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Climatic Change

, Volume 139, Issue 2, pp 265–278 | Cite as

Enhancement of heavy daily snowfall in central Japan due to global warming as projected by large ensemble of regional climate simulations

  • Hiroaki Kawase
  • Akihiko Murata
  • Ryo Mizuta
  • Hidetaka Sasaki
  • Masaya Nosaka
  • Masayoshi Ishii
  • Izuru Takayabu
Article

Abstract

This study investigates future changes in the accumulated and daily heavy winter snowfall in central Japan and the surrounding regions. We analyze outputs of the 48-member ensemble regional climate simulations in the historical and future climates. In the historical climate simulations, each ensemble member has a 61-year simulation from September 1950 to August 2011. For the future climate simulations, we also conduct 61-year simulations assuming the climate at the end of the twenty-first century (2080–2099) when the global mean surface air temperature is about 4 °C warmer than the pre-industrial climate (1861–1880) as projected under the Representative Concentration Pathway (RCP) 8.5 scenario. Our simulations show that the heavy snowfall occurring at a frequency of every 10 years is enhanced in the inland areas of the central part of the Japanese archipelago (central Japan) where the total winter snowfall amount decreases significantly. Heavy snowfall is also intensified in the northern part of the Asian continent where the surface air temperature is much colder than over central Japan. A composite analysis of heavy snowfall events in central Japan indicates that such events occur when the Japan Sea polar air mass convergence zone (JPCZ) appears during the East Asian winter monsoon season. In the future climate projections, the JPCZ is intensified since the warm ocean supplies more moisture due to warming. An upward wind anomaly is also found over the windward side of mountains where the upward flow is prevalent climatologically. The intensification of both the JPCZ and the upward wind over the mountain ranges result in the enhancement of heavy snowfall in inland areas where the surface air temperature is still below 0 °C.

Keywords

Ensemble Member Couple Model Intercomparison Project Phase Climate Simulation East Asian Winter Monsoon Snow Water Equivalent 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

Notes

Acknowledgments

We thank all members of MRI, AORI, NIES, DPRI, JAMSTEC, and the University of Tsukuba, who built up d4PDF. The Earth Simulator was used in this study as a “Strategic Project with Special Support” of JAMSTEC. Also, the study was supported by the Program for Risk Information on Climate Change (SOUSEI) and the Data Integration and Analysis System (DIAS), both of which are sponsored by the Ministry of Education, Culture, Sports, Science and Technology of Japan. This study was partly supported by JSPS KAKENHI Grant Number 26750111. The dataset of d4PDF is available from the website of DIAS (http://www.editoria.u-tokyo.ac.jp/projects/dias.old2/?locale=en).

Supplementary material

10584_2016_1781_MOESM1_ESM.docx (42 kb)
ESM 1 (DOCX 41 kb)
10584_2016_1781_MOESM2_ESM.pdf (1.7 mb)
ESM 2 (PDF 1746 kb)
10584_2016_1781_MOESM3_ESM.docx (43 kb)
ESM 3 (DOCX 43 kb)

References

  1. Armstrong RL, Brun E (eds) (2008) Snow and climate: physical processes, surface energy exchange and modeling. Cambridge University Press, Cambridge, 222 ppGoogle Scholar
  2. Brown RD, Mote P (2009) The response of Northern Hemisphere snow cover to a changing climate. J Clim 22:2124–2145CrossRefGoogle Scholar
  3. Burnett AW, Kirby ME, Mullins HT, Patterson WP (2003) Increasing Great Lake-effect snowfall during the twentieth century: a regional response to global warming? J Clim 16:3535–3542CrossRefGoogle Scholar
  4. Collins M, Knutti R, Arblaster J, et al. (2013) Long-term climate change: projections, commitments and irreversibility. In: Stocker TF et al. (eds) Climate Change 2013: The Physical Science Basis, Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, chap. 12. Cambridge Univ. Press, CambridgeGoogle Scholar
  5. de Vries H, Lenderink G, van Meijgaard E (2014) Future snowfall in western and central Europe projected with a high-resolution regional climate model ensemble. Geophys Res Lett 41:4294–4299. doi: 10.1002/2014GL059724 CrossRefGoogle Scholar
  6. Gula J, Peltier RW (2012) Dynamical downscaling over the Great Lakes basin of North America using the WRF regional climate model: the impact of the Great Lakes system on regional greenhouse warming. J Clim 25:7723–7742CrossRefGoogle Scholar
  7. Heo KY, Ha KJ (2008) Snowstorm over the southwestern coast of the Korean Peninsula associated with the development of mesocyclone over the Yellow Sea. Adv Atmos Sci 25(5):765–777. doi: 10.1007/s00376-008-0765-2 CrossRefGoogle Scholar
  8. Hirahara S, Ishii M, Fukuda Y (2014) Centennial-Scale Sea surface temperature analysis and its uncertainty. J Clim 27:57–75. doi: 10.1175/JCLI-D-12-00837.1 CrossRefGoogle Scholar
  9. Hjelmfelt MR (1990) Numerical study of the influence of environmental conditions on lake-effect snowstorms over Lake Michigan. Mon Weather Rev 118:138–150CrossRefGoogle Scholar
  10. Ishizaki NN, Takayabu I, Oh’izumi M, et al. (2012) Improved performance of simulated Japanese climate with a multi-model ensemble. J Meteorol Soc Jpn 90:235–254CrossRefGoogle Scholar
  11. Kawase H, Hara M, Yoshikane T, et al. (2013) Altitude dependence of future snow cover changes over Central Japan evaluated by a regional climate model. J Geophys Res 118:12444–12457. doi: 10.1002/2013JD020429 Google Scholar
  12. Kawase H, Suzuki C, Ishizaki NN, et al. (2015a) Simulations of monthly variation in snowfall over complicated mountainous areas around Japan’s Northern Alps. SOLA 11:138–143. doi: 10.2151/sola.2015-032 CrossRefGoogle Scholar
  13. Kawase H, Sasaki H, Murata A, et al. (2015b) Future changes in winter precipitation around Japan projected by ensemble experiments using NHRCM. J Meteorol Soc Jpn 93:571–580. doi: 10.2151/jmsj.2015-034 CrossRefGoogle Scholar
  14. Lim K-S, Hong S-Y (2007) Numerical simulation of heavy snowfall over the Ho-Nam province of Korea in December 2005. J Korean Meteorol Soc 43:161–173Google Scholar
  15. Lute AC, Abatzoglou JT, Hegewisch KC (2015) Projected changes in snowfall extremes and interannual variability of snowfall in the western United States. Water Resour Res 51:960.972. doi: 10.1002/2014WR016267 CrossRefGoogle Scholar
  16. Ma X, Yoshikane T, Hara M, et al. (2010) Hydrological response to future climate change in the Agano River basin, Japan. Hydrol Res Lett 4:25–29Google Scholar
  17. Manabe S (1957) On the modification of air-mass over the Japan Sea when the outburst of cold air predominates. J Meteorol Soc Jpn 35:311–326Google Scholar
  18. Mizuta R, Yoshimura H, Murakami H, et al. (2012) Climate simulations using MRI-AGCM with 20-km grid. J Meteorol Soc Jpn 90(A):233–258CrossRefGoogle Scholar
  19. Mizuta R, Arakawa O, Ose T, et al. (2014) Classification of CMIP5 future climate responses by the tropical sea surface temperature changes. SOLA 10:167–171. doi: 10.2151/sola.2014-035 CrossRefGoogle Scholar
  20. Nagata M, Ikawa M, Yoshizumi S, Yoshida T (1986) On the formation of a convergent cloud band over the Japan Sea in winter; numerical experiments. J Meteorol Soc Jpn 64:841–855Google Scholar
  21. Notaro M, Bennington V, Vavrus S (2015) Dynamically downscaled projections of lake-effect snow in the Great Lakes basin. J Clim 28:1661–1684. doi: 10.1175/JCLI-D-14-00467.1 CrossRefGoogle Scholar
  22. O’Gorman PA (2014) Contrasting responses of mean and extreme snowfall to climate change. Nature 512(7515):416–418CrossRefGoogle Scholar
  23. Peace RL, Sykes RB Jr. (1966) Mesoscale study of a lake-effect snowstorm. Mon Weather Rev 94(8):495–507CrossRefGoogle Scholar
  24. Räisänen J, Eklund J (2012) Twenty-first century changes in snow climate in northern Europe: A high-resolution view from ENSEMBLES regional climate models. Clim Dyn 38:2575–2591. doi: 10.1007/s00382-011-1076-3 CrossRefGoogle Scholar
  25. Rasmussen R, Liu C, Ikeda K, et al. (2011) High-resolution coupled climate runoff simulations of seasonal snowfall over Colorado: a process study of current and warmer climate. J Clim 24:3015–3048CrossRefGoogle Scholar
  26. Sasaki H, Kurihara K, Takayabu I, Uchiyama T (2008) Preliminary experiments of reproducing the present climate using the non-hydrostatic regional climate model. SOLA 4:25–28. doi: 10.2151/sola.2008-007 CrossRefGoogle Scholar
  27. Shi X, Durran DR (2015) Estimating the response of extreme precipitation over midlatitude mountains to global warming. J Clim 28(10):4246–4262CrossRefGoogle Scholar
  28. Siler N, Roe G (2014) How will orographic precipitation respond to surface warming? An idealized thermodynamic perspective. Geophys Res Lett 41. doi: 10.1002/2013GL059095
  29. Steenburgh WJ, Halvorson SF, Onton DJ (2000) Climatology of lake-effect snowstorms of the Great Salt Lake. Mon Weather Rev 128:709–727CrossRefGoogle Scholar
  30. Steger C, Kotlarski S, Jonas T, Schär C (2012) Alpine snow cover in a changing climate: a regional climate model perspective. Clim Dyn 41:735–754. doi: 10.1007/s00382-012-1545-3 CrossRefGoogle Scholar
  31. Steiger SM, Schrom R, Stamm A, et al. (2013) Circulations, bounded weak echo regions, and horizontal vortices observed within long-lake-axis-parallel-lake-effect storms by the Doppler on wheels. Mon Weather Rev 141(8):2821–2840CrossRefGoogle Scholar
  32. Sun J, Wang H, Yuan W, Chen H (2010) Spatial-temporal features of intense snowfall events in China and their possible change. J Geophys Res 115:D16110. doi: 10.1029/2009JD013541 CrossRefGoogle Scholar
  33. Vaughan DG, Comiso JC, Allison I, et al. (2013) Observations: cryosphere. In: Stocker TF et al. (eds) Climate Change 2013: The Physical Science Basis, Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, chap. 4. Cambridge Univ. Press, CambridgeGoogle Scholar
  34. Wi S, Dominguez F, Durcik M, Valdes J, et al. (2012) Climate change projection of snowfall in the Colorado River Basin using dynamical downscaling. Water Resour Res 48:W05504. doi: 10.1029/2011WR010674 CrossRefGoogle Scholar

Copyright information

© Springer Science+Business Media Dordrecht 2016

Authors and Affiliations

  • Hiroaki Kawase
    • 1
  • Akihiko Murata
    • 1
  • Ryo Mizuta
    • 1
  • Hidetaka Sasaki
    • 1
  • Masaya Nosaka
    • 1
  • Masayoshi Ishii
    • 1
  • Izuru Takayabu
    • 1
  1. 1.Meteorological Research InstituteJapan Meteorological AgencyIbarakiJapan

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