• Title/Summary/Keyword: RCP SCENARIOS

Search Result 275, Processing Time 0.03 seconds

Change in potential evapotranspiration based on representative scenario by TOPSIS in North Korea (TOPSIS에 의한 대표 시나리오에 근거한 북한 잠재증발산량의 변화)

  • Ryu, Young;Sung, Jang Hyun
    • Proceedings of the Korea Water Resources Association Conference
    • /
    • 2020.06a
    • /
    • pp.195-195
    • /
    • 2020
  • 이 연구는 기후변화 위험에 노출되어 있는 북한에 대한 잠재증발산량의 미래 변화를 전망하였다. 이를 위해 IPCC AR5의 RCP 기후변화 시나리오로부터 모의된 미래 기온자료를 APCC (APEC Climate Center) Integrated Modeling (AIMS)를 사용하여 25개 관측 지점에 대해서 상세화하여, McGuinness-Borne 방법으로 잠재증발산량을 추정하였다. 6개의 성능 지표와 TOPSIS(Technique for Order of Preference by Similarity to Ideal Solution)로 27개 GCMs 간의 과거 기후 재현성을 비교하여, 관측 지점 규모에서 적정 GCM을 선정하였다. 마지막으로 각 지점에서 선정된 대표 시나리오(representative climate change scenarios, RCCS)로 북한 지역의 잠재증발산량의 미래 변화를 3개의 구간(F1: 2011-2040; F2: 2041-2070; F3: 2071-2100)에서 all CCS(climate change scenario)와 비교하고, 미래 변화를 정량적으로 제시하였다. 그 결과 공간 해상도가 더 높은 GCM이 RCCS로 선정되었으며, 미래로 갈수록 잠재증발산량이 증가하리라 전망되었다. 또한, 여름철 잠재증발산량의 모델 간 변동성은 미래 구간에 따라 점진적으로 증가되었고, 연 평균 증발산량은 과거 기후대비 1.4배(F1), 2.0배(F2) 및 2.6배(F3) 증가하였다.

  • PDF

The Future of Extreme Climate Change in Korean Peninsula Using National Standard Climate Change Scenarios and ETCCDI Index (국가 표준기후변화 시나리오와 ETCCDI지수를 이용한 한반도의 미래 극한사상변화 전망)

  • Jeong, Jin Woo;Jeung, Se Jin;Kim, Byung Sik
    • Proceedings of the Korea Water Resources Association Conference
    • /
    • 2020.06a
    • /
    • pp.134-134
    • /
    • 2020
  • 본 논문의 목적은 기후변화가 한반도에서의 극한기후에 미치는 영향을 전망하고자한다. 먼저, 기상청에서 제공하고 있는 SDQDM 편의보정을 거친 CCAW의 국가 표준기후변화 시나리오 13종을 이용하였으며, 참조기간을 기준으로 기후변화 시나리오의 모의 능력을 검토하였다. 이어 미래의 극한기후변화를 전망하기위해 WMO의 ETCCDI 지수를 이용하여 미래 극한기후를 전망하였다. 또한 Mann Kendall tau를 이용하여 한반도의 강수와 기온관련 극한지수 변화를 전망하였다. 분석 결과를 기온관련 지수에서 Current 기간일 때 WSDI지수가 공간적 변동성이 54%로 예상되며, TXx지수가 지역간의 공간적 변동성이 121%로 가장 클 것이라 예상된다. 강우관련 지수를 살펴보면 Current기간 일 때 r95p지수의 지역별 공간변동성이 59%로, RCP 4.5시나리오일 때 PRCP 지수의 공간변동성이 42%로, CDD지수의 공간변동성이 최대 59%로 분석되었다. 공간분포를 확인해본 결과 기온과 강수관련 지수 모두 한반도 중부지역에서 큰 상승 경향을 보였고, 미래기간의 경우 북한의 서해안, 남한의 남해안 지역에서 가장 큰 증가경향을 보였다. 즉 일습윤지속일수를 의미하는 CWD지수는 경상도, 전라도 지역에서 증가 경향을 나타냈으며, 충청도와 북한전역에서 감소경향을 나타났다. 또한 일교차를 의미하는 DTR지수는 한반도 전역에서 증가하는 것으로 전망되었다.

  • PDF

A Study on derivation of drought severity-duration-frequency curve through a non-stationary frequency analysis (비정상성 가뭄빈도 해석 기법에 따른 가뭄 심도-지속기간-재현기간 곡선 유도에 관한 연구)

  • Jeong, Minsu;Park, Seo-Yeon;Jang, Ho-Won;Lee, Joo-Heon
    • Journal of Korea Water Resources Association
    • /
    • v.53 no.2
    • /
    • pp.107-119
    • /
    • 2020
  • This study analyzed past drought characteristics based on the observed rainfall data and performed a long-term outlook for future extreme droughts using Representative Concentration Pathways 8.5 (RCP 8.5) climate change scenarios. Standardized Precipitation Index (SPI) used duration of 1, 3, 6, 9 and 12 months, a meteorological drought index, was applied for quantitative drought analysis. A single long-term time series was constructed by combining daily rainfall observation data and RCP scenario. The constructed data was used as SPI input factors for each different duration. For the analysis of meteorological drought observed relatively long-term since 1954 in Korea, 12 rainfall stations were selected and applied 10 general circulation models (GCM) at the same point. In order to analyze drought characteristics according to climate change, trend analysis and clustering were performed. For non-stationary frequency analysis using sampling technique, we adopted the technique DEMC that combines Bayesian-based differential evolution ("DE") and Markov chain Monte Carlo ("MCMC"). A non-stationary drought frequency analysis was used to derive Severity-Duration-Frequency (SDF) curves for the 12 locations. A quantitative outlook for future droughts was carried out by deriving SDF curves with long-term hydrologic data assuming non-stationarity, and by quantitatively identifying potential drought risks. As a result of performing cluster analysis to identify the spatial characteristics, it was analyzed that there is a high risk of drought in the future in Jeonju, Gwangju, Yeosun, Mokpo, and Chupyeongryeong except Jeju corresponding to Zone 1-2, 2, and 3-2. They could be efficiently utilized in future drought management policies.

Impacts assessment of Climate change on hydrologic cycle changes in North Korea based on RCP climate change scenarios I. Development of Long-Term Runoff Model Parameter Estimation for Ungauged Basins (RCP 기후변화시나리오를 이용한 미래 북한지역의 수문순환 변화 영향 평가 I. 미계측유역의 장기유출모형 매개변수 추정식 개발)

  • Jeung, Se Jin;Kang, Dong Ho;Kim, Byung Sik
    • Journal of Wetlands Research
    • /
    • v.21 no.spc
    • /
    • pp.28-38
    • /
    • 2019
  • Climate change on the Korean peninsula is progressing faster than the global average. For example, typhoons, extreme rainfall, heavy snow, cold, and heatwave that are occurring frequently. North Korea is particularly vulnerable to climate change-related natural disasters such as flooding and flooding due to long-term food shortages, energy shortages, and reckless deforestation and development. In addition, North Korea is classified as an unmeasured area due to political and social influences, making it difficult to obtain sufficient hydrologic data for hydrological analysis. Also, as interest in climate change has increased, studies on climate change have been actively conducted on the Korean Peninsula in various repair facilities and disaster countermeasures, but there are no cases of research on North Korea. Therefore, this study selects watershed characteristic variables that are easy to acquire in order to apply localization model to North Korea where it is difficult to obtain observed hydrologic data and estimates parameters based on meteorological and topographical characteristics of 16 dam basins in South Korea. Was calculated. In addition, as a result of reviewing the applicability of the parameter estimation equations calculated for the fifty thousand, Gangneungnamdaecheon, Namgang dam, and Yeonggang basins, the applicability of the parameter estimation equations to North Korea was very high.

Prediction of present and future distribution of the Schlegel's Japanese gecko (Gekko japonicus) using MaxEnt modeling

  • Kim, Dae-In;Park, Il-Kook;Bae, So-Yeon;Fong, Jonathan J.;Zhang, Yong-Pu;Li, Shu-Ran;Ota, Hidetoshi;Kim, Jong-Sun;Park, Daesik
    • Journal of Ecology and Environment
    • /
    • v.44 no.1
    • /
    • pp.33-40
    • /
    • 2020
  • Background: Understanding the geographical distribution of a species is a key component of studying its ecology, evolution, and conservation. Although Schlegel's Japanese gecko (Gekko japonicus) is widely distributed in Northeast Asia, its distribution has not been studied in detail. We predicted the present and future distribution of G. japonicus across China, Japan, and Korea based on 19 climatic and 5 environmental variables using the maximum entropy (MaxEnt) species distribution model. Results: Present time major suitable habitats for G. japonicus, having greater than 0.55 probability of presence (threshold based on the average predicted probability of the presence records), are located at coastal and inland cities of China; western, southern, and northern coasts of Kyushu and Honshu in Japan; and southern coastal cities of Korea. Japan contained 69.3% of the suitable habitats, followed by China (27.1%) and Korea (4.2%). Temperature seasonality (66.5% of permutation importance) was the most important predictor of the distribution. Future distributions according to two climate change scenarios predicted that by 2070, and overall suitable habitats would decrease compared to the present habitats by 18.4% (scenario RCP 4.5) and 10.4% (scenario RCP 8.5). In contrast to these overall trends, range expansions are expected in inland areas of China and southern parts of Korea. Conclusions: Suitable habitats predicted for G. japonicus are currently located in coastal cities of Japan, China, and Korea, as well as in isolated patches of inland China. Due to climate change, suitable habitats are expected to shrink along coastlines, particularly at the coastal-edge of climate change zones. Overall, our results provide essential distribution range information for future ecological studies of G. japonicus across its distribution range.

Development of index for flood risk assessment on national scale and future outlook (전국 단위 홍수위험도 평가를 위한 지수 개발과 미래 전망)

  • Kim, Daeho;Kim, Young-Oh;Jee, Hee Won;Kang, Tae-Ho
    • Journal of Korea Water Resources Association
    • /
    • v.53 no.5
    • /
    • pp.323-336
    • /
    • 2020
  • Owing to climate change, the annual precipitation in Korea has increased since the 20th century, and it is projected to continue increasing in the future. This trend of increasing precipitation will raise the possibility of floods; hence, it is necessary to establish national adaptation plans for floods, based on a reasonable flood risk assessment. Therefore, this study focuses on developing a framework that can assess the flood risk across the country, as well as computing the flood risk index (FRI). The framework, which is based on IPCC AR5, is established as a combination of three indicators: hazard, exposure, and capacity. A data-based approach was used, and the weights of each component were assigned to improve the validity of the FRI. A Spearman correlation analysis between the FRI and flood damage verified that the index was capable of assessing potential flood damage. When predicting scenarios for future assessment using the HadGEM3-RA based on RCP 4.5 and 8.5, the flood risk tends to be lower in the early and mid-21st century, and it becomes higher at the end of the 21st century as compared with the present.

Effects of high temperature on the flowering & pod setting and rain in the seed elongation stage on the soybean growth

  • Han, Won Young;Park, Hyeon Jin;Jeon, Weon Tai;Ryu, Jong Soo;Bae, Jin Woo;Park, Jin Ki;Kwak, Kang Su;Baek, In Youl;Kang, Hang Won
    • Proceedings of the Korean Society of Crop Science Conference
    • /
    • 2017.06a
    • /
    • pp.326-326
    • /
    • 2017
  • Climate warming is the issue on the global scale. Soybean can be seriously damaged when high temperature occurs during a reproductive stage such as the flowering and pod-setting period according to the Representative Concentration Pathway (RCP) (2021~2100) 8.5 scenarios. The weather in 2016 was very different from other years (average for 30 years from 1980 to 2010) ; the highest temperature was $33.7^{\circ}C$ which was higher $3.29^{\circ}C$ than average temperature from last 30 years and average rainfall was 26.5 mm, lower 140.9 mm than average rainfalls from other years. Especially, the highest temperature during soybean flow-ering and pod setting stage was $26.8^{\circ}C$ which was higher $0.1^{\circ}C$ and rainfall was 172.2 mm, higher 47.8 mm than other years from the first to the 20th in the October at soybean seed elongation stage. Soybean leaves were turned upside down by the drought stress during the flowering and pod-setting stage. The numbe-r of pods and seeds per unit area decreased 11.0% and 30.3% compared with the previous year, respectively. The ripening period was prolonged by 21 days because of high temperature and soil moisture contents due to the continual rainmade increase of the seed weight up to 15.6% and the yield decreased 7.1% compared to the previous year.

  • PDF

Water temperature assessment on the small ecological stream under climate change (기후변화에 따른 소하천에서의 수온 모의연구)

  • Park, Jung Sool;Kim, Sam Eun;Kwak, Jaewon;Kim, Jungwook;Kim, Hung Soo
    • Journal of Wetlands Research
    • /
    • v.18 no.3
    • /
    • pp.313-323
    • /
    • 2016
  • Water temperature affects physical and biological processes in ecologies on river system and is important conditions for growth rate and spawning of fish species. The objective of this study is to compare models for water temperature during the summer season for the Fourchue River (St-Alexandre-de-Kamouraska, Quebec, Canada). For this, three different models, which are CEQUEAU, Auto-regressive Moving Average with eXogenous input and Nonlinear Autoregressive with eXogenous input, were applied and compared. Also, future water temperature in the Fourchue river were simulated and analyzed its result based on the CMIP5 climate models, RCP 2.6, 4.5, 8.5 climate change scenarios. As the result of the study, the water temperature in the Fourchue river are actually changed and median water temperature will increase $0.2{\sim}0.7^{\circ}C$ in June and could decrease by $0.2{\sim}1.1^{\circ}C$ in September. Also, the UILT ($24.9^{\circ}C$) for brook trout are also likely to occurred for several days.

An Outlook of Changes in the Flowering Dates and Low Temperature after Flowering under the RCP8.5 Projected Climate Condition (기후변화 시나리오에 근거한 과수 개화기 변화 및 개화 후 저온 발생 전망)

  • Kim, Dae-jun;Kim, Jin-Hee
    • Korean Journal of Agricultural and Forest Meteorology
    • /
    • v.20 no.4
    • /
    • pp.313-320
    • /
    • 2018
  • In the spring of 2018, opened-flowers of fruit trees were frozen to death due to abnormal low temperature around Jeonbuk Province and southern Gyeonggi Province areas. In the 2000s, abnormal weather is observed all over the world very frequently. As a consequence, various sectors of the society suffer from economic damage and negative effects of the abnormal weather. Moreover, recent global climate change is believed to increase the incidence of extreme weathers, which are out of the normal range of the local climate. It is necessary to identify these abnormal weather phenomena accurately and analyze the effects of them on crops in order to understand the effects of them on crop yields. This study projected the trend of the low-temperature occurrence in the future by predicting the changes in future flowering dates and quantifying the temperature distribution after flowering using climate change scenarios. This study targeted areas actually producing a major portion of pear, peach, and apple in South Korea. The results of this study predicted that the flowering dates of these fruits will be approximately 20 days earlier than the current normal year in the future (2071-2100) for the study area. Moreover, it was found that the distribution of low temperature would vary by fruit type and region to some degree. The results of this study present only a portion of fruit trees cultivars grown in South Korea. It was expected that, when this approach is applied to various crops and fruit trees, it will be possible to contribute to preparing countermeasures for climate change in the agricultural sector.

Potential Impacts of Climate Change on Water Temperature of the Streams in Han-River Basin (기후변화 시나리오별 한강유역의 수계별 수온상승 가능성)

  • Kim, Minhee;Lee, Junghee;Sung, Kyounghee;Lim, Cheolsoo;Hwang, Wonjae;Hyun, Seunghun
    • Journal of Korean Society on Water Environment
    • /
    • v.38 no.1
    • /
    • pp.19-30
    • /
    • 2022
  • Climate change has increased the average air temperature. Rising air temperature are absorbed by water bodies, leading to increasing water temperature. Increased water temperature will cause eutrophication and excess algal growth, which will reduce water quality. In this study, long-term trends of air and water temperatures in the Han-river basin over the period of 1997-2020 were discussed to assess the impacts of climate change. Future (~2100s) levels of air temperature were predicted based on the climate change scenarios (Representative concentration pathway (RCP) 2.6, 4.5, 6.0, and 8.5). The results showed that air and water temperatures rose at an average rate of 0.027℃ year-1 and 0.038℃ year-1 respectively, over the past 24 years (1997 to 2020). Future air temperatures under RCP 2.6, 4.5, 6.0, and 8.5 increased up to 0.32℃ 1.18℃, 2.14℃, and 3.51℃, respectively. An increasing water temperature could dissolve more minerals from the surrounding rock and will therefore have a higher electrical conductivity. It is the opposite when considering a gas, such as oxygen, dissolved in the water. Water temperature also governs the kinds of organisms that can live in rivers and lakes. Fish, insects, zooplankton, phytoplankton, and other aquatic species all have a preferred temperature range. As temperatures get too far above or below this preferred range, the number of individuals of the species decreases until finally there are none. Therefore, changes of water temperature that are induced by climate change have important implications on water supplies, water quality, and aquatic ecosystems of a watershed.