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The significant relationship between the Arctic Oscillation (AO) in December and the January climate over South China

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Abstract

Using NCEP/NCAR reanalysis data, the China rainfall and surface temperature data of the China Meteorological Administration, and the Arctic Oscillation (AO) indices of NOAA, the author investigates relationships between the AO and the precipitation and temperature over China. There exists a good relationship between the AO index in December and the succeeding January precipitation over South China, indicating that when the December AO index is positive (negative), the January precipitation over South China increases (decreases). A remarkable negative correlation between the December AO index and the January surface temperature also exists over South China, indicating that when the December AO index is positive (negative), the January temperature over South China drops (rises). The occurrence of this anomalous climate is related to the anomalies of the atmospheric circulation systems. The December AO greatly influences circulation anomalies in January. A positive phase of the AO is found to lead to a stronger subtropical jet over the south side from the Iran Plateau to the Tibetan Plateau. Consequently, it results in a deepening pressure trough around the Bay of Bengal, which transports the warm and wet air to South China continuously. The Siberian High in January is stronger and extends farther southeastward. It results in continual cold air at 1000 hPa pouring into South China, inducing low temperature. Cooperating with the trough of the Bay of Bengal, anomalous precipitation occurs over South China. For the negative phase of the December AO, the opposite situation is observed.

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References

  • Chen, J., and S. Q. Sun, 1999: Eastern Asian winter monsoon anomaly and variation of global circulation. Part II: Influence on SST by winter monsoon. Chinese J. Atmos. Sci., 23(3), 286–295. (in Chinese)

    Google Scholar 

  • Chen, W., and L. H. Kang, 2006: Linkage between the Arctic Oscillation and winter climate over East Asia on the interannual timescale: Roles of quasistationary planetary waves. Chinese J. Atmos. Sci., 30, 863–870. (in Chinese)

    Google Scholar 

  • Chun, H., and J. H. He, 2003: Relation between Arctic Oscillation and North China air temperature in winter. Journal of Nanjing Institute of Meteorology, 26(1), 1–7. (in Chinese)

    Google Scholar 

  • Clark, M. P., and M. C. Serreze, 2000: Effects of variations in East Asian snow cover on modulating atmospheric circulation over the North Pacific Ocean. J. Climate, 13, 3700–3710.

    Article  Google Scholar 

  • Ding, Y. H., 1990: Build up, air mass transformation and propagation of Siberian High and its relation to cold surge in East Asia. Meteor. Atmos. Phys., 44, 281–292.

    Article  Google Scholar 

  • Fyfe, J. C., J. Boer, and G. M. Flato, 1999: The Arctic and Antarctic oscillation and their projected changes under global warming. Geophys. Res. Lett., 26(11), 1601–1604.

    Article  Google Scholar 

  • Gong, D. Y., and C. H. Ho, 2002: The Siberian High and climate change over middle to high latitude Asia. Theoretical and Applied Climatology, 72, 1–9.

    Article  Google Scholar 

  • Gong, D. Y., and S. W. Wang, 2003: Influence of Arctic Oscillation on winter climate over China. Journal of Geographical Sciences, 13(2), 208–216.

    Article  Google Scholar 

  • Gong, D. Y., S. W. Wang, and J. H. Zhu, 2001: East Asian winter monsoon and Arctic Oscillation. Geophys. Res. Lett., 28, 2073–2076.

    Article  Google Scholar 

  • Gong, D. Y., J. H. Zhu, and S. W. Wang, 2002: Significant relationship between spring AO and the summer rainfall along the Yangtze River. Chinese Science Bulletin, 47(11), 948–951.

    Article  Google Scholar 

  • Gong, D. Y., S. W. Wang, and J. H. Zhu, 2004a: Arctic Oscillation influence on daily temperature variance in winter over China. Chinese Science Bulletin, 49(6), 637–642.

    Article  Google Scholar 

  • Gong, G., D. Entekhabi, and J. Cohen, 2003: Modeled Northern Hemisphere winter climate response to realistic Siberian snow anomalies. J. Climate, 16, 3917–3931.

    Article  Google Scholar 

  • Gong, G. D., Entekhabi, J. Cohen, and D. Robinson, 2004b: Sensitivity of atmospheric response to modeled snow anomaly characteristics. J. Geophys. Res., 109, doi: 10.1029/2003JD004160.

  • Guo, Q. Y., 1994: Relationship between the variations of East Asian winter monsoon and temperature anomalies in China. Journal of Applied Meteorological Science, 5(2), 218–225. (in Chinese)

    Google Scholar 

  • Huang, J. Y., B. K. Tan, L. L. Suo, and Y. Y. Hu, 2007: Monthly changes in the influence of the Arctic Oscillation on surface air temperature over China. Adv. Atmos. Sci., 24(5), 799–807.

    Article  Google Scholar 

  • Ji, L. R., C. L. Bueh, N. Shi, and Z. W. Xie, 2008: On the medium-range process of the rainy, snowy and cold weather of South China in early 2008. Part III: pressure trough over the Tibetan Plateau/Bay of Bengal. Climatic and Environmental Research, 13(4), 446–458. (in Chinese)

    Google Scholar 

  • Ju, J. H., J. Z. Ren, and J. M. Lü, 2004: Effect of interdecadal variation of Arctic Oscillation on temperature increasing in north of East Asian winter. Plateau Meteorology, 23(4), 429–434. (in Chinese)

    Google Scholar 

  • Ju, J. H., J. M. Lü, J. Cao, and J. Z. Ren, 2005: Possible impacts of the Arctic Oscillation on the interdecadal variation of summer monsoon rainfall in East Asia. Adv. Atmos. Sci., 22(1), 39–48.

    Article  Google Scholar 

  • Kalnay, E., and Coauthors, 1996: The NCEP/NCAR 40-Year Reanalysis Project. Bull. Amer. Meteor. Soc., 77, 437–471.

    Article  Google Scholar 

  • Kumar, A., and F. Yang, 2003: Comparative influence of snow and SST variability on extratropical climate in Northern winter. J. Climate, 16, 2248–2261.

    Article  Google Scholar 

  • Li, C., D. H. Luo, Z. F. Fang, and H. F. Zhou, 2005a: Linkage of inter-decadal variations of the Arctic Oscillation and summer precipitation over North China. Journal of Nanjing Institute of Meteorology, 28(6), 755–762. (in Chinese)

    Google Scholar 

  • Li, C. Y., and Z. X. Long, 1998: AGCM Numerical simulation on atmospheric memory. Climatic and Environmental Research, 3, 193–200. (in Chinese)

    Google Scholar 

  • Li, C. Y., H. Yang, and W. Gui, 2008a: Cause of severe weather with cold air, freezing rain and snow over South China in January 2008. Climatic and Environmental Research, 13(2), 113–122. (in Chinese)

    Google Scholar 

  • Li, J., R. C. Yu, T. J. Zhou, and B. Wang, 2005b: Why is there an early Spring cooling shift downstream of the Tibetan Plateau, J. Climate, 18(22), 4660–4668.

    Article  Google Scholar 

  • Li, J., R. C. Yu, and T. J. Zhou, 2008b: Teleconnection between NAO and climate downstream of the Tibetan Plateau. J. Climate, 21, 4680–4690.

    Article  Google Scholar 

  • Mao, R., D. Y. Gong, and Q. M. Fang, 2007: Influences of the East Asian jet stream on winter climate in China. Journal of Applied Meteorological Science, 18(2), 137–146. (in Chinese)

    Google Scholar 

  • Sun, S. Q., and J. Chen, 2000: The variations of wind and thermodynamics fields in the South China Sea in summer during the anomaly winter monsoon. Climatic and Environmental Research, 5(4), 400–416. (in Chinese)

    Google Scholar 

  • Suo, L. L., J. Y. Huang, and B. K. Tan, 2008: The influence of winter arctic oscillation on maximum and minimum air temperature over China in winter. Journal of Tropical Meteorology, 24(2), 163–168. (in Chinese)

    Google Scholar 

  • Thompson, D. W. J., and J. M Wallace, 1998: The Arctic Oscillation signature in the wintertime geopotential height and temperature fields. Geophys. Res. Lett., 25, 1297–1300.

    Article  Google Scholar 

  • Thompson, D. W. J., and J. M. Wallace, 2001: Regional climate impacts of the Northern Hemisphere annular mode and associated climate trends. Science, 293(5527), 85–89.

    Article  Google Scholar 

  • Wang, X. J., and F. Z. Fang, 2004: Surface air temperature in China and its relation to Arctic Oscillation index. Plateau Meteorology, 24, 429–434. (in Chinese)

    Google Scholar 

  • Wu, B. Y., and J. Wang, 2002a: Possible impacts of winter Arctic Oscillation on Siberian High, the East Asian winter monsoon and sea-ice extent. Adv. Atmos. Sci., 19, 297–320.

    Article  Google Scholar 

  • Wu, B. Y., and J. Wang, 2002b: Winter Arctic Oscillation, Siberian High and East Asian winter monsoon. Geophys. Res. Lett., 29, 1897, doi: 1810.1029/2002GL015373.

    Article  Google Scholar 

  • Xin, X. G., R. C. Yu, T. J. Zhou, and B. Wang. 2006: Drought in late spring of South China in recent decades. J. Climate, 19(13), 3197–3206.

    Article  Google Scholar 

  • Xin, X. G., T. J. Zhou, and R. C. Yu, 2010: Increased Tibetan Plateau snow depth_An indicator of the connection between enhanced winter NAO and latespring tropospheric cooling over East Asia. Adv. Atmos. Sci., 27(4), 788–794, doi: 10.1007/s00376-009-9071-x.

    Article  Google Scholar 

  • Yang, H., and C. Y. Li, 2008: Influence of Arctic Oscillation in winter. Climatic and Environmental Research, 13(4), 395–404. (in Chinese)

    Google Scholar 

  • Yang, S., K. M. Lau, and K. M. Kim, 2002: Variations of the East Asian jet stream and Asian-Pacific-American winter climate anomalies. J. Climate, 15, 306–325.

    Article  Google Scholar 

  • Yu, R. C., and T. J. Zhou, 2004: Impacts of winter-NAO on March cooling trends over subtropical Eurasia continent in the recent half century. Geophys. Res. Lett., 31, L12204, doi: 10.1029/2004GL019814.

    Article  Google Scholar 

  • Yu, R. C., and T. J. Zhou, 2007: Seasonality and threedimensional structure of the interdecadal change in East Asian monsoon. J. Climate, 20, 5344–5355.

    Article  Google Scholar 

  • Zhang, P. Z., and G. M. Chen, 1999: A statistical analysis of the cold wave high which influences on China. Acta Meterologica Sinica, 57(4), 493–501. (in Chinese)

    Google Scholar 

  • Zhang, Z. Y., D. Y. Gong, M. Hu, D. Guo, X. Z. He, and Y. N. Lei, 2009: Anomalous winter temperature and precipitation events in southern China. Journal of Geographical Sciences, 19(4), 471–488, doi: 10.1007/s11442-009-0471-8.

    Article  Google Scholar 

  • Zhou, T. J., and J. Li, 2008: Climate change in China congruent with the linear trends of the annular modes. Atmos. Oceanic Sci. Lett., 1, 1–7.

    Google Scholar 

Download references

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Authors and Affiliations

  1. State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China

    Hui Yang  (杨 辉)

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  1. Hui Yang  (杨 辉)
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Correspondence to Hui Yang  (杨 辉).

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Yang, H. The significant relationship between the Arctic Oscillation (AO) in December and the January climate over South China. Adv. Atmos. Sci. 28, 398–407 (2011). https://doi.org/10.1007/s00376-010-0019-y

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  • DOI: https://doi.org/10.1007/s00376-010-0019-y

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