• Title/Summary/Keyword: RCP4.5

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Predicting change of suitable plantation of Schisandra chinensis with ensemble of climate change scenario (기후변화 시나리오 앙상블을 통한 오미자의 재배적지 변화 예측)

  • Lee, Sol Ae;Lee, Sang-Hyuk;Ji, Seung-Yong;Choi, Jaeyong
    • Journal of Environmental Impact Assessment
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    • v.25 no.1
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    • pp.77-87
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    • 2016
  • Predicting possible distributed area of Schisandra chinensis which has long term cultivation period among non-timber forest products is needed to be studied to deal with climate change. Hence, distribution of Schisandra chinensis in the 2050s and 2070s was predicted under two scenario, RCP 4.5 and RCP 8.5, with ensemble of 5 climate models used in IPCC AR5. According to estimation using RCP 4.5, distribution of Schisandra chinensis in 2050s appeared to decrease 43% of current area and appeared to decrease 57% in 2070s respectively. Moreover, According to estimation using RCP 8.5, distribution of Schisandra chinensis in 2050s appeared to decrease 55% of current area and appeared to decrease 85% in 2070s. As a final outcome, Schisandra chinensis was estimated to extinct in the future except Gangwon-do and Gyeongsangbuk-do when analyzing change between current distributed area and future distributed area. As a result, those areas were classified as vulnerable areas to climate change. Therefore, Gangwon-do and Gyeongsangbuk-do were thought to be ideal for growing Schisandra chinensis. The result from this study can be used to provide basic information for selecting proper area of Schisandra chinensis considering climate change effect.

Analysis of dam inflow and sediment changes in the andongdam watershed according to the RCP scenario (RCP 시나리오에 따른 안동댐 유역의 댐유입량 및 유사량 변화 분석)

  • Do, Yeonsu;Kim, Gwangseob
    • Proceedings of the Korea Water Resources Association Conference
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    • 2018.05a
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    • pp.187-187
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    • 2018
  • 최근 우리나라에서는 기후변화에 따른 이상기후로 인하여 홍수와 가뭄 등 자연 재해의 빈도가 증가하는 등 사회, 경제, 환경 등 다양한 분야에 영향을 받고 있다. 또한 우리나라는 기후변화와 더불어 강우의 계절적 특징상 강우량의 편중현상이 발생하므로 물 관리의 어려움이 크다. 이러한 상황에서 수자원의 미래 변화에 관한 연구는 필수적이며, 본 연구에서는 안동댐 유역을 대상 유역으로 하여 댐유입량과 유사량의 RCP 시나리오에 따른 변화 분석을 실시하였다. 댐유입량은 수자원의 이용에 있어서 직접적인 연관이 있는 중요한 요소이며, 유사량 또한 수자원의 효용가치를 증가시키기 위해 제어해야할 중요한 요소이다. 경상북도 안동시에 위치한 다목적댐인 안동댐은 유역면적이 $1,584km^2$이고, 총 저수용량은 $1,248\;10^6m^3$으로 용수공급 및 발전, 관광지 등으로 이용되고 있다. 안동댐 유역의 RCP 시나리오에 따른 변화 분석을 실시하기 위해, 분포형 수문모형인 SWAT(Soil and Water Assessment Tool) 모형을 이용하였다. RCP 시나리오를 적용하기 전, ASOS 관측자료를 이용하여 2010-2017 기간을 모의하고 2010년을 모형의 안정화 기간으로 두고, 2011-2017년에 대해 검보정을 실시한 후, RCP 시나리오에 따른 모의를 실시하였다. RCP 시나리오는 기후변화센터에서 제공하는 RCP 4.5와 RCP 8.5 시나리오를 이용하였으며, 2010-2099 기간에 관하여 SWAT 모형을 모의하고, 2010년을 모형의 안정화 기간, 2011-2040 기간을 2025s, 2041-2070 기간을 2055s, 2071-2099 기간을 2085s로 두어 결과를 ASOS 관측자료를 이용한 결과와 비교 분석하였다.

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A Study on Runoff and Pollutant Loading Prediction Using AR5 RCP4.5 Scenario in Nakdong River Watershed (AR5 RCP4.5 시나리오를 이용한 낙동강 유역에서의 유출 및 오염부하 전망)

  • Kim, Jung Min;Kim, Young Do;Kang, Busik;Park, Jin Hyeog
    • Proceedings of the Korea Water Resources Association Conference
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    • 2016.05a
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    • pp.111-111
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    • 2016
  • 최근 전 세계적으로 이상기후로 인해 극한 사상의 기후현상이 잦아지고 있으며 그로인한 피해가 확산되면서 관심이 높아지고 있다. 특히, 국내하천의 경우 높은 하상계수를 가지고 있는 만큼 수자원보전에 취약하고 수질의 문제 또한 대두되고 있다. 4대강 중 하나인 낙동강에는 8개의 보가 설치되었고 유역에 안동, 임하, 합천, 남강, 밀양댐 등 다기능댐이 있어 댐의 방류량이 낙동강의 유량에 큰 영향을 미치고 있다. 낙동강의 유량 및 수질을 관리하기 위해서는 이러한 현황들을 반영하여 유역관리를 포함한 통합적인 유량 및 수질관리가 필요하다. 본 연구에서는 IPCC에서 제공하는 AR5 RCP4.5 시나리오를 분위사상법(Quantile mapping)과 CF 다운스케일링 기법을 사용하여 유역에 맞게 상세화를 수행하였으며, 검 보정을 거친 SWAT 모형의 입력자료로 사용하여 낙동강 유역의 본류 및 지류의 미래 유출량 및 오염부하량을 예측하였다. 낙동강 유역에서의 미래기후변화 시나리오를 분석한 결과, 비홍수기에 32.3%, 홍수기에 31.1% 증가하는 것으로 나타났고, 2041 ~ 2070년도에 6%까지 증가하였다가 2071 ~ 2100년에 0.4% 감소하였다. 미래기후변화 시나리오를 SWAT 모형에 적용한 결과로는 주요 8개 지류에서 비슷한 패턴을 보였으며, 위천과 남강에서 각각 최대 45.5%, 16.6% 유출량이 증가하는 것으로 나타났다.

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Impact of IPCC RCP Scenarios on Streamflow and Sediment in the Hoeya River Basin (대표농도경로 (RCP) 시나리오에 따른 회야강 유역의 미래 유출 및 유사 변화 분석)

  • Hwang, Chang Su;Choi, Chul Uong;Choi, Ji Sun
    • Journal of Korean Society for Geospatial Information Science
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    • v.22 no.3
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    • pp.11-19
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    • 2014
  • This study is analyze future climate and land cover change affects behaviors for amount of streamflow and sediment discharge within basin. We used the climate forecast data in RCP 4.5 and 8.5 (2011-2100) which is opposite view for each other among RCP scenarios that are discussed for 5th report for IPCC. Land cover map built based on a social economic storyline in RCP 4.5/8.5 using Logistic Regression model. In this study we set three scenarios: one scenario for climate change only, one for land cover change only, one for Last both climate change and land cover change. It simulated amount of streamflow and sediment discharge and the result showed a very definite change in the seasonal variation both of them. For climate change, spring and winter increased the amount of streamflow while summer and fall decreased them. Sediment showed the same pattern of change steamflow. Land cover change increases the amount of streamflow while it decreases the amount of sediment discharge, which is believed to be caused by increase of impervious Surface due to urbanization. Although land cover change less affects the amount of streamflow than climate change, it may maximize problems related to the amount of streamflow caused by climate change. Therefore, it's required to address potential influence from climate change for effective water resource management and prepare suitable measurement for water resource.

Projection of Future Snowfall and Assessment of Heavy Snowfall Vulnerable Area Using RCP Climate Change Scenarios (RCP 기후변화 시나리오에 따른 미래 강설량 예측 및 폭설 취약지역 평가)

  • Ahn, So Ra;Lee, Jun Woo;Kim, Seong Joon
    • KSCE Journal of Civil and Environmental Engineering Research
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    • v.35 no.3
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    • pp.545-556
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    • 2015
  • This study is to project the future snowfall and to assess heavy snowfall vulnerable area in South Korea using ground measured snowfall data and RCP climate change scenarios. To identify the present spatio-temporal heavy snowfall distribution pattern of South Korea, the 40 years (1971~2010) snowfall data from 92 weather stations were used. The heavy snowfall days above 20 cm and areas has increased especially since 2000. The future snowfall was projected by HadGEM3-RA RCP 4.5 and 8.5 scenarios using the bias-corrected temperature and snow-water equivalent precipitation of each weather station. The maximum snowfall in baseline period (1984~2013) was 122 cm and the future maximum snow depth was projected 186.1 cm, 172.5 mm and 172.5 cm in 2020s (2011~2040), 2050s (2041~2070) and 2080s (2071~2099) for RCP 4.5 scenario, and 254.4 cm, 161.6 cm and 194.8 cm for RCP 8.5 scenario respectively. To analyze the future heavy snowfall vulnerable area, the present snow load design criteria for greenhouse (cm), cattleshed ($kg/m^2$), and building structure ($kN/m^2$) of each administrative district was applied. The 3 facilities located in present heavy snowfall areas were about two times vulnerable in the future and the areas were also extended.

Evaluation of the past and future droughts using Standardized Precipitation Index (SPI) and Effective Drought Index (EDI) in the western region of Chungnam Province (SPI와 EDI를 이용한 충남 서부지역 과거와 미래 가뭄 평가)

  • An, Hyowon;Ha, Kyoochul
    • Journal of Soil and Groundwater Environment
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    • v.25 no.4
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    • pp.14-27
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    • 2020
  • The drought has occurred from the past, and has caused a lot of damage. It is important to analyze the past droughts and predict them in the future. In this study, the temperature and precipitation of the past and the future from climate change RCP 4.5 and 8.5 scenarios were analyzed for Seosan and Boryeong in the western region of Chungnam Province, which is considered as a drought-prone area on the Korean Peninsula. Comparing Standardized Precipitation Index (SPI) and Effective Drought Index (EDI) based on the past droughts, EDI was verified to be more suitable for the drought assessment. According to RCP 4.5, the frequency and intensity of droughts in the early future (2021~2060) were expected to increase and to be stronger. Particularly, severe droughts were predicted for a long time from 2022 to 2026, and from 2032 to 2039. Droughts were expected to decrease in the late future (2061~2100). From RCP 8.5, drought occurrences were predicted to increase, but the intensity of the droughts were expected to decrease in the future. As a result of evaluation of the frequencies of droughts by seasons, the region would be most affected by fall drought in the early future and by spring drought in the late future according to RCP 4.5. In the case of RCP 8.5, the seasonal effects were not clearly distinguished. These results suggest that droughts in the future do not have any tendency, but continue to occurr as in the past. Therefore, the measures and efforts to secure water resources and reinforcement of water supply facilities should be prepared to cope with droughts.

Predicting the Potential Distribution of Korean Pine (Pinus koraiensis) Using an Ensemble of Climate Scenarios (앙상블 기후 시나리오 자료를 활용한 우리나라 잣나무림 분포 적지 전망)

  • Kim, Jaeuk;Jung, Huicheul;Jeon, Seong Woo;Lee, Dong-Kun
    • Journal of the Korean Society of Environmental Restoration Technology
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    • v.18 no.2
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    • pp.79-88
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    • 2015
  • Preparations need to be made for Korean pine(Pinus koraiensis) in anticipation of climate change because Korean pine is an endemic species of South Korea and the source of timber and pine nut. Therefore, climate change adaptation policy has been established to conduct an impact assessment on the distribution of Korean pine. Our objective was to predict the distribution of Korean pine while taking into account uncertainty and afforestation conditions. We used the 5th forest types map, a forest site map and BIOCLIM variables. The climate scenarios are RCP 4.5 and RCP 8.5 for uncertainty and the climate models are 5 regional climate models (HadGEM3RA, RegCM4, SNURCM, GRIMs, WRF). The base period for this study is 1971 to 2000. The target periods are the mid-21st century (2021-2050) and the end of the 21st century (2071-2100). This study used the MaxEnt model, and 50% of the presences were randomly set as training data. The remaining 50% were used as test data, and 10 cross-validated replicates were run. The selected variables were the annual mean temperature (Bio1), the precipitation of the wettest month (Bio13) and the precipitation of the driest month (Bio14). The test data's ROC curve of Korean pine was 0.689. The distribution of Korean pine in the mid-21st century decreased from 11.9% to 37.8% on RCP 4.5 and RCP 8.5. The area of Korean pine at an artificial plantation occupied from 32.1% to 45.4% on both RCPs. The areas at the end of the 21st century declined by 53.9% on RCP 4.5 and by 86.0% on RCP 8.5. The area of Korean pine at an artificial plantation occupied 23.8% on RCP 4.5 and 7.2% on RCP 8.5. Private forests showed more of a decrease than national forests for all subsequent periods. Our results may contribute to the establishment of climate change adaptation policies for considering various adaptation options.

Assessment of climate change impacts on uncertainty and sensitivity of paddy water requirement in South Korea using multi-GCMs (Multi-GCMs을 활용한 논벼 필요수량의 불확성 및 민감도 기후영향평가)

  • Yoo, Seung-Hwan;Lee, Sang-Hyun;Choi, Jin-Yong;Yoon, Kwangsik;Choi, Dongho
    • Proceedings of the Korea Water Resources Association Conference
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    • 2016.05a
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    • pp.516-516
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    • 2016
  • 기후변화는 농업생산량 감소와 식량 안보 문제와 같이 농업에 심각한 영향을 미칠 수 있다. 또한 기존의 농업수리 및 관개배수 시설 운영에 영향을 줄 수 있다. 따라서 지속가능한 농업 수자원 관리를 위해서는 기후변화의 영향을 고려한 장기적인 계획 수립이 필요하다. 따라서 본 연구에서는 논벼 지역의 설계용수량의 확률론적 분석을 통한 논벼 필요수량 및 설계용수량에 대한 기후변화영향 평가를 실시하였다. 이를 위해서 본 연구에서는 23개 GCM의 36개 산출물을 활용하여 Multi-model ensemble 구축하였다. 먼저 GCM별 증발산량과 유효우량을 산정한 결과 중부지역에서는 IPSL-CM5A 모델의 기후변화자료를 활용할 경우 증발산량과 유효우량이 타 GCM 모델들과 비하여 크게 산정되었다. 남부지역에서는 CanESM2 모델을 적용할 경우 가장 많은 증발산량과 유효우량이 모의되는 것으로 나타났다. 이처럼 GCM별로 다양한 결과가 모의되기 때문에 농업시설 설계에 적용되는 설계용수량의 경우 안전성을 위하여 Multi-GCM models을 활용할 필요가 있다. Multi-model ensemble의 RCP 4.5와 RCP 8.5 시나리오를 적용한 결과, 모든 경우에서 1995s(1981-2014)에 비해 설계용수량은 점차적으로 증가하는 것으로 나타났다. 평균 증가율은 RCP 4.5에서 중부지역이 9.4%, 남부지역이 6.0% 증가하는 것으로 나타난 반면, RCP 8.5에서는 중부지역이 11.1%, 남부지역이 8.2% 증가하는 것으로 나타났다. 또한 여러 GCM 산출물간의 불확실성은 RCP 4.5보다는 RCP 8.5 시나리오가, 중부 지역보다는 남부 지역이, 논벼 증발산량 보다는 유효우량이 더 큰 것으로 분석되었다. 본 연구는 향후 미래 가뭄 위험성을 최소화하기 위한 농업 수자원관리 전략수립에 활용될 수 있을 것이다. 또한 본 연구결과는 기후변화 영향 평가에 있어서 적합한 GCM 자료를 선택하는데 있어, 불확실성을 가늠할 수 있는 유용한 척도로 이용될 수 있을 것으로 기대된다.

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Economic Analysis of Rural Green-Village Planning with Solar Energy considering Climate Change (기후변화를 고려한 농촌지역 그린빌리지의 태양에너지 활용에 관한 경제성 분석)

  • Kim, Dae-Sik;Wang, Young-Doo
    • Journal of Korean Society of Rural Planning
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    • v.19 no.3
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    • pp.25-36
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    • 2013
  • This study aims to perform the economic analysis to the use of solar power facilities in rural villages considering the climate change scenario. IPCC climate change scenarios in the recently adopted the RCP scenarios (RCP8.5, RCP6.5, RCP4.5, RCP2.6) was used. By RCP scenarios, solar radiation, depending on the scenario in 2100, respectively, 3.6%, 2.5%, 1.9%, 1.1% was assumed to increase. From the economic analysis(payback period is 25 year) on 8 points of each province, in all cases of normal data and four RCP scenarios, at all points analyzed were NPV indicate a negative, BC ratio less than 1.0, respectively. In the case of Mokpo, Chunnam RCP8.5, BC ratio were found to be up to a 0.92, followed by 0.89 in the case of RCP8.5 in Jinju, Kyungnam shows, while the minimum was in Jeju. BC ratio is 1.0 or bigger, in order for the normal solar radiation data in Mokpo, Chonnam was the minimum that it takes 37 years. Similarly, in the case of RCP scenarios, 30 years in Mokpo, Chonnam RCP8.5 and 31 years in the cases of Jinju, Kyungnam and Jeonju, Cheonbuk RCP8.5 were analyzed. It was analyzed that RCP8.5 has the highest value. BC analysis models for each of the factors, the results of the sensitivity analysis, the initial installation costs, electricity sales price, discount rate in the order of economy showed higher sensitivity, and the rest factors showed lower changes. Although there are some differences of solar radiation by region, but in Korea most facilities in rural areas, the use of solar power was considered to be economical enough, considering change of several factors with high sensitivity, such as increasing of government subsidies for the solar power installation of the facility, rising oil prices due to a rise in electricity sales price, and a change in discount rate. In particular, when considering climate change scenarios, the use of solar energy for rural areas of the judgment that there was more economical.

Future Changes in Surface Radiation and Cloud Amount over East Asia under RCP Scenarios (RCP 시나리오에 따른 미래 동아시아 지표복사에너지와 운량 변화 전망)

  • Lee, Cheol;Boo, Kyung-On;Shim, Sungbo;Byun, Youngwha
    • Journal of Climate Change Research
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    • v.7 no.4
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    • pp.433-442
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    • 2016
  • In this study, we examine future changes in surface radiation associated with cloud amount and aerosol emission over East Asia. Data in this study is HadGEM2-CC (Hadley Centre Global Environmental Model version 2, Carbon Cycle) simulations of the Representative Concentration Pathways (RCPs) 2.6/4.5/8.5. Results show that temperature and precipitation increase with rising of the atmosphere $CO_2$. At the end of $21^{st}$ century (2070~2099) relative to the end of $20^{st}$ century (1981~2005), changes in temperature and precipitation rate are expected to increase by $+1.85^{\circ}C/+6.6%$ for RCP2.6, $+3.09^{\circ}C/+8.5%$ for RCP4.5, $+5.49^{\circ}C/10%$ for RCP8.5. The warming results from increasing Net Down Surface Long Wave Radiation Flux (LW) and Net Down Surface Short Wave Radiation Flux (SW) as well. SW change increases mainly from reduced total Aerosol Optical Depth (AOD) and low-level cloud amount. LW change is associated with increasing of atmospheric $CO_2$ and total cloud amount, since increasing cloud amounts are related to absorb LW radiation and remit the energy toward the surface. The enhancement of precipitation is attributed by increasing of high-level cloud amount. Such climate conditions are favorable for vegetation growth and extension. Expansion of C3 grass and shrub is distinct over East Asia, inducing large latent heat flux increment.