Vol.35, NO.3, 2024
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Article Navigation >  Journal of Applied Meteorological Science  > 2024  >  35(3): 298-310
Wang Miaomiao, Ding Minghu, Lü Junmei, et al. Climatology of winter cold waves and associated atmospheric circulation anomalies in China during the last 40 years. J Appl Meteor Sci, 2024, 35(3): 298-310. DOI:  10.11898/1001-7313.20240304.
Citation: Wang Miaomiao, Ding Minghu, Lü Junmei, et al. Climatology of winter cold waves and associated atmospheric circulation anomalies in China during the last 40 years. J Appl Meteor Sci, 2024, 35(3): 298-310. DOI:  10.11898/1001-7313.20240304.
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Climatology of Winter Cold Waves and Associated Atmospheric Circulation Anomalies in China During the Last 40 Years

DOI: 10.11898/1001-7313.20240304
  • 1.

    State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081

  • 2.

    Xiong'an Atmospheric Boundary Layer Key Laboratory, CMA, Xiong'an New Area 071000

  • Received Date: 2024-02-24
  • Rev Recd Date: 2024-04-22
  • Publish Date: 2024-05-31
    Abstract
  • Based on daily high-resolution temperature observations at 1941 meteorological stations in China from 1980 to 2023, stations reaching standard for cold wave and 418 cold wave processes (including 152 strong cold waves processes) in winter are identified according to the monitoring indices of cold air processes. And cold wave processes are objectively classified according to their intensity and influencing areas using K-means++ clustering method. The temporal and spatial characteristics of the single-station cold waves and 418 cold wave events are discussed. Results show that the frequency of cold waves in the high affecting areas of China has not increased significantly but has shown a decreasing trend over the last 40 years. The increasing trend of frequency and intensity of single-station cold waves in the middle-lower reaches of the Yangtze River Plain is significant. Additionally, the intensity of single-station cold waves in South China is also noticeably enhanced. The frequency of winter cold wave events in China has decreased significantly in the last 40 years with an expanding range of influence, while the intensity of strong cold wave events has increased significantly, accompanied by a marked increase in the amplitude of interannual variations. The cold air associated with cold waves in China mainly originates from the southeast of Novaya Zemlya, and its trajectory varies depending on the type of cold wave. Based on the fifth-generation European Centre for Medium-Range Weather Forecasts (ECMWF) atmospheric reanalysis data (ERA5), characteristics of atmospheric circulation anomalies in the preceding and the simultaneous period for cold wave processes in the countrywide, Northeast-North China and Northwest-North China are analyzed. It is found that the deep warm high pressure in Greenland is an important precursor of the countrywide cold wave, and the zonal wave train in the middle and upper troposphere of Eurasia is a prominent feature of the cold wave outbreak. The cold wave in Northeast-North China is related to the eastward movement of the cold vortex under the block of anomalous high-pressure system in the mid-low latitudes. The cold wave in Northwest-North China is closely related to the development of a warm high ridge over the East European Plain and the circulation situation of two-ridge-one-trough in mid-high latitudes of Eurasia. All types of cold waves are preceded by the maintenance of the Ural blocking high and the accumulation of cold air in Siberia.
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  • Fig. 1  Composites of the daily maximum temperature drops within 24 hours (the shaded) at their peak days for six types of cold waves (the shaded denotes temperature drops passing the test of 0.05 level, the red dot denotes frequency of single-station cold waves) (a)countrywide, (b)Northeast-North China, (c)Northwest-North China, (d)East China, (e)Northeast-Southwest China, (f)Southwest China

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    Fig. 2  Trajectories of cold air for 418 cold waves (the thick red line denotes cold air trajectory composited by the minimum value of 2 m temperature negative anomalies, green and the purple dots denote starting and ending of trajectories, respetively) (a)countrywide, (b)Northeast-North China, (c)Northwest-North China, (d)East China, (e)Northeast-Southwest China, (f)Southwest China

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    Fig. 3  Spatial distribution of single-station cold wave frequency and linear trend coefficient in China during 1980-2022 (the red dot denotes passing the test of 0.05 level) (a)climate mean of cold wave frequency, (b)the maximum frequency of cold wave, (c)linear trend coefficients of cold wave frequency, (d)linear trend coefficients of the maximum temperature drops within 48 hours

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    Fig. 4  Interannual variation of cold waves in China from 1980 to 2022 (a)frequency, (b)cold air process intensity index

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    Fig. 5  Composites of 500 hPa geopotential height (the contour, unit:gpm) and its anomalies (the shaded) for countrywide cold waves (the contour interval is 40 gpm and the thick line denotes 5440 gpm, the black dot denotes anomalies passing the test of 0.05 level)

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    Fig. 6  The same as in Fig. 5, but for cold waves in Northeast-North China (the contour interval is 30 gpm)

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    Fig. 7  The same as in Fig. 5, but for cold waves in Northwest-North China

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  • [1]
    Song Y L, Zhou G S, Guo J P, et al. Freezing injury of winter wheat in Northern China and delaying sowing date to adapt. J Appl Meteor Sci, 2022, 33(4): 454-465. doi:  10.11898/1001-7313.20220406
    [2]
    Tao S Y. China's research on the cold wave in East Asia in the past decade. Acta Meteor Sinica, 1959, 17(3): 226-230. https://www.cnki.com.cn/Article/CJFDTOTAL-QXXB195903006.htm
    [3]
    Xu G H. Medium-term forecast scheme of cold wave. Meteor Mon, 1985, 11(2): 6-10. https://www.cnki.com.cn/Article/CJFDTOTAL-QXXX198502001.htm
    [4]
    Zhu Q G. Lin J R, Shou S W, et al. Principles and Methods of Meteorology(3rd Ed). Beijing: China Meteorological Press, 2000: 269-319.
    [5]
    Ding Y H. The propagation of the winter monsoon during cold air outbreaks in East Asia and the associated planetary-scale effect. Q J Appl Meteor, 1991, 2(2): 124-132. http://qikan.camscma.cn/article/id/19910218
    [6]
    Qiu Y K, Li X D, Qiu Y Y. Statistical features of the cold waves invaded China and their relation to the snow cover area over the Eurasian continent. Q J Appl Meteor, 1992, 3(2): 235-241. http://qikan.camscma.cn/article/id/19920239
    [7]
    Zhang P Z, Ding Y H, Guo C S, et al. Study on potential vorticity diagnosis of cold wave high pressure in East Asia. Q J Appl Meteor, 1994, 5(1): 49-56. http://qikan.camscma.cn/article/id/19940109
    [8]
    Wei F Y. Variation characteristics of cold wave disasters in China under the background of climate warming. Progress in Natural Science, 2008, 18(3): 289-295. https://www.cnki.com.cn/Article/CJFDTOTAL-ZKJZ200803007.htm
    [9]
    Zhu J T, Lu Y, Li Y. Study on interdecadal variations of cold wave and genesis of atmospheric circulation in the Chinese Mainland from 1970 to 2019. J Lanzhou Univ Nat Sci, 2022, 58(3): 337-346;355. https://www.cnki.com.cn/Article/CJFDTOTAL-LDZK202203007.htm
    [10]
    Ma L, Wei Z G, Li X R, et al. Comparative analysis of the cold surge characteristics over China before and after 2000. J Glaciol Geocryol, 2022, 44(6): 1757-1772. https://www.cnki.com.cn/Article/CJFDTOTAL-BCDT202206008.htm
    [11]
    Wang Z Y, Ding Y H. Climate change of the cold wave frequency of China in the last 53 years and the possible reasons. Chinese J Atmos Sci, 2006, 30(6): 1068-1076. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200606001.htm
    [12]
    Qian W H, Zhang W W. Changes in cold wave events and warm winter in China during the last 46 years. Chinese J Atmos Sci, 2007, 31(6): 1266-1278. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200706022.htm
    [13]
    Zhou L, Sun Z B. Activity characteristics of cold air in China from 1961 to 2010. Trans Atmos Sci, 2015, 38(3): 342-353. https://www.cnki.com.cn/Article/CJFDTOTAL-NJQX201503006.htm
    [14]
    Li H Y, Lin S, Wang Y P, et al. Characteristics of cold wave activities in Beijing-Tianjin-Hebei Region from 1961 to 2017. J Arid Meteor, 2022, 40(1): 41-48. https://www.cnki.com.cn/Article/CJFDTOTAL-GSQX202201005.htm
    [15]
    Li F, Li J, Lin R, et al. Interdecadal variation of cold wave characteristics and its relationship with influencing factors in Northeast China. Acta Agric Jiangxi, 2022, 34(7): 142-149. https://www.cnki.com.cn/Article/CJFDTOTAL-JXNY202207024.htm
    [16]
    Liu M J, Li Y, Sun M P. Spatial-temporal variation of cold wave frequency and its influencing factors of circulation in Hexi Corridor during 1961-2018. J Glaciol Geocryol, 2020, 42(3): 801-811. https://www.cnki.com.cn/Article/CJFDTOTAL-BCDT202003008.htm
    [17]
    Xiao H R, Long K J, Wu Q, et al. Temperature changes of cold wave in Sichuan Basin from 1980 to 2017. Plateau Mt Meteor Res, 2020, 40(4): 47-52. https://www.cnki.com.cn/Article/CJFDTOTAL-SCCX202004008.htm
    [18]
    Song Y L. Global research progress of drought indices. J Appl Meteor Sci, 2022, 33(5): 513-526. doi:  10.11898/1001-7313.20220501
    [19]
    Ren S L, Niu N, Qin D Y, et al. Extreme cold and snowstorm event in North America in February 2021 based on satellite data. J Appl Meteor Sci, 2022, 33(6): 696-710. doi:  10.11898/1001-7313.20220605
    [20]
    He L F, Chyi D, Yu W. Development mechanisms of the Yellow Sea and Bohai Sea cyclone causing extreme snowstorm in Northeast China. J Appl Meteor Sci, 2022, 33(4): 385-399. doi:  10.11898/1001-7313.20220401
    [21]
    Wu B Y, Yang K, Francis J A. A cold event in Asia during January-February 2012 and its possible association with Arctic Sea ice loss. J Climate, 2017, 30(19): 7971-7990.
    [22]
    Wu B Y. Two extremely cold events in East Asia in January of 2012 and 2016 and their possible associations with Arctic warming. Trans Atmos Sci, 2019, 42(1): 14-27. https://www.cnki.com.cn/Article/CJFDTOTAL-NJQX201901003.htm
    [23]
    Zhang L, Lü J M, Ding M H. Impact of Arctic extreme cyclones on cold spells in China during early 2015. J Appl Meteor Sci, 2020, 31(3): 315-327. doi:  10.11898/1001-7313.20200306
    [24]
    Hersbach H, Bell B, Berrisford P, et al. The ERA5 global reanalysis. Q J R Meteor Soc, 2020, 146(730): 1999-2049.
    [25]
    National Technical Committee on Standardization of Climate and Climate Change. Monitoring Indices of Cold Air Processes QX/T 393-2017. Beijing: China Meteorological Press, 2017.
    [26]
    National Climate Center. Atlas of Hazardous Weather and Climate in China(1961-2015). Beijing: China Meteorological Press, 2018.
    [27]
    Peng J B, Bueh C. The definition and classification of extensive and persistent extreme cold events in China. Atmos Ocean Sci Lett, 2011, 4(5): 281-286.
    [28]
    Bueh C, Peng J B, Xie Z W, et al. Recent progresses on the studies of wintertime extensive and persistent extreme cold events in China and large-scale tilted ridges and troughs over the Eurasian continent. Chinese J Atmos Sci, 2018, 42(3): 656-676. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXK201803014.htm
    [29]
    Peng J B, Sun S Q. The relationship between persistent cold spell in Southern China and the variation mode of East Asian winter monsoon with opposite signs in the north and south. Chinese J Atmos Sci, 2017, 41(4): 691-701. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXK201704003.htm
    [30]
    Zhang Z C, Zhou F, Zhang H X, et al. Predication of typical winter circulation systems based on BCC_CSM1.1m model. J Appl Meteor Sci, 2023, 34(1): 27-38. doi:  10.11898/1001-7313.20230103
    [31]
    Fang Y H, Lin Y T, Zhao C Y, et al. Two types of cold waves affecting Northeast China and the corresponding different key regions of precedent sea ice and sea surface temperature. Int J Climatol, 2022, 42(16): 10451-10463.
    [32]
    Liang K, Li L P, Ren J H, et al. Synergistic effects of mid-latitude sea surface temperature on intensity anomalies of cold waves in winter of Northern China. Plateau Meteor, 2023, 42(3): 711-724. https://www.cnki.com.cn/Article/CJFDTOTAL-GYQX202303015.htm
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    • Received : 2024-02-24
    • Accepted : 2024-04-22
    • Published : 2024-05-31
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