest (especially in the middle of the West Sea) in 2013 or 2014. The SWH did not vary significantly by year. Wind patterns varied according to coastal waters, but their yearly variations for each coastal water were similar. The maximum monthly/seasonal mean values of Temp and SST occurred in summer (especially in August), and the minimum values in winter (January for Temp and February for SST). Monthly/seasonal mean SWH was highest in winter (especially in December) and lowest in summer (June), while the monthly/seasonal variations in wind speed over most of the coastal waters (except for the southern part of Jeju Island) were similar to those of SWH. In addition, sea fog during spring and summer was likely to be in the form of advection fog, possibly because of the high Temp and low SST (especially clear SST cooling in the eastern part of South Sea in summer), while autumn sea fog varied between different coastal waters (either advection fog or steam fog). The SST (and Temp-SST) during sea fog events in all coastal waters was lower (and more variable) than during non-sea-fog events, and was up to -5.7℃ for SST (up to 5.8℃ for Temp-SST).