Abstract
Strong rainfall events originated from the northeast (NE) and southwest (SW) directions of the plain area of Beijing City (BJP) over 8 recent warm seasons (May-September of 2009–2016) were analyzed by using hourly merged rainfall, satellite brightness temperature, and the fifth-generation ECMWF reanalysis (ERA5) data. Such heavy regional rainfall events (RREs) with different origins present quite different features in both the precipitation itself and its corresponding circulations. The heavy RREs originated from the SW occur more frequently in the flood season of North China (July and August), and the peak time of rainfall occurrences is in the early morning. They are linked with stronger large-scale circulation forcing, compared with the NE-originated events. Meanwhile, the ratio of heavy rainfall to the total rainfall in SW-originated events, the mean spatial coverage of rainfall, and associated convective index, are also larger, for the SW events. The heavy RREs from the NE occur more frequently in June and July (before the traditional flood season), with a more apparent afternoon peak. They exhibit stronger convective features, with higher maximum convective index values, but the large-scale forcing is weaker at the hour of onset. These features of the RREs from different directions of Beijing City and associated precursor circulation signals help better forecast RREs over the BJP.
Similar content being viewed by others
References
Bao, X. H., F. Q. Zhang, and J. H. Sun, 2011: Diurnal variations of warm-season precipitation east of the Tibetan Plateau over China. Mon. Wea. Rev., 139, 2790–2810, doi: https://doi.org/10.1175/mwrd-11-00006.1.
Carbone, R. E., J. D. Tuttle, D. A. Ahijevych, et al., 2002: Inferences of predictability associated with warm season precipitation episodes. J. Atmos. Sci., 59, 2033–2056, doi: https://doi.org/10.1175/1520-0469(2002)059<2033:iopaww>2.0.co;2.
Chen, H. M., R. C. Yu, J. Li, et al., 2010: Why nocturnal long-duration rainfall presents an eastward-delayed diurnal phase of rainfall down the Yangtze River valley. J. Climate, 23, 905–917, doi: https://doi.org/10.1175/2009jcli3187.1.
Chen, M. X., Y. C. Wang, F. Gao, et al., 2012: Diurnal variations in convective storm activity over contiguous North China during the warm season based on radar mosaic climatology. J. Geophys. Res. Atmos., 117, D20115, doi: https://doi.org/10.1029/2012jd018158.
Chen, S., Y. C. Wang, W. L. Zhang, et al., 2011: Intensifying mechanism of the convective storm moving from the mountain to the plain over Beijing area. Meteor. Mon., 37, 802–813. (in Chinese)
Ding, Y. H., and J. C. L. Chan, 2005: The East Asian summer monsoon: An overview. Meteor. Atmos. Phys., 89, 117–142, doi: https://doi.org/10.1007/s00703-005-0125-z.
Du, Y., and G. X. Chen, 2019: Heavy rainfall associated with double low-level jets over southern China. Part II: Convection initiation. Mon. Wea. Rev., 147, 543–565, doi: https://doi.org/10.1175/mwr-d-18-0102.1.
Findlater, J., 1969: A major low-level air current near the Indian Ocean during the northern summer. Quart. J. Roy. Meteor. Soc., 95, 362–380, doi: https://doi.org/10.1002/qj.49709540409.
Gao, C. C., Y. Y. Li, and H. W. Chen, 2019: Diurnal variations of different cloud types and the relationship between the diurnal variations of clouds and precipitation in central and East China. Atmosphere, 10, 304, doi: https://doi.org/10.3390/atmos10060304.
He, H. Z., and F. Q. Zhang, 2010: Diurnal variations of warm-season precipitation over northern China. Mon. Wea. Rev., 138, 1017–1025, doi: https://doi.org/10.1175/2010mwr3356.1.
He, J., F. Q. Zhang, X. C. Chen, et al., 2019: Development and evaluation of an ensemble-based data assimilation system for regional reanalysis over the Tibetan Plateau and surrounding regions. J. Adv. Model. Earth Syst., 11, 2503–2522, doi: https://doi.org/10.1029/2019ms001665.
Hersbach, H., and D. Dee, 2016: ERA5 reanalysis is in production. ECMWF Newsletter, 147, 7–7.
Hersbach, H., B. Bell, P. Berrisford, et al., 2019: Global reanalysis: goodbye ERA-Interim, hello ERA5. ECMWF Newsletter, 159, 17–24.
Higgins, R. W., Y. Yao, E. S. Yarosh, et al., 1997: Influence of the Great Plains low-level jet on summertime precipitation and moisture transport over the central United States. J. Climate, 10, 481–507, doi: https://doi.org/10.1175/1520-0442(1997)010<0481:iotgpl>2.0.co;2.
Kuo, H. L., and K. L. Seitter, 1985: Instability of shearing geostrophic currents in neutral and partly unstable atmospheres. J. Atmos. Sci., 42, 331–345, doi: https://doi.org/10.1175/1520-0469(1985)042<0331:iosgci>2.0.co;2.
Li, J., and R. C. Yu, 2014: A method to linearly evaluate rainfall frequency-intensity distribution. J. Appl. Meteor. Climatol., 53, 928–934, doi: https://doi.org/10.1175/jamc-d-13-0272.1.
Li, J., R. C. Yu, and J. J. Wang, 2008: Diurnal variations of summer precipitation in Beijing. Chinese Sci. Bull., 53, 1933–1936, doi: https://doi.org/10.1007/s11434-008-0195-7.
Limaitre, Y., and P. Brovelli, 1990: Role of a low level jet in triggering and organizing moist convection in a baroclinic atmosphere. A case study: 18 May 1984. J. Atmos. Sci., 47, 82–100, doi: https://doi.org/10.1175/1520-0469(1990)047<0082:roallj>2.0.co;2.
Liu, Y., J. Xia, C. X. Shi, et al., 2009: An improved cloud classification algorithm for China’s FY-2C multi-channel images using artificial neural network. Sensors, 9, 5558–5579, doi: https://doi.org/10.3390/s90705558.
Luo, Y. L., M. W. Wu, F. M. Ren, et al., 2016: Synoptic situations of extreme hourly precipitation over China. J. Climate, 29, 8703–8719, doi: https://doi.org/10.1175/jcli-d-16-0057.1.
Ninomiya, K., and Y. Shibagaki, 2007: Multi-scale features of the Meiyu-Baiu front and associated precipitation systems. J. Meteor. Soc. Japan, 85B, 103–122, doi: https://doi.org/10.2151/jmsj.85b.103.
Nitta, T., and S. Sekine, 1994: Diurnal variation of convective activity over the tropical western Pacific. J. Meteor. Soc. Japan, 72, 627–641, doi: https://doi.org/10.2151/jmsj1965.72.5_627.
Oh, T. H., W. T. Kwon, and S. B. Ryoo, 1997: Review of the researches on changma and future observational study (kormex). Adv. Atmos. Sci., 14, 207–222, doi: https://doi.org/10.1007/s00376-997-0020-2.
Rossow, W. B., and R. A. Schiffer, 1999: Advances in understanding clouds from ISCCP. Bull. Amer. Meteor. Soc., 80, 2261–2288, doi: https://doi.org/10.1175/1520-0477(1999)080<2261:aiucfi>2.0.co;2.
Saulo, C., J. Ruiz, and Y. G. Skabar, 2007: Synergism between the low-level jet and organized convection at its exit region. Mon. Wea. Rev., 135, 1310–1326, doi: https://doi.org/10.1175/mwr3317.1.
Shen, Y., P. Zhao, Y. Pan, et al., 2014: A high spatiotemporal gauge-satellite merged precipitation analysis over China. J. Geophys. Res. Atmos., 119, 3063–3075, doi: https://doi.org/10.1002/2013jd020686.
Shin, C.-S., and T.-Y. Lee, 2005: Development mechanisms for the heavy rainfalls of 6–7 August 2002 over the middle of the Korean Peninsula. J. Meteor. Soc. Japan, 83, 683–709, doi: https://doi.org/10.2151/jmsj.83.683.
Shinoda, T., H. Uyeda, and K. Yoshimura, 2005: Structure of moist layer and sources of water over the southern region far from the Meiyu/Baiu front. J. Meteor. Soc. Japan, 83, 137–152, doi: https://doi.org/10.2151/jmsj.83.137.
Sun, J. S., 2005: A study of the basic features and mechanism of boundary layer jet in Beijing area. Chinese J. Atmos. Sci., 29, 445–452, doi: https://doi.org/10.3878/j.issn.1006-9895.2005.03.12. (in Chinese)
Sun, J. S., and W. J. Shu, 2007: The effect of urban heat island on winter and summer precipitation in Beijing region. Chinese J. Atmos. Sci., 31, 311–320, doi: https://doi.org/10.3878/j.issn.1006-9895.2007.02.12. (in Chinese)
Sun, J. S., N. He, G. R. Wang, et al., 2012: Preliminary analysis on synoptic configuration evolvement and mechanism of a torrential rain occurring in Beijing on 21 July 2012. Torren. Rain Disas., 31, 218–225. (in Chinese)
Sun, W., J. Li, R. C. Yu, et al., 2018: Circulation structures leading to propagating and non-propagating heavy summer rainfall in central North China. Climate Dyn., 51, 3447–3465, doi: https://doi.org/10.1007/s00382-018-4090-x.
Tao, S. Y., 1980: Torrential Rain in China. Science Press, Beijing, 225 pp. (in Chinese)
Wu, Q. M., H. Guo, B. Yang, et al., 2009: Effects of topography and urban heat circulation on a meso-β-scale torrential rain in Beijing area. Meteor. Mon., 35, 58–64. (in Chinese)
Yang, B., J. S. Sun, X. Mao, et al., 2016: Multi-scale characteristics of atmospheric circulation related to short-time strong rainfall events in Beijing. Acta Meteor. Sinica, 74, 919–934, doi: https://doi.org/10.11676/qxxb2016.072. (in Chinese)
Yang, C. J., J. M. Xu, and F. S. Zhao, 2008: The application of time series in FY-2C cloud detection. J. Atmos. Environ. Optics, 3, 377–391, doi: https://doi.org/10.3969/j.issn.1673-6141.2008.05.010. (in Chinese)
Yin, S. Q., D. L. Chen, and Y. Xie, 2009: Diurnal variations of precipitation during the warm season over China. Int. J. Climatol., 29, 1154–1170, doi: https://doi.org/10.1002/joc.1758.
Yin, S. Q., W. J. Li, D. L. Chen, et al., 2011: Diurnal variations of summer precipitation in the Beijing area and the possible effect of topography and urbanization. Adv. Atmos. Sci., 28, 725–734, doi: https://doi.org/10.1007/s00376-010-9240-y.
Yu, R. C., J. Li, H. M. Chen, et al., 2014: Progress in studies of the precipitation diurnal variation over contiguous China. J. Meteor. Res., 28, 877–902, doi: https://doi.org/10.1007/s13351-014-3272-7.
Yu, R. C., H. M. Chen, and W. Sun, 2015: The definition and characteristics of regional rainfall events demonstrated by warm season precipitation over the Beijing Plain. J. Hydrometeor., 16, 396–406, doi: https://doi.org/10.1175/jhm-d-14-0086.1.
Yuan, W. H., R. C. Yu, H. M. Chen, et al., 2010: Subseasonal characteristics of diurnal variation in summer monsoon rainfall over central eastern China. J. Climate, 23, 6684–6695, doi: https://doi.org/10.1175/2010jcli3805.1.
Yuan, W. H., W. Sun, H. M. Chen, et al., 2014: Topographic effects on spatiotemporal variations of short-duration rainfall events in warm season of central North China. J. Geophys. Res. Atmos., 119, 11,223–11,234, doi: https://doi.org/10.1002/2014jd022073.
Yuan, W. H., H. Xu, R. C. Yu, et al., 2018: Regimes of rainfall preceding regional rainfall events over the plain of Beijing City. Int. J. Climatol., 38, 4979–4989, doi: https://doi.org/10.1002/joc.5796.
Zhong, L. Z., R. Mu, D. L. Zhang, et al., 2015: An observational analysis of warm-sector rainfall characteristics associated with the 21 July 2012 Beijing extreme rainfall event. J. Geophys. Res. Atmos., 120, 3274–3291, doi: https://doi.org/10.1002/2014jd022686.
Acknowledgments
The authors are very grateful to the constructive comments and suggestions from the anonymous reviewers.
Author information
Authors and Affiliations
Corresponding author
Additional information
Supported by the National Key Research and Development Program of China (2018YFE0196000 and 2018YFC1507603) and National Natural Science Foundation of China (41675075 and 41875112).
Rights and permissions
About this article
Cite this article
Yuan, W., Hu, X. Comparison of Heavy Rainfall Events Originated from Different Directions of Beijing City. J Meteorol Res 34, 1299–1308 (2020). https://doi.org/10.1007/s13351-020-0051-5
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s13351-020-0051-5