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      https://www.riss.kr/link?id=A103452716

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      다국어 초록 (Multilingual Abstract)

      Regional climate simulations for the CORDEX East Asia domain were conducted between 1981 and 2100 using five models to project future climate change based on RCP2.6, 4.5, 6.0, and 8.5 scenarios. By using the ensemble mean of five model results, future changes in climate zones and four extreme temperature events of South Korea were investigated according to Köppen-Trewartha’s classification criteria. The four temporal periods of historical (1981-2005), early future (2021-2040), middle future (2041-2070), and late future (2071-2100) were defined to examine future changes. The analysis domain was divided into 230 administrative districts of South Korea. In historical (1981-2005) period, the subtropical zones are only dominant in the southern coastal regions and Jeju island, while those tend to expand in the future periods. Depending on the RCP scenarios, the more radiative forcing results in the larger subtropical zone over South Korea in the future. The expansion of the subtropical zone in metropolitan areas is more evident than that in rural areas. In addition, the enlargement of the subtropical zone in coastal regions is more prominent than that of in inland regions. Particularly, the subtropical climate zone for the late future period of RCP8.5 scenario is significantly dominant in most South Korea. All scenarios show that cold related extreme temperature events are expected to decrease and hot related extreme temperature events to increase in late future. This study can be utilized by administrative districts for the strategic plan of responses to future climate change.
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      Regional climate simulations for the CORDEX East Asia domain were conducted between 1981 and 2100 using five models to project future climate change based on RCP2.6, 4.5, 6.0, and 8.5 scenarios. By using the ensemble mean of five model results, future...

      Regional climate simulations for the CORDEX East Asia domain were conducted between 1981 and 2100 using five models to project future climate change based on RCP2.6, 4.5, 6.0, and 8.5 scenarios. By using the ensemble mean of five model results, future changes in climate zones and four extreme temperature events of South Korea were investigated according to Köppen-Trewartha’s classification criteria. The four temporal periods of historical (1981-2005), early future (2021-2040), middle future (2041-2070), and late future (2071-2100) were defined to examine future changes. The analysis domain was divided into 230 administrative districts of South Korea. In historical (1981-2005) period, the subtropical zones are only dominant in the southern coastal regions and Jeju island, while those tend to expand in the future periods. Depending on the RCP scenarios, the more radiative forcing results in the larger subtropical zone over South Korea in the future. The expansion of the subtropical zone in metropolitan areas is more evident than that in rural areas. In addition, the enlargement of the subtropical zone in coastal regions is more prominent than that of in inland regions. Particularly, the subtropical climate zone for the late future period of RCP8.5 scenario is significantly dominant in most South Korea. All scenarios show that cold related extreme temperature events are expected to decrease and hot related extreme temperature events to increase in late future. This study can be utilized by administrative districts for the strategic plan of responses to future climate change.

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      참고문헌 (Reference)

      1 박창용, "남한 상세 기후변화 시나리오를 이용한 아열대 기후대 및극한기온사상의 변화에 대한 연구" 한국지역지리학회 19 (19): 600-614, 2013

      2 Korea government, "Second National Climate Change Adaptation Measures"

      3 오석근, "Projections of High Resolution Climate Changes for South Korea Using Multiple-Regional Climate Models Based on Four RCP Scenarios. Part 2: Precipitation" 한국기상학회 52 (52): 171-189, 2016

      4 Belda, M., "Global warming-induced changes in climate zones based on CMIP5 projections" 71 (71): 17-31, 2016

      5 차동현, "Future Changes in Summer Precipitation in Regional Climate Simulations over the Korean Peninsula Forced by Multi-RCP Scenarios of HadGEM2-AO" 한국기상학회 52 (52): 139-149, 2016

      6 Feng, S., "Evaluating observed and projected future climate changes for the Arctic using the Köppen-Trewartha climate classification" 38 (38): 1359-1373, 2012

      7 Suh, M. -S., "Development of new ensemble methods based on the performance skills of regional climate models over South Korea" 25 (25): 7067-7082, 2012

      8 Belda, M., "Climate classification revisited: from Köppen to Trewartha" 59 (59): 1-13, 2014

      9 Korea Meteorological Administration, "Climate Change Outlook Report on the Korean Peninsula" Korea Meteorological Administration 151-, 2012

      10 IPCC, "Climate Change 2013: Synthesis Report, Contribution of Working Groups I, II and III to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change" IPCC 151-, 2013

      1 박창용, "남한 상세 기후변화 시나리오를 이용한 아열대 기후대 및극한기온사상의 변화에 대한 연구" 한국지역지리학회 19 (19): 600-614, 2013

      2 Korea government, "Second National Climate Change Adaptation Measures"

      3 오석근, "Projections of High Resolution Climate Changes for South Korea Using Multiple-Regional Climate Models Based on Four RCP Scenarios. Part 2: Precipitation" 한국기상학회 52 (52): 171-189, 2016

      4 Belda, M., "Global warming-induced changes in climate zones based on CMIP5 projections" 71 (71): 17-31, 2016

      5 차동현, "Future Changes in Summer Precipitation in Regional Climate Simulations over the Korean Peninsula Forced by Multi-RCP Scenarios of HadGEM2-AO" 한국기상학회 52 (52): 139-149, 2016

      6 Feng, S., "Evaluating observed and projected future climate changes for the Arctic using the Köppen-Trewartha climate classification" 38 (38): 1359-1373, 2012

      7 Suh, M. -S., "Development of new ensemble methods based on the performance skills of regional climate models over South Korea" 25 (25): 7067-7082, 2012

      8 Belda, M., "Climate classification revisited: from Köppen to Trewartha" 59 (59): 1-13, 2014

      9 Korea Meteorological Administration, "Climate Change Outlook Report on the Korean Peninsula" Korea Meteorological Administration 151-, 2012

      10 IPCC, "Climate Change 2013: Synthesis Report, Contribution of Working Groups I, II and III to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change" IPCC 151-, 2013

      11 Teutschbein, C., "Bias correction of regional climate model simulations for hydrological climate-change impact studies: Review and evaluation of different methods" 456 : 12-29, 2012

      12 Gallardo, C., "Assessment of climate change in Europe from an ensemble of regional climate models by the use of Köppen-Trewartha classification" 33 (33): 2157-2166, 2013

      13 Trewartha, G. T., "An Introduction to climate" McGraw-Hill 397-403, 1980

      14 권영아, "A1B 시나리오 자료를 이용한 우리나라 아열대 기후구 전망" 대한지리학회 42 (42): 355-367, 2007

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      학술지 이력

      학술지 이력
      연월일 이력구분 이력상세 등재구분
      2022 평가예정 재인증평가 신청대상 (재인증)
      2019-01-01 평가 등재학술지 유지 (계속평가) KCI등재
      2016-01-01 평가 등재학술지 유지 (계속평가) KCI등재
      2012-01-01 평가 등재학술지 선정 (등재후보2차) KCI등재
      2011-01-01 평가 등재후보 1차 PASS (등재후보1차) KCI등재후보
      2009-01-01 평가 등재후보학술지 선정 (신규평가) KCI등재후보
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      학술지 인용정보

      학술지 인용정보
      기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
      2016 0.63 0.63 0.67
      KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
      0.71 0.67 0.962 0.3
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