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    반경험식법을 이용한 미래 해수면 상승 예측 = Forecasting of Sea-Level Rise using a Semi-Empirical Method

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    https://www.riss.kr/link?id=A103023199

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    다국어 초록 (Multilingual Abstract) kakao i 다국어 번역

    In this paper, we predicted sea-level rise for RCP 4scenarios(RCP 2.6, RCP 4.5, RCP 6.0, RCP 8.5). To calculate sea-level rise, a semi-empirical method was used and it needs atmospheric temperature rise for each scenario. According to the results, the sea-level has been rising steadily in all scenarios. By 2050 the maximum difference of sea-level rise between the scenarios was within 0.08 m, but its difference was showed more than 0.5 m in 2100. The values of sea-level rise for RCP 2.6, RCP 4.5, RCP 6.0, RCP 8.5 scenarios are 0.87 m, 1.21 m, 1.02 m, 1.36 m, respectively. In the case of RCP 8.5, the slope of atmospheric temperature rise since 2060 was very steep compared to the other scenarios so that the maximum difference of sea-level rise between the scenarios will be much larger after 2100. Estimated by a simple approximation, the maximum difference of sea-level rise can be more than 1.2 m in 2120.
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    In this paper, we predicted sea-level rise for RCP 4scenarios(RCP 2.6, RCP 4.5, RCP 6.0, RCP 8.5). To calculate sea-level rise, a semi-empirical method was used and it needs atmospheric temperature rise for each scenario. According to the results, the...

    In this paper, we predicted sea-level rise for RCP 4scenarios(RCP 2.6, RCP 4.5, RCP 6.0, RCP 8.5). To calculate sea-level rise, a semi-empirical method was used and it needs atmospheric temperature rise for each scenario. According to the results, the sea-level has been rising steadily in all scenarios. By 2050 the maximum difference of sea-level rise between the scenarios was within 0.08 m, but its difference was showed more than 0.5 m in 2100. The values of sea-level rise for RCP 2.6, RCP 4.5, RCP 6.0, RCP 8.5 scenarios are 0.87 m, 1.21 m, 1.02 m, 1.36 m, respectively. In the case of RCP 8.5, the slope of atmospheric temperature rise since 2060 was very steep compared to the other scenarios so that the maximum difference of sea-level rise between the scenarios will be much larger after 2100. Estimated by a simple approximation, the maximum difference of sea-level rise can be more than 1.2 m in 2120.

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    참고문헌 (Reference)

    1 오상명, "지구온난화에 의한 북서태평양 및 한반도 근해의 해수면 상승" 한국해안,해양공학회 23 (23): 236-247, 2011

    2 van Vuuren, D. P., "The representative concentration pathwasys: an overview" 109 : 5-31, 2011

    3 Nakicenovic, N., "Special Report on Emissions Scenarios. Intergovernmental Panel on Climate Change" Cambridge University Press 570-, 2000

    4 National Academy of Science, "Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future" The National Academies Press 260-, 2012

    5 Rahmstorf, S., "Response to comments on “A semi-empirical approach to projecting future sea-level rise”" 317 (317): 1866-, 1866

    6 Radic V., "Regionally differentiated contribution of mountain glaciers and ice caps to future sea-level rise" 4 : 91-94, 2011

    7 Gehrels, W. R., "Rapid sea-level rise in the North Atlantic Ocean since the first half of the nineteenth century" 16 (16): 949-965, 2006

    8 Gregory, J. M., "Predictions of global and regional sea-level rise using AOGCMs with and without flux adjustment" 27 (27): 3069-3072, 2000

    9 Gehrels, W. R., "Onset of recent rapid sea-level rise in the western Atlantic Ocean" 24 : 2083-2100, 2005

    10 NIMR, "National Institute of Meteorological Research" National Institute of Meteorological Research Press 117-, 2011

    1 오상명, "지구온난화에 의한 북서태평양 및 한반도 근해의 해수면 상승" 한국해안,해양공학회 23 (23): 236-247, 2011

    2 van Vuuren, D. P., "The representative concentration pathwasys: an overview" 109 : 5-31, 2011

    3 Nakicenovic, N., "Special Report on Emissions Scenarios. Intergovernmental Panel on Climate Change" Cambridge University Press 570-, 2000

    4 National Academy of Science, "Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future" The National Academies Press 260-, 2012

    5 Rahmstorf, S., "Response to comments on “A semi-empirical approach to projecting future sea-level rise”" 317 (317): 1866-, 1866

    6 Radic V., "Regionally differentiated contribution of mountain glaciers and ice caps to future sea-level rise" 4 : 91-94, 2011

    7 Gehrels, W. R., "Rapid sea-level rise in the North Atlantic Ocean since the first half of the nineteenth century" 16 (16): 949-965, 2006

    8 Gregory, J. M., "Predictions of global and regional sea-level rise using AOGCMs with and without flux adjustment" 27 (27): 3069-3072, 2000

    9 Gehrels, W. R., "Onset of recent rapid sea-level rise in the western Atlantic Ocean" 24 : 2083-2100, 2005

    10 NIMR, "National Institute of Meteorological Research" National Institute of Meteorological Research Press 117-, 2011

    11 Yin, J., "Model projections of rapid sea-level rise on the northeast coast of the United States" 2 : 262-266, 2009

    12 Schaeffer M., "Long-term sea-level rise implied by 1.5°C and 2°C warming levels" 2 : 867-870, 2012

    13 IPCC SRES, "Intergovernmental Panel on Climate Change, Special Report on Emissions Scenarios" Cambridge University Press 1-20, 2000

    14 Vermeer, M., "Global sea level linked to global temperature" 106 (106): 21527-21532, 2009

    15 Leggett, J., "Emissions Scenarios for the IPCC: An Update, In Climate Change 1992: The Supplementary Report to the IPCC Scientific Assessment" Cambridge University Press 69-95, 1992

    16 Gregory, J. M., "Comparison of results from several AOGCMs for global and regional sea-level change 1900-2100" 18 : 225-240, 2001

    17 Horton, B. P., "Compaction of Holocene strata and the implications for relative sea-level change on the east coast of England" 37 (37): 1083-1086, 2009

    18 Kemp, A. C., "Climate related sea-level variations over the past two millennia" 108 (108): 11017-11022, 2011

    19 Solomon S., "Climate Change 2007 - The Physical Science Basis, Contribution of Working Group Ⅰ to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change(IPCC)" Cambridge University Press 1-996, 2007

    20 Rahmstorf, S., "A semi-empirical approach to projecting future sea-level rise" 315 : 368-370, 2007

    21 Church, J. A., "A 20th century acceleration in global sea-level rise" 33 : L01602-, 2006

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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 등재학술지 유지 (등재유지) KCI등재
    2010-01-01 등재 등재학술지 선정 (등재후보2차) KCI등재
    2009-01-01 등재 등재후보 1차 PASS (등재후보1차) KCI등재후보
    2008-01-01 등재 신청제한 (등재후보1차) KCI등재후보
    2007-01-01 등재 등재후보 1차 FAIL (등재후보1차) KCI등재후보
    2005-01-01 등재 등재후보학술지 선정 (신규평가) KCI등재후보
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    기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
    2016 0.42 0.42 0.43
    KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
    0.45 0.43 0.592 0.13
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