• Title/Summary/Keyword: Trewartha's climate classification

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Future Projection of Climatic Zone Shifts over Korean Peninsula under the SSP-RCP Scenario using Trewartha's Climate Classification (트레와다 기후구분을 이용한 SSP-RCP 기반 미래 한반도 기후대 변화 전망)

  • Jina Hur;Sera Jo;Yong-Seok Kim;Eung-Sup Kim;Kyo-Moon Shim;Min-Gu Kang;Seung-Gil Hong;Hojung Kim
    • Korean Journal of Agricultural and Forest Meteorology
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    • v.26 no.3
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    • pp.175-190
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    • 2024
  • In order to project changes in climate zones across the Korean Peninsula, the Trewartha's climate classification was applied to the SSP-RCP scenario data with a 1km resolution produced by the National Institute of Agricultural Sciences of the Rural Development Administration. Currently, most of the Korean Peninsula (92.3%) belongs to the temperate climate type (D), whereas only some areas (4.9%), such as Jeju Island, belongs to the subtropical climate type (C). According to SSP-RCP scenarios, the temperature is expected to gradually increase due to the influence of global warming during the 21st century, and the subtropical climate type is expected to expand to 14.1 to 48.6% of the total area of the Korean Peninsula in the far future. On the other hand, the temperate zone, which is currently most dominant on the Korean Peninsula, is expected to shrink by 85.8 to 51.4% in the late 21st century. If carbon dioxide emissions continue at the current rate, the entire Korean Peninsula will likely be dominated by subtropical and temperate regions in the distant future. In particular, the subtropical climate type is expected to dominate most of South Korea in the high-carbon scenario, except for highlands.

Future Projections on Subtropical Climate Regions over South Korea Using SRES A1B Data (A1B 시나리오 자료를 이용한 우리나라 아열대 기후구 전망)

  • Kwon, Young-Ah;Kwon, Won-Tae;Boo, Kyung-On;Choi, Young-Eun
    • Journal of the Korean Geographical Society
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    • v.42 no.3 s.120
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    • pp.355-367
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    • 2007
  • As the global warming has been influenced on various sectors including agriculture, fisheries and health, it is essential to project more accurate future climate for an assessment of climate change impact and adaptation strategy. The purpose of this study is to examine the boundary changes in the subtropical climate region in South Korea using observed 30-year(1971-2000) data and projected 100-year data based on the IPCC SRES A1B emission scenario. We have selected Trewartha's climate classification among various climate classification, defining the subtropical climate region as the region with monthly mean temperature $10^{\circ}C$ or higher during 8-12 months. By observed data, the subtropical climate region was only limited in Jeju-do and the farmost southern coastal area(Busan, Tongyeong, Geoje, Yeosu, Wando, Mokpo) of South Korea. The future projected climate region for the period of 2071-2100 included have shown that subtropical climate region extended to most of stations except for the ares of Taebaeksan and Sobaeksan Mountains.

Studies on Changes and Future Projections of Subtropical Climate Zones and Extreme Temperature Events over South Korea Using High Resolution Climate Change Scenario Based on PRIDE Model (남한 상세 기후변화 시나리오를 이용한 아열대 기후대 및 극한기온사상의 변화에 대한 연구)

  • Park, Chang Yong;Choi, Young Eun;Kwon, Young A;Kwon, Jae Il;Lee, Han Su
    • Journal of the Korean association of regional geographers
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    • v.19 no.4
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    • pp.600-614
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    • 2013
  • This study aims to examine spatially-detailed changes and projection of subtropical climate zones based on the modified K$\ddot{o}$ppen-Trewartha's climate classification and extreme temperature indices using $1km{\times}1km$ high resolution RCP 4.5 and RCP 8.5 climate change scenarios based on PRIDE model over the Republic of Korea. Subtropical climate zones currently located along the southern coastal region. Future subtropical climate zones would be pushed northwards expanding to the western and the eastern coastal regions as well as some metropolitan areas. For both scenarios, the frequency of cold-related extreme temperatures projects to be reduced while the frequency of hot-related ones projects to be increased. Especially, hot days with $33^{\circ}C$ or higher temperature projects to occur more than 30 days over the most of regions except for some mountain areas with high altitudes during the period of 2070~2100. This study might provide essential information to make climate change adaptation processes be enhanced.

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