• 제목/요약/키워드: ANNUAL MEAN TEMPERATURE

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Assessment of GCM and Scenario Uncertainties under Future Climate Change Conditions

  • Jang, S.;Hwang, M.;Park, J.;Lim, K.
    • 국제학술발표논문집
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    • The 6th International Conference on Construction Engineering and Project Management
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    • pp.658-659
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    • 2015
  • GCM and scenario uncertainties are first investigated for 5 major watersheds (Han River, Paldang dam, Namhan River, Bukhan River and Imjin River watersheds). As a result of this study, it is found that CCSM3-based annual precipitation increases linearly with respect to the 10-year moving average values while CSIRO-based precipitation does not show much of trend. The results from annual DJF mean precipitation show a similar trend with respect to their 10-year moving average values. Both CCSM3- and CSIRO-based annual JJA mean precipitation do not show much of trend toward 21st century. In general, CCSM3-based precipitation values are slightly higher than CSIRO-based values with respect to their annual and annual JJA mean precipitation values, but CSIRO-based annual DJF mean precipitation values are slightly higher than CCSM3-based values. In case of mean air temperature between CCSM3 and CSIRO during 21st century, all of results show a clear trend in warming with the passage of time for 5 watersheds. However the upward trends from CCSM3-based values slow down toward end of 21stcentury while CSRIO-based values increases almost linearly.

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영산강하류의 계절 변화에 따른 수질특성과 유기인산염의 분해율에 관한 연구 I - 부영양화를 중심으로 - (A study on characteristics of water quality and degradation rates of organic phosphates in Young-San river)

  • 조기안;안병권;홍순강;정동옥
    • 한국환경과학회지
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    • 제8권6호
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    • pp.691-697
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    • 1999
  • The work on the eutropication of Youngsan river was conducted from Jul. 1997 to Jun. 1998. The value of water temperature in the study area varied from $4^{\circ}C\;to\;32^{\circ}C$ with an annual mean of $17.5^{\circ}C$. DO varied from 4.0 $mg/{\ell}$ to 13.5 $mg/{\ell}$, with an annual mean 10.2 $mg/{\ell}$,. BOD varied from 0.8 $mg/{\ell}$, to 6.4 $mg/{\ell}$ with an annual mean 3.1 $mg/{\ell}$. COD varied from 4.6 $mg/{\ell}$, to 9.0 $mg/{\ell}$ with an annual mean 6.38 $mg/{\ell}$. Nitrate varied from 1.58 $mg/{\ell}$, to 6.77 $mg/{\ell}$, with an annual mean of 3.475 $mg/{\ell}$, Total-nitrogen varied from 2.14 $mg/{\ell}$ to 8.38 $mg/{\ell}$ with an annual mean of 5.083 $mg/{\ell}$. Total-phosphate varied from 0.035 $mg/{\ell}$ to 0.588 $mg/{\ell}$ with an annual mean of 0.128 $mg/{\ell}$. Chl.a varied from 1.8 ${\mu}g/{\ell}$ to 75.0 ${\mu}g/{\ell}$ with an annual mean of 19.55 ${\mu}g/{\ell}$. The euthrophic state index of $Carlson^{16)}$ were showed 61.8(TP) and 71(SD) value

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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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Inverse Relationship of Hemiptera Richness with Temperature in South Korea

  • Kwon, Tae-Sung;Jung, Sungcheol;Park, Young-Seuk
    • 생태와환경
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    • 제54권2호
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    • pp.102-107
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    • 2021
  • The distribution pattern of species richness was determined by temperature. To examine the relationship between hemipteran richness and temperature, hemipteran species were collected using pitfall traps at six different oak forest sites with different annual mean temperatures in South Korea. Multiple linear regression analyses were conducted with mean annual temperature (MAT) and plant richness to evaluate differences in hemipteran richness. The influences of MAT and plant richness of study sites on hemipteran richness were examined by comparing three models (plant richness+MAT+MAT2, plant richness+MAT, and MAT) or two models (plant richness+MAT and MAT). Hemipteran richness showed an inverse diversity pattern as a function of temperature, with higher species richness at lower temperature sites. Meanwhile, Aphididae showed a bell-shaped diversity pattern with the highest value at low medium temperatures. The regression analysis showed that hemipteran richness was affected by temperature and plant richness in their habitats.

한반도 미래 기온 변화 예측을 위한 ECHO-G/S 시나리오의 통계적 상세화에 관한 연구 (A Study on Statistical Downscaling for Projection of Future Temperature Change simulated by ECHO-G/S over the Korean Peninsula)

  • 신진호;이효신;권원태;김민지
    • 대기
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    • 제19권2호
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    • pp.107-125
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    • 2009
  • Statistical downscaled surface temperature datasets by employing the cyclostationary empirical orthogonal function (CSEOF) analysis and multiple linear regression method are examined. For evaluating the efficiency of this statistical downscaling method, monthly surface temperature of the ECMWF has been downscaled into monthly temperature having a fine spatial scale of ~20km over the Korean peninsula for the 1973-2000 period. Monthly surface temperature of the ECHOG has also been downscaled into the same spatial scale data for the same period. Comparisons of temperatures between two datasets over the Korean peninsula show that annual mean temperature of the ECMWF is about $2^{\circ}C$ higher than that of the ECHOG. After applying to the statistical downscaling method, the difference of two annual mean temperatures reduces less than $1^{\circ}C$ and their spatial patterns become even close to each other. Future downscaled data shows that annual temperatures in the A1B scenario will increase by $3.5^{\circ}C$ by the late 21st century. The downscaled data are influenced by the ECHOG as well as observation data which includes effects of complicated topography and the heat island.

기후변화에 따른 농업생태계 변동과 대책 (Climate Change and Its Impact on Agricultural Ecosystem)

  • 윤성호
    • 한국작물학회:학술대회논문집
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    • 한국작물학회 1998년도 21세기 한반도 농업전망과 대책(한국작물학회.한국육종학회 공동주관 심포지움 회보)
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    • pp.313-335
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    • 1998
  • If the atmospheric concentrations of greenhouse gases double, the annual temperature increase in mean surface temperature relative to 1990 will be about 2.0 to $2.5^{\circ}C$ and the annual precipitation increase about $15{\%}$ by 2100 in Korea. When the temperature rises $2^{\circ}C$, the annual temperature will be $13^{\circ}C,\;15^{\circ}C,\;and\;16^{\circ}C$ in Western Central, Yeongnam Basin, and Southern Coastal respectively. Consequently the crop period could be prolonged $10{\~}29$ days. In the case of gradual global warming, annual crops could be adapted to the changed environment by breeding, and the perennial crops should be shifted to ether area. If global warming happens suddenly over the threshold of atmospheric greenhouse gases concentration, then we shall have disturbance of ecosystem. When $2^{\circ}C$ higher than present, the optimum flowering date of rice plant delayed about 10 days, so it may not possible to adopt the fate with present japonica rices, therefore, the recommended characteristics of rice varieties are longer basic vegetative period, more late maturing and higher ripening temperature. Barley and wheat crops could be shifted to northern coastal areas and apple production areas should be shifted to those areas under $13.5^{\circ}C$ in annual mean temperature at global warming. Ideotypes of crops under climate changes should have such ecological characteristics that are indispensable to accomplish the sustainable agriculture under increased $CO_{2}$ and temperature condition as the diversification of genetic resources from yield-oriented to biomass-oriented characteristics with the higher potentials of $CO_{2}$ absorption and Primary production. In addition, a heat-tolerance, a pest resistance, an environmental adaptability and a production stability should be also incorporated collectively into our integrated agroecosystem.

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부산광역시 국지적 기후 패턴에 대한 기온변화율과 불투수면의 영향 (Influences of Temperature Change Rates and Impervious Surfaces on the Intra-City Climatic Patterns of Busan Metropolitan Area)

  • 박선엽
    • 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.

Geographic Variation in Survival Rate and Height Growth of Pinus densiflora S. et Z. in Korea

  • Kim, In-Sik;Ryu, Keun-Ok;Song, Jeong-Ho;Kim, Tae-Su
    • 한국산림과학회지
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    • 제94권2호통권159호
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    • pp.73-81
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    • 2005
  • This study was conducted to examine the geographic variation among provenances of Pinus densiflora in survival rate and height growth at four test plantations (Jungsun, Chungju, Naju, and Jeju). The plantations were parts of the eleven provenance trials of Pinus densiflora established by Korea Forest Research Institute in 1996. The survival rate and height growth were significantly different among test plantations at $p{\leq}0.01$. Latitude and longitude of test plantation were negatively correlated with survival rate and height growth. On the other hand, annual mean temperature, mean temperature (Nov.~Feb.), extremely low temperature (Dec.~Feb.), and annual mean growing days of test plantation were positively correlated with these two. The relationships between growth variables and geographic variables were analysed with canonical correlation analysis. A considerable amount of variation in survival rate and height growth was explained by latitude, annual mean growing days, extremely low temperature (Dec.~Feb.) and extremely high temperature (Nov.~Feb.) of provenances. It is estimated that up to 47.1% and 67.4% of the genetic variability in survival rate and height growth was attributable to the environmental variability of the provenances, respectively. The response surface curve of survival rate and height growth was plotted against latitude and longitude to examine growth performance of provenances for each test site. Generally, the local provenances showed better survival rate and height growth.

남극 세종기지에서 최근 태양 복사, 기온과 운량의 변화 (Recent Changes in Solar Irradiance, Air Temperature and Cloudiness at King Sejong Station, Antarctica)

  • 이방용;조희구;김준;정연진;이윤곤
    • 대기
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    • 제16권4호
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    • pp.333-342
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    • 2006
  • The long-term trends of global solar irradiance, air temperature, specific humidity and cloudiness measured at King Sejong station, Antarctica, during the period of 1988-2004, have been investigated. A statistically insignificant decrease, -0.21 $Wm^{-2}yr^{-1}$ (-0.26 %$yr^{-1}$, P<0.5) in global solar irradiance was found in an analysis from the time series of the monthly mean values, except for the increasing trends only in two months of January and June. The trends in irradiance are directly and inversely associated with the cloudiness trends in annual and monthly means. The trends in surface air temperature show a slight warming, $0.03^{\circ}Cyr^{-1}$ (1.88 %$yr^{-1}$, P<0.5) on the annual average, with cooling trend in the summer months and the warming in the winter. The exact relationship, if any, between the irradiance and temperature trends is not known. No significant tendency was found in specific humidity for the same periods. Recent (1996-2004) erythermal ultraviolet irradiance shows decreasing trend in annual mean, -0.15 $mWm^{-2}yr^{-1}$ (-1.18 %$yr^{-1}$, P<0.1) which is about five times the trends of global solar irradiance. The ratio of erythermal ultraviolet to global solar irradiance shows remarkable seasonal variations with annual mean value of 0.01 % and a peak in October and November, showing the increase of ultraviolet irradiance resulting from the Antarctic ozone hole. The sensitivity of global solar irradiance to the change in cloudiness is roughly $13%oktas^{-1}$ which is about twice of the value at the South Pole due to the difference in the average surface reflectance between the two stations. Much more sensitive values of $59%oktas^{-1}$ was found for erythermal UV irradiance than for the global solar irradiance.

Developmental and Environmental Sources of Variation on Annual Growth Increments of Ascophyllum nodosum (Phaeophyceae)

  • Eckersley, Lindsay K.;Garbary, David J.
    • ALGAE
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    • 제22권2호
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    • pp.107-116
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    • 2007
  • Annual growth segments of Ascophyllum nodosum (L.) Le Jolis (Fucales, Fucaceae) are denoted by air bladders that form each spring. By examining annual growth segments, it may be possible to infer information about the physical conditions during the growth period; however, it is uncertain whether the annual segments will expand in size after the initial growth. We examined A. nodosum segments from three populations in Nova Scotia, and statistically evaluated whether the annual growth (length, mass, and maximum diameter) of segments was independent of the age of the frond, whether the segments increased in size after the initial growth, and whether the segment lengths were correlated with mean water temperatures and mean air temperatures when the segments were formed. We found that the growth in length of A. nodosum is dependent on the age of the frond, but frond age explained less than 12 % of the overall variation in length. However, the mass and maximum diameter of segments were independent of the age of the frond. Differences occurred between the lengths of segments formed in different years, but there was no significant correlation with regional mean water or air temperatures. This study indicates that the length of A. nodosum segments may be an indicator of the annual physical characteristics of a site, but future studies are needed to identify which factors have the strongest influence on growth patterns.