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Variations of winter precipitation over southeastern China in association with the North Atlantic Oscillation

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Abstract

The synoptic-scale winter precipitation variations over southeastern China (22°–32°N, 105°–125°E) and their association with the North Atlantic Oscillation (NAO) during 1951–2007 are investigated in this paper. The variability of wintertime precipitation is characterized by meridional displacement of its maximum center. Two precipitation regimes, with maximum centers located over the Yangtze and Pearl River basins, are identified via cluster analysis. Time-lagged analyses suggest that the two precipitation regimes are connected with the decaying phases of positive NAO (NAO+) events of different amplitudes. A strong (medium) NAO+ event is defined as one when the maximum amplitude of the NAO index exceeds 1.0 (in the range of 0.7–1.0) for at least 4 consecutive days and drops to less than 0.3 within 7 days following the peak index. After the peak of a strong NAO+, southerly winds expand northward to the Yangtze River (about 30°N), a northeast–southwest-tilted trough migrates to east of Lake Baikal, and cold air intrudes into central eastern China; thus, precipitation is strengthened over the Yangtze River basin where warm and cold air masses converge. In comparison, during the decaying phase of medium NAO+ events, the southerly winds are relatively weak, and precipitation tends to be enhanced at lower latitudes (around 25°N). Further analysis indicates that downstream Rossby-wave propagation may account for the latitudinal expansion of the southerly wind anomalies over the eastern coastal area of China during the decaying phase of NAO+ events of different strengths.

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Authors and Affiliations

  1. Zhejiang Provincial Meteorological Observatory, Hangzhou, 310017, China

    Maoyuan Lou, Chao Li & Shifeng Hao

  2. Zhejiang Institute of Meteorological Sciences, Hangzhou, 310008, China

    Chao Li

  3. Zhejiang Meteorological Service Center, Hangzhou, 310017, China

    Juan Liu

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  1. Maoyuan Lou
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  2. Chao Li
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  3. Shifeng Hao
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  4. Juan Liu
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Correspondence to Chao Li.

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Supported by the National Natural Science Foundation of China (41405047 and 41675086) and China Meteorological Administration Special Public Welfare Research Fund (GYHY201306010).

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Lou, M., Li, C., Hao, S. et al. Variations of winter precipitation over southeastern China in association with the North Atlantic Oscillation. J Meteorol Res 31, 476–489 (2017). https://doi.org/10.1007/s13351-017-6103-9

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