Climatic Change

, Volume 100, Issue 3–4, pp 757–768 | Cite as

Perspectives of Northern Sea Route and Northwest Passage in the twenty-first century

  • V. C. Khon
  • I. I. Mokhov
  • M. Latif
  • V. A. Semenov
  • W. Park
Article

Abstract

The ability of modern climate models to simulate ice season length in the Arctic, its recent changes and navigation season on Arctic marine routes along the Eurasian and the North American coastlines is evaluated using satellite ice cover observations for 1979–2007. Simulated mean sea ice season duration fits remarkably well to satellite observations and so do the simulated 20th century changes using historical forcing. This provides confidence to extend the analysis to projections for the twenty-first century. The navigation season for the Northern Sea Route (NSR) and Northwest Passage (NWP), alternative sea routes from the North Atlantic to Asia, will considerably increase during this century. The models predict prolongation of the season with a free passage from 3 to 6 months for the NSR and from 2 to 4 months for the NWP by the end of twenty-first century according to A1B scenario of the IPCC. This suggests that transit through the NSR from Western Europe to the Far East may be up to 15% more profitable in comparison to Suez Canal transit by the end of the twenty-first century.

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References

  1. ACIA (2005) Arctic climate impact assessment. Cambridge University Press, CambridgeGoogle Scholar
  2. AMTW (2004) Arctic marine transport workshop. Cambridge University, CambridgeGoogle Scholar
  3. Arzel O, Fichefet T, Goosse H (2006) Sea ice evolution over the 20th and 21st centuries as simulated by the current AOGCMs. Ocean Model 12:401–415CrossRefGoogle Scholar
  4. Cavalieri DJ, Parkinson CL, Gloersen P, Comiso JC, Zwally HJ (1999) Deriving long-term time series of sea ice cover from satellite passive-microwave multisensor data sets. J Geophys Res 104:15803–15814CrossRefGoogle Scholar
  5. Collins WD, Bitz CM, Blackmon ML, Bonan GB, Bretherton CS, Carton JA, Chang P, Doney SC, Hack JJ, Henderson TB (2006) The community climate system model: CCSM3. J Clim 19:2122–2143CrossRefGoogle Scholar
  6. Comiso JC, Parkinson CL, Gersten R, Stock L (2008) Accelerated decline in the Arctic sea ice cover. Geophys Res Lett 35:L01703. doi:10.1029/2007GL031972 CrossRefGoogle Scholar
  7. Cressey D (2007) Arctic melt opens Northwest passage. Nature 449:267–267CrossRefGoogle Scholar
  8. Delworth TL, Rosati A, Stouffer RJ, Dixon KW et al (2006) GFDL’s CM2 global coupled climate models part 1: Formulation and simulation characteristics. J Clim 19:643–674CrossRefGoogle Scholar
  9. Granberg AG (1998) The Northern Sea route: trends and prospects of commercial use. Ocean Coast Manag 41:175–207CrossRefGoogle Scholar
  10. Granberg AG, Peresypkin VI (eds) (2006) Problemy Severnogo morskogo puti (Problems of the Northern Sea Route). Nauka, MoscowGoogle Scholar
  11. Granier C, Niemeier U, Jungclaus JH, Emmons L, Hess P, Lamarque JF, Walters S, Brasseur GP (2006) Ozone pollution from future ship traffic in the Arctic Northern passages. Geophys Res Lett 33:L13807. doi:10.1029/2006GL026180 CrossRefGoogle Scholar
  12. Howell SEL, Yackel JJ (2004) A vessel transit assessment of sea ice variability in the Western Arctic (1969-2002): implications for ship navigation. Can J Remote Sens 30:205–215Google Scholar
  13. IPCC (2007) Climate change 2007: impacts adaptation and vulnerability. Contribution of working group II to the fourth assessment report of the intergovernmental panel on climate change. Cambridge University Press, CambridgeGoogle Scholar
  14. Johns TC et al (2003) Anthropogenic climate change for 1860 to 2100 simulated with the HadCM3 model under updated emissions scenarios. Clim Dyn 20:583–612Google Scholar
  15. Johns TC et al (2006) The new Hadley Centre climate model HadGEM1: Evaluation of coupled simulations. J Clim 19:1327–1353CrossRefGoogle Scholar
  16. Kattsov VM, Alekseev GV, Pavlova TV, Sporyshev PV, Bekryaev RV, Govorkova VA (2007) Modeling the evolution of the world ocean ice cover in the 20th and 21st centuries. Izv Atmos Ocean Phys 43:142–157CrossRefGoogle Scholar
  17. Kitagawa H (ed) (2001) The Northern Sea route - The shortest sea route linking East Asia and Europe. Ship and Ocean Foundation, TokyoGoogle Scholar
  18. Marti O, Braconnot P, Bellier J, Benshila R et al (2005) The new IPSL climate system model: IPSL-CM4. Inst Pierre Simon Laplace des Sci de l’Environ Global, ParisGoogle Scholar
  19. Meehl GA, Covey C, Delworth T, Latif M et al (2007) The WCRP CMIP3 multimodel dataset - A new era in climate change research. Bull Am Meteorol Soc 88:1383–1394CrossRefGoogle Scholar
  20. Min SK, Legutke S, Hense A, Kwon WT (2005) 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 pressure. Tellus 57A:605–621Google Scholar
  21. Mokhov II, Khon VC, Roeckner E (2007) Variations in the ice cover of the Arctic basin in the 21st century based on model simulations: estimates of the perspectives of the Northern Sea Route. Dokl Earth Sci 415:759–763CrossRefGoogle Scholar
  22. Mulherin ND (1996) The Northern Sea Route: its development and evolving state of operations in the 1990s. CRREL, Hanover, New HampshireGoogle Scholar
  23. Park W, Keenlyside N, Latif M, Ströh A, Redler R, Roeckner E, Madec G (2009) Tropical Pacific climate and its response to global warming in the Kiel climate model. J Clim 22:71–92CrossRefGoogle Scholar
  24. Parkinson CL (1992) Spatial patterns of increases and decreases in the length of the sea ice season in the North Polar Region (1979–1986). J Geophys Res 97:14377–14388CrossRefGoogle Scholar
  25. Parkinson CL (2000) Variability of Arctic sea ice: the view from space, an 18-year record. Arctic 53:341–358Google Scholar
  26. Parkinson CL, Vinnikov KY, Cavalieri DJ (2006) Evaluation of the simulation of the annual cycle of Arctic and Antarctic sea ice coverages by 11 major global climate models. J Geophys Res 111:C07012. doi:101029/2005JC003408, with an erratum for the French model results at C12009, doi:10.1029/2006JC003949
  27. Peresypkin VI (2006) Further development of the NSR in the coming decades. In: Kitagawa H (ed) New era in Far East Russia and Asia. OPRF, Tokyo, pp 29–44Google Scholar
  28. Rayner NA, Parker DE, Horton EB, Folland CK, Alexander LV, Rowell DP, Kent EC, Kaplan A (2003) Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. J Geophys Res 108:4407Google Scholar
  29. Stewart EJ, Howell SEL, Draper D, Yackel J, Tivy A (2007). Sea ice in Canada’s Arctic: implications for cruise tourism. Arctic 60:370–380Google Scholar
  30. Stroeve J, Holland MM, Meier W, Scambos T, Serreze M (2007) Arctic sea ice decline: faster than forecast. Geophys Res Lett 34:L09501. doi:10.1029/2007GL029703 CrossRefGoogle Scholar
  31. Zhang X, Walsh JE (2006) Toward a seasonally ice-covered Arctic Ocean: scenarios from the IPCC AR4 model simulations. J Clim 19:1730–1747CrossRefGoogle Scholar
  32. Zhang J, Lindsay R, Steele M, Schweiger A (2008) What drove the dramatic retreat of Arctic sea ice during summer 2007? Geophys Res Lett 35:L11505. doi:10.1029/2008GL034005 CrossRefGoogle Scholar

Copyright information

© Springer Science+Business Media B.V. 2009

Authors and Affiliations

  • V. C. Khon
    • 1
    • 2
  • I. I. Mokhov
    • 1
  • M. Latif
    • 3
  • V. A. Semenov
    • 1
    • 3
  • W. Park
    • 3
  1. 1.Obukhov Institute of Atmospheric PhysicsRussian Academy of SciencesMoscowRussia
  2. 2.Institute of GeosciencesUniversity of KielKielGermany
  3. 3.Leibniz Institute of Marine SciencesUniversity of KielKielGermany

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