DOI QR코드

DOI QR Code

Forecasting of Sea-Level Rise using a Semi-Empirical Method

반경험식법을 이용한 미래 해수면 상승 예측

  • 김태윤 (한국환경정책.평가연구원) ;
  • 조광우 (한국환경정책.평가연구원)
  • Received : 2013.01.11
  • Accepted : 2013.02.25
  • Published : 2013.02.28

Abstract

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.

본 연구는 RCP 4종 시나리오(RCP 2.6, RCP 4.5, RCP 6.0, RCP 8.5)를 적용하여 얻어진 2100년까지의 대기온도 상승값을 해수면 상승 계산방법 중에 하나인 반경험식법(Semi-empirical method)에 적용하여 해수면 상승치를 예측하였다. RCP 4종 시나리오에서 얻어진 결과에 따르면 모든 시나리오에서 해수면이 꾸준히 상승하고 있음을 알 수 있었다. 2050년도까지 RCP 4종 시나리오에 대한 해수면 상승의 차이가 최대 0.08 m 이내였으나 2100년도에는 최대 0.5 m까지 해수면 상승의 격차를 보이고 있었다. RCP 2.6, RCP 4.5, RCP 6.0, RCP 8.5 시나리오의 2100년도 해수면 예상 상승치는 각각 0.87 m, 1.21 m, 1.02 m, 1.36 m였다. RCP 8.5시나리오는 2060년 이후로 대기온도 상승치가 다른 시나리오에 비해 급상승하는데, 2100년 이후 다른 시나리오와의 해수면 상승 격차는 더 커질 것으로 예상된다. 단순한 비례식으로 추정하면, 2080년도에 RCP 4종 시나리오의 최대 격차가 0.21 m였으나 20년 후인 2100년에는 그 두 배가 넘는 최대 0.5 m였다. 따라서 2120년에는 그 격차가 1.2 m 이상 될 수도 있다.

Keywords

References

  1. Church, J. A. and N. J. White(2006), A 20th century acceleration in global sea-level rise, Geophysical Research Letters, 33, L01602, doi:10.1029/2005GL024826.
  2. Gehrels, W. R., J. R. Kirby, A. Prokoph, R. M. Newnham, E. P. Achterberg, H. Evans, S. Black, and D. B. Scott(2005), Onset of recent rapid sea-level rise in the western Atlantic Ocean, Quaternary Science Reviews, 24, pp. 2083-2100. https://doi.org/10.1016/j.quascirev.2004.11.016
  3. Gehrels, W. R., W. A. Marshall, M. J. Gehrels, G. Larsen, J. R. Kirby, J. Eiriksson, J. Heinemeier, T. Shimmield(2006), Rapid sea-level rise in the North Atlantic Ocean since the first half of the nineteenth century, The Holocene, Vol. 16, No. 7, pp. 949-965. https://doi.org/10.1177/0959683606hl986rp
  4. Gregory, J. M., J. A. Church, G. J. Boer, K. W. Dixon, G. M. Flato, D. R. Jacket, J. A. Lowe, S. P. O'Farrell, E. Roeckner, G. L. Russell, R. J. Stouffer and M. Winton(2001), Comparison of results from several AOGCMs for global and regional sea-level change 1900-2100, Climate Dynamics, 18, pp. 225-240. https://doi.org/10.1007/s003820100180
  5. Gregory, J. M. and J. A. Lowe(2000), Predictions of global and regional sea-level rise using AOGCMs with and without flux adjustment, Geophysical Research Letters, Vol. 27, No. 19, pp. 3069-3072. https://doi.org/10.1029/1999GL011228
  6. Horton, B. P. and I. Shennan(2009), Compaction of Holocene strata and the implications for relative sea-level change on the east coast of England, Geology, Vol. 37, No. 12, pp. 1083-1086. https://doi.org/10.1130/G30042A.1
  7. IPCC SRES(2000), Intergovernmental Panel on Climate Change, Special Report on Emissions Scenarios, Cambridge University Press, Cambridge UK, pp. 1-20.
  8. IPCC AR4(2007), 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), Solomon S., et al. Eds., Cambridge University Press, Cambridge UK. pp. 1-996.
  9. Kemp, A. C., B. P. Horton, J. P. Donnelly, M. E. Mann, M. Vermeer, and S. Rahmstorf(2011), Climate related sea-level variations over the past two millennia, PNAS, Vol. 108, No. 27, pp. 11017-11022.
  10. Leggett, J., W. J. Pepper, and R. J. Swart(1992), Emissions Scenarios for the IPCC: An Update. In: Climate Change 1992: The Supplementary Report to the IPCC Scientific Assessment, Houghton, J. T., B. A. Callander, and S. K. Varney Eds., Cambridge University Press, Cambridge, pp. 69-95.
  11. Nakicenovic, N. and R. Swart(eds)(2000), Special Report on Emissions Scenarios. Intergovernmental Panel on Climate Change, Cambridge University Press, Cambridge UK. p. 570.
  12. National Academy of Science(2012), Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future, The National Academies Press, p. 260.
  13. NIMR(2011), National Institute of Meteorological Research, Climate Change Scenario Report 2011 to respond to the IPCC 5th Assessment Report, National Institute of Meteorological Research Press, p. 117.
  14. Oh, S. M., S. J. Kwon, I. J. Moon, and E. I. Lee(2011), Sea Level Rise due to Global Warming in the Northwestern Pacific and Seas around the Korean Peninsula, Journal of Korean Society of Coastal and Ocean Engineers, Vol. 23, No. 3, pp. 236-247. https://doi.org/10.9765/KSCOE.2011.23.3.236
  15. Rahmstorf, S.(2007a), A semi-empirical approach to projecting future sea-level rise, Science, 315, pp. 368-370. https://doi.org/10.1126/science.1135456
  16. Rahmstorf, S.(2007b), Response to comments on "A semi-empirical approach to projecting future sea-level rise", Science, Vol. 317, No. 5846, p. 1866, doi:10.1126/science.1141283.
  17. Radic V. and R. Hock(2011), Regionally differentiated contribution of mountain glaciers and ice caps to future sea-level rise, Nature Geoscience, 4, pp. 91-94. https://doi.org/10.1038/ngeo1052
  18. Schaeffer M., W. Hare, S. Rahmstorf, and M. Vermeer(2012), Long-term sea-level rise implied by $1.5^{\circ}C$ and $2^{\circ}C$ warming levels, Nature Climate Change, 2, pp. 867-870. https://doi.org/10.1038/nclimate1584
  19. van Vuuren, D. P., J. Edmonds, M. Kainuma, K. Riahi, A. Thomson, K. Hibbard, G. C. Hurtt, T. Kram, V. Krey, J-F. Lamarque, T. Masui, M. Meinshausen, N. Nakicenovic, S. J. Smith, and S. K. Rose(2011), The representative concentration pathwasys: an overview, Climate Change, 109, pp. 5-31. https://doi.org/10.1007/s10584-011-0148-z
  20. Vermeer, M. and S. Rahmstorf(2009), Global sea level linked to global temperature, PNAS, Vol. 106, No. 51, pp. 21527-21532. https://doi.org/10.1073/pnas.0907765106
  21. Yin, J., M. E. Schlesinger and R. J. Stouffer(2009), Model projections of rapid sea-level rise on the northeast coast of the United States, Nature Geoscience, 2, pp. 262-266. https://doi.org/10.1038/ngeo462

Cited by

  1. A Study on Estimation of Design Tidal level Considering Sea Level Change in the Korean Peninsula vol.17, pp.4, 2016, https://doi.org/10.5762/KAIS.2016.17.4.464
  2. Cost-Benefit Analysis of Seawalls in South Korea: A Bottom-Up Assessment vol.44, pp.6, 2016, https://doi.org/10.1080/08920753.2016.1233795
  3. Impact Assessment of Sea_Level Rise based on Coastal Vulnerability Index vol.27, pp.5, 2015, https://doi.org/10.9765/KSCOE.2015.27.5.304
  4. Game Theory–Based Analysis of Decision Making for Coastal Adaptation under Multilateral Participation vol.34, pp.6, 2018, https://doi.org/10.1061/(ASCE)ME.1943-5479.0000637
  5. Estimation of the non-exceedance probability of extreme storm surges in South Korea using tidal-gauge data vol.21, pp.8, 2013, https://doi.org/10.5194/nhess-21-2611-2021