Skip to main content

Spatial and Temporal Variation of Temperature and Precipitation in Southwestern China

  • Chapter
  • First Online:
Study on Climate Change in Southwestern China

Part of the book series: Springer Theses ((Springer Theses))

Abstract

Annual and seasonal warming trends in southwestern China during 1961–2008 were significant. About 77% of the 110 stations displayed statistically significant increases of annual temperature. The increase was more apparent in higher altitude areas than in lower ones. Warm–dry flow in summer affected the study region, and the southern extent of the winter monsoon has also been weakened, which in part accounts for some of the climate warming experienced especially in the warmest years in southwestern China. Sunshine hours have a crucial influence on the SB temperature especially during spring and summer, whereas this influence mainly is effective in winter at the Xizang Plateau–Hengduna Mountains and Yunnan–Guizhou Plateau. In addition, the increased net longwave radiation flux over the most areas in the study region and sea surface temperature in Western Pacific may have also made some contributions to temperature rise. Precipitation variations were less marked than those of temperature, generally showing weak decreasing trends during 1961–2008. About 53% of the stations experienced a trend of increasing annual precipitation. Stations with precipitation increases were also mainly at higher altitudes mainly owing to the more water vapor flux, but the significance level was low. Northward penetration of the summer monsoon is limited by an increasing northeasterly air flow over the region, and northwesterly winds in the north are preventing southward transportation of water vapor from the ocean in summer. In addition, the water vapor flux showed a weak variation from the most precipitation years to the least years. These characteristics suggest a weakened monsoonal flow and vapor transportation in recent years, and also partly explain the inconspicuous precipitation variations over southwestern China. In addition, the strengthening Western Pacific Subtropical High also has had some influence on precipitation variations.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 39.99
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 54.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book
USD 54.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

References

  • Beniston, M., & Rebetez, M. (1996). Regional behavior of minimum temperatures in Switzerland for the period 1979–1993. Theoretical and Applied Climatology, 53, 231–243.

    Article  Google Scholar 

  • Bian, D., & Du, J. (2006). Climate variation feature and its effect on environment change in central Tibet from 1961 to 2000. Journal of Applied Meteorological Science, 17(2), 169–175. (in Chinese).

    Google Scholar 

  • Chen, J. Q., et al. (2008). The interannual and interdecadal change of climate during 1951–2000 in Sichuan Basin. Journal of Changjiang Engineering Vocational College, 25(3), 23–25. (in Chinese).

    Google Scholar 

  • Cheng, J. G., & Xie, M. E. (2008). The analysis of regional climate change features over Yunnan in recent 50 years. Advance in Earth Sciences, 27(5), 19–26. (in Chinese).

    Google Scholar 

  • Dong, M. Y. & Wu, Z. F. (2008). Analysis on the spatial and temporal characteristics of temperature change in Northeastern China over the past 50 years. Geology Journals, 30(7), 1093–1199. (in Chinese).

    Google Scholar 

  • Duan, A. M., & Wu, G. X. (2006). Change of cloud amount and the climate warming on the Tibetan Plateau. Geophysical Reseach Letters, 33, L22704.

    Article  Google Scholar 

  • Duan, K. Q., et al. (2002). Response of monsoon rainfall on climate warming from the glacier accumulation in himalayas. Chinese Science Bulletin, 47(19), 1058–1511. (in Chinese).

    Google Scholar 

  • Duan, J. P., et al. (2010). Temperature variability since A.D. 1837 inferred from tree-ring maximum density of abies fabric in Gongga mountains. Chinese Science Bulletin, 55(11), 1036–1042. (in Chinese).

    Google Scholar 

  • Fan, Z. X., et al. (2008). Annual temperature reconstruction in the central Hengduan Mountains, China, as deduced from tree rings. International Journal of Climatology, 28, 1879–1887.

    Article  Google Scholar 

  • Fyfe, J. C., & Flato, G. M. (1999). Enhanced climate change and its detection over the Rocky Mountains. Journal of Climate, 12, 230–243.

    Article  Google Scholar 

  • Hou, S. G, Zhang D. Q. (2003). Comparison of two ice core records since 1954 from Mt. Qomolangma (Everest) Region. Journal of Glaciology and Geocryology. 25(3):256–260. (in Chinese).

    Google Scholar 

  • Hou, S. G., et al. (2002). Recent change in ice cores accumulation rate of Qinghai-Xizang Plateau. Chinese Science Bulletin, 47(20), 1588–1591. (in Chinese).

    Google Scholar 

  • Intergovernmental Panel on Climate Change (IPCC). (2007). Summary for policy makers. In S. Solomon et al. (Eds.) Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change (pp. 1–13). Cambridge: Cambridge University Press.

    Google Scholar 

  • Jia, W. X., et al. (2008). The regional difference and catastrophe of climatic change in Qilian Mt. Region. Journal of Geographical Sciences, 63(3), 257–269. (in Chinese).

    Google Scholar 

  • Jones, P. D., et al. (2008). Urbanization effects in large-scale temperature records, with an emphasis on China. Journal Geophysical Research, 113, D16132.

    Article  Google Scholar 

  • Kang, S. C., et al. (2000). The record of ice core in far east Rongbuk in the north slope of himalayas. Journal of Glaciology and Geocryology, 22(3), 211–217. (in Chinese).

    Google Scholar 

  • Kim, Y. H., & Baik, J. J. (2002). Maximum urban heat island intensity in Seoul. Journal of Applied Meteorology, 41, 651–659.

    Article  Google Scholar 

  • Li, Z. X., et al. (2011). Climate and glacier change in Southwestern China during the past several decades. Environmental Research Letters, 6(2011), 045404. doi:10.1088/1748-9326/6/4/045404.

    Article  Google Scholar 

  • Liu, X. D., & Chen, B. D. (2000). Climatic warming in the Tibetan Plateau during recent decades. International Journal of Climatology, 20, 1729–1742.

    Article  Google Scholar 

  • Liu, X., Cheng, Z., Yan, L., & Yin, Z. Y. (2009). Elevation dependency of recent and future minimum surface air temperature trends in the Tibetan Plateau and its surroundings. Global and Planetary Change, 68(3), 164–174.

    Google Scholar 

  • Morris, C. J. G., et al. (2001). Quantification of the influences of wind and cloud on the nocturnal urban heat island of a large city. Journal of Applied Meteorology, 40(2), 169–182.

    Article  Google Scholar 

  • Qian, Y., et al. (2011). Sensitivity studies on the impacts of Tibetan Plateau snowpack pollution on the Asian hydrological cycle and monsoon climate. Atmospheric Chemistry and Physics, 11, 1929–1948.

    Article  CAS  Google Scholar 

  • Ren, J. W., et al. (2003). Characters of glacier change and the warming and drying climate in the central of Himalaya mountains. Chinese Science Bulletin, 48(23), 2478–2482. (in Chinese).

    Google Scholar 

  • Ren, G., et al. (2008). Urbanization effects on observed surface air temperature trends in north China. Journal of Climate, 21, 1333–1348.

    Article  Google Scholar 

  • Shao, X. M., & Fan, J. M. (1999). Past climate on west Sichuan Plateau as reconstructed from ring-widths of dragon spruce. Quaternary Sciences, 19(1), 81–89. (in Chinese).

    Google Scholar 

  • Song, H. M., et al. (2007). Winter mean lowest temperature derived from tree-ring width in Jiuzhaigou Region, China since 1750A.D. Quaternary Sciences, 27(4), 486–491. (in Chinese).

    Google Scholar 

  • Tang, G. L., et al. (2008). Change of Urban Heat Island Intensity and Its Effect on Surface Mean Air Temperature Records in Southwest China. Journal of Applied Meteorological Science, 19(6), 722–730. (in Chinese).

    Google Scholar 

  • Tang, X. P., et al. (2009). The changing characteristics of total cloud cover observed during 1971–2008 in Xizang Province. Advances in Climate Change Research., 5(6), 343–347. (in Chinese).

    Google Scholar 

  • Wu, J. H., et al. (2008). Variation trend of precipitation and climate factors in Gansu province for the last 50 years. Journal of Arid Land Resources and Environment, 22(11), 24–29. (in Chinese).

    Google Scholar 

  • Yang, L. L., et al. (2006). Infection of Southwest China tourism caused by global climatic change. Journal of Capital Normal University (Natural Sciences Edition), 27(3), 71–86. (in Chinese).

    Google Scholar 

  • Yao, T. D., et al. (2006). Temperature change and oxygen isotope over the past millennium recorded in ice cores from the Tibetan Plateau. Science in China Series D: Earth Sciences, 36(1), 1–8. (in Chinese).

    Article  Google Scholar 

  • Yao, Y. B., et al. (2009). Climatic changes of semi-arid region over the northwest China in recent 50a. Arid Land Geography, 32(2), 159–165. (in Chinese).

    Google Scholar 

  • Zhang, Y. L., et al. (2004). Analysis of 40 year records of solar radiation data in Shanghai, Nanjing and Hangzhou in eastern China. Theoretical and Applied Climatology, 78, 217–227.

    Article  CAS  Google Scholar 

  • Zhang, Y. J., et al. (2007a). The change in the accumulation rate of ice core and the atmospheric circulation in geladandong of Qinghai-Xizang Plateau. Chinese Science Bulletin, 52(20), 2423–2427. (in Chinese).

    Google Scholar 

  • Zhang, Y. J., et al. (2007b). The temperature variation from the records of ice core in geladandong of Qinghai-Xizang Plateau. Journal of Geographical Sciences, 62(5), 501–509. (in Chinese).

    Google Scholar 

  • Zhang, R. B., et al. (2010). Analysis on mean minimum temperature in the east Tibet from autumn to winter in tree ring of the past 400 years. Plateau Meteorology, 29(2), 359–365. (in Chinese).

    Google Scholar 

  • Zhou, L. et al. (2004). Evidence for a significant urbanization effect on climate in China. Proceedings of the National Academy of Sciences of the United States of America, 101(26), 9540–9544.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Zongxing Li .

Rights and permissions

Reprints and permissions

Copyright information

© 2015 Springer-Verlag Berlin Heidelberg

About this chapter

Cite this chapter

Li, Z. (2015). Spatial and Temporal Variation of Temperature and Precipitation in Southwestern China. In: Study on Climate Change in Southwestern China. Springer Theses. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-44742-0_3

Download citation

Publish with us

Policies and ethics