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    ECHO-G/S에 나타난 기후변화에 따른 엘니뇨 변화 특성 분석

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    https://www.riss.kr/link?id=A76202477

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    다국어 초록 (Multilingual Abstract) kakao i 다국어 번역

    Global warming may shift the properties and dynamics of ENSO. We study the changes in ENSO characteristics in a coupled general circulation model, ECHO-G/S. First, we analyse the mean state changes by comparing present day simulation and various high CO₂ climates. The model shows a little El Nino-like changes in the sea surface temperature and wind stress in the eastern tropical Pacific. As the mean temperature rises, the ENSO amplitude and the frequency of strong El Ninos and La Nina decrease. The analysis shows that the weakening of the oceanic sensitivities is related to the weakening of ENSO. In addition to the surface changes, the remote subsurface sea temperature response in the western Pacific to the wind stress in the eastern Pacific influences the subsequent ENSO amplitude. However, ENSO amplitude does not show linear response to the greenhouse gas concentrations.
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    Global warming may shift the properties and dynamics of ENSO. We study the changes in ENSO characteristics in a coupled general circulation model, ECHO-G/S. First, we analyse the mean state changes by comparing present day simulation and various high ...

    Global warming may shift the properties and dynamics of ENSO. We study the changes in ENSO characteristics in a coupled general circulation model, ECHO-G/S. First, we analyse the mean state changes by comparing present day simulation and various high CO₂ climates. The model shows a little El Nino-like changes in the sea surface temperature and wind stress in the eastern tropical Pacific. As the mean temperature rises, the ENSO amplitude and the frequency of strong El Ninos and La Nina decrease. The analysis shows that the weakening of the oceanic sensitivities is related to the weakening of ENSO. In addition to the surface changes, the remote subsurface sea temperature response in the western Pacific to the wind stress in the eastern Pacific influences the subsequent ENSO amplitude. However, ENSO amplitude does not show linear response to the greenhouse gas concentrations.

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    참고문헌 (Reference)

    1 문병권, "해양동화자료에서 나타난 열대태평양 연직경압모드 분석 II : 엘니뇨의 발달과 성장에 미치는 영향" 40 : 613-621,

    2 문병권, "해양동화자료에서 나타난 열대태평양 연직경압모드 분석 I : 일반적 특성" 40 : 603-612, 2004a

    3 구교숙, "온실가스 증가 시나리오 에 따른 미래 연직기온변화 전망" 41 : 1077-1088, 2005

    4 MR050C03, "기후변화협약대응 지역기후시나리오 활용기술 개발 (II)" 기상연구소 연구보고서 411-, 2006

    5 MR050C03, "기후변화협약대응 지역기후시나리오 활용기술 개발" 기상연구소 연구보고서 408-, 2005

    6 기상연구소, "기후변화협약대응 지역기후시나리오 산출기술 개발 (II)" 기상연구소 연구보고서 502-, 2003

    7 "Vertical structure variability in the equatorial Pacific before and after the Pacific climate shift of the 1970s"

    8 "Understanding diferences between the equatorial Pacific as simulated by two coupled GCMs" 15 : 449-469, 2002

    9 "Tropical air-sea interaction in general circulation models" Allaart 73-104, 1992

    10 "Toward understanding the response of the tropical atmosphere-ocean system to increased CO2 using equilibrium asynchronous coupling" 19 : 355-369, 2002

    1 문병권, "해양동화자료에서 나타난 열대태평양 연직경압모드 분석 II : 엘니뇨의 발달과 성장에 미치는 영향" 40 : 613-621,

    2 문병권, "해양동화자료에서 나타난 열대태평양 연직경압모드 분석 I : 일반적 특성" 40 : 603-612, 2004a

    3 구교숙, "온실가스 증가 시나리오 에 따른 미래 연직기온변화 전망" 41 : 1077-1088, 2005

    4 MR050C03, "기후변화협약대응 지역기후시나리오 활용기술 개발 (II)" 기상연구소 연구보고서 411-, 2006

    5 MR050C03, "기후변화협약대응 지역기후시나리오 활용기술 개발" 기상연구소 연구보고서 408-, 2005

    6 기상연구소, "기후변화협약대응 지역기후시나리오 산출기술 개발 (II)" 기상연구소 연구보고서 502-, 2003

    7 "Vertical structure variability in the equatorial Pacific before and after the Pacific climate shift of the 1970s"

    8 "Understanding diferences between the equatorial Pacific as simulated by two coupled GCMs" 15 : 449-469, 2002

    9 "Tropical air-sea interaction in general circulation models" Allaart 73-104, 1992

    10 "Toward understanding the response of the tropical atmosphere-ocean system to increased CO2 using equilibrium asynchronous coupling" 19 : 355-369, 2002

    11 "The oasis coupler user guide. version 2.2 Technical report TR/CMGC/ 98-05" CERFAS -2, 1998

    12 "The atmospheric general circulation model ECHAM4: Model description and simulation of present-day climate Technical report 218" Max Planck Institut fr Meteorologie 1996

    13 "Simulation of El Nino-Southern Oscillation-like variability in a global AOGCM and its response to CO2 increase" 8 : 1473-1502, 1995

    14 Knutson, T. R, "Simulated ENSO in a global coupled ocean atmosphere model" 10 : 131-161, 1997

    15 "Shifts in ENSO coupling processes under global warming" 33 : L11704-, 2006

    16 Guilyardi, E, "Representing El Nino in coupled ocean-atmos-phere GCMs the dominant role of the atmospheric component" 17 : 4623-4629, 2004

    17 "Internal variability in a 1000-year control simulation with the coupled climate model ECHO-G. Part II: El Nino Southern Oscillation and North Atlantic Oscillation" 57 : 622-640, 2005b

    18 "Internal variability in a 1000-year control simulation with the coupled climate model ECHO-G. Part I: near surface temperature, precipitation and mean sea level presure" 57 : 605-621, 2005a

    19 "Increased El Nio fre-quency in a climate model forced by future greenhouse warming" 398 : 694-697, 1999

    20 "Global warming patterns over the North Pacific: ENSO versus AO" 84 : 221-241, 2006

    21 "Future projec-tions of East Asian climate change from multi-model en-sembles of IPCC SRES Scenario simulations" 82 : 1187-1211, 2004

    22 "Future changes of El Nino in two global coupled climate models" 2006

    23 "Factors that afect the ampli-tude of El Nino in global coupled climate models" 17 : 515-526, 2001

    24 Guilyardi, E, "El Nio-mean state-seasonal cycle in-teractions in a multi-model ensemble" 26 : 329-348, 2006

    25 "El Nio and climate change" 24 : 3057-3060, 1997

    26 "El Nino in a changing climate : a multi-model study" 1 : 81-95, 2005

    27 "East Asian climate change in the 21st century as simulated by the coupled climate model ECHO-G under IPC SRES Scenarios" 84 : 1-26, 2006

    28 차유미, "ECHO-G/S를 활용한 미래 동아시아 기후 전망" 한국기상학회 17 (17): 55-68, 2007

    29 Merryfield, W. J, "Changes to ENSO under CO2 dou-bling in a multi-model ensemble" 19 : 4009-4027, 2006

    30 Chen, X, "Changes in ENSO in response to grenhouse warming as imulated by the CCSR/NIES/FRCG coupled GCM" 1 : 149-152, 2005-039

    31 "Anthropogenic forcing and decadal climate variability in sensitivity experiments of twentieth- and twenty-first-century climate" 13 : 3728-3744, 2000

    32 Ji, "An ocean analysis sys-tem for seasonal to interannual climate studies" 460-481,

    33 "A study of the sensitivity of ENSO to the mean climate" 6 : 111-18, 2006

    34 "A possible efect of an increase in the warm-pol SST on the magnitude of El Nio warming" 16 : 185-205, 2003

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    학술지 이력

    학술지 이력
    연월일 이력구분 이력상세 등재구분
    2026 평가 재인증평가 신청대상 (재인증)
    2020-01-01 등재 등재학술지 유지 (재인증) KCI등재
    2017-01-01 등재 등재학술지 유지 (계속평가) KCI등재
    2013-01-01 등재 등재 1차 FAIL (등재유지) KCI등재
    2010-01-01 등재 등재학술지 선정 (등재후보2차) KCI등재
    2009-01-01 등재 등재후보 1차 PASS (등재후보1차) KCI등재후보
    2008-01-01 등재 등재후보 1차 FAIL (등재후보1차) KCI등재후보
    2006-01-01 등재 등재후보학술지 선정 (신규평가) KCI등재후보
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    학술지 인용정보

    학술지 인용정보
    기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
    2016 0.64 0.64 0.57
    KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
    0.55 0.55 0.864 0.1
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