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Climate Dynamics

, Volume 50, Issue 3–4, pp 825–843 | Cite as

Predecessor rain events over China’s low-latitude highlands associated with Bay of Bengal tropical cyclones

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Abstract

A predecessor rain event (PRE) is defined as organized heavy rainfall that occurs far ahead of tropical cyclone (TC), yet directly associated with the deep tropical moisture originating from the TC vicinity. The PREs occurring over China’s low-latitude highlands (CLLH) in association with Bay of Bengal TCs were investigated from 1981 to 2012. Results indicate that about 19% of Bay of Bengal TCs produces PRE. The PREs frequently occur when TCs are active in the northern Bay of Bengal with northeastward paths. The PREs are more likely to appear in the pre-monsoon and post-monsoon seasons, with peaks in May and October, respectively. The median lifetime of the PREs was approximately two days. The distances between PREs and parent TCs are ranged from 745 to 1849 km, with a median distance of 1118 km. Composite results of PREs suggested that deep moisture is advected from the TC vicinity to the remote CLLH region, which is situated beneath the equatorward entrance of the upper-level East Asia subtropical jet (EASJ). The lower-level southwesterly flow, which is associated with a strong pressure gradient between the western Pacific subtropical high and a trough in Bay of Bengal, steers TCs conveying abundant moisture from the Bay of Bengal to the CLLH region. The enhancement of the ascent and frontogenesis within the equatorward entrance region of the EASJ is favorable for occurrence of PREs in CLLH. TCs may also have a dynamical role in occurrence of PREs by intensifying the upper-level EASJ.

Notes

Acknowledgements

We thank Dr. Lan Xia and Dr. Tao Feng for providing helpful discussions. This work was supported by the National Natural Science Foundation of China (41305078; U1502233; 41305043), the program of KLME1304, and the Chinese Jiangsu Collaborative Innovation Center for Climate Change.

References

  1. Bosart LF, Carr FH (1978) A case study of excessive rainfall centered around Wellsville, New York, 20–21 June 1972. Mon Wea Rev 106: 348–362Google Scholar
  2. Bosart LF, Cordeira JM, Galarneau TJ, Moore BJ, Archambault HM (2012) An analysis of multiple predecessor rain events ahead of Tropical Cyclones Ike and Lowell: 10–15 September 2008. Mon Wea Rev 140: 1081–1107Google Scholar
  3. Byun KY, Lee TY (2012) Remote effects of tropical cyclones on heavy rainfall over the Korean peninsula—Statistical and composite analysis. Tellus 64:14983. doi: 10.3402/tellusa.v64i0.14983 CrossRefGoogle Scholar
  4. Cao J, Yao P, Wang L, Liu K (2014) Summer rainfall variability in low-latitude highlands of china and subtropical indian ocean dipole. J Clim 27(2):880–892CrossRefGoogle Scholar
  5. Chen LS (2007) Study and forecast on Landfall tropical cyclone heavy rainfall. Proceeding of the 14th Proseminar on Tropical Cyclone, Shanghai, pp 3–7 (in Chinese) Google Scholar
  6. Chen LS, Li Y, Cheng ZQ (2010) An overview of research and forecasting on rainfall associated with landfalling tropical cyclones. Adv Atmos Sci 27(5): 967–976CrossRefGoogle Scholar
  7. Chu JH, Sampson CR, Levine AS, Fukada E (2002) The Joint Typhoon Warning Center tropical cyclone best-tracks, 1945–2000. U.S. Naval Research Laboratory Rep. NRL/MR/ 7540-02-16, 22Google Scholar
  8. Cong CH, Chen LS, Lei XT, Li Y (2014) A study on the tropical cyclone remote precipitation-statistical and diagnostic analyses. J Meteor Res 27. doi: 10.1007/s13351-014-2070-6
  9. Cote MR (2007) Predecessor rain events in advance of tropical cyclones. Dissertation, State University of New YorkGoogle Scholar
  10. Dee DP, Uppala SM, Simmons AJ, Berrisford P, Poli P, Kobayashi S, Andrae U, Balmaseda MA, Balsamo G, Bauer P, Bechtold P, Beljaars ACM, vande Berg L, Bidlot J, Bormann N, Delsol C, Dragani R, Fuentes M, Geer AJ, Haimberger L, Healy SB, Hersbach H, Holm EV, Isaksen L, Kallberg P, Kohler M, Matricardi M, McNally AP, Monge-Sanz BM, Morcrette J-J, Park B-K, Peubey C, de Rosnay P, Tavolato C, Thepaut J-N, Vitart F (2011) The ERA-Interim reanalysis: configuration and performance of the data assimilation system. Q J Roy Meteorol Soc 137: 553–597CrossRefGoogle Scholar
  11. Draxler RP, Hess GD (1998) An overview of the HYSPLIT_4 modeling system for trajectories, dispersion, and deposition. Aust Meteor Mag 47: 295–308Google Scholar
  12. Duan X, Duan W (2015) Impact of Bay of Bengal storms on precipitation over Plateau Area. Plateau Meteorol 34(1): 1–10 (in Chinese) Google Scholar
  13. Duan X, Tao J, Cun C, Guo S, Lü L (2009) Temporal and spatial distributions of storms over the Bay of Bengal and its activity characteristic. Plateau Meteorol 28(3): 634–641 (in Chinese) Google Scholar
  14. Gaffney SJ (2004) Probabilistic Curve-Aligned Clustering and Prediction with Regression Mixture Models. Ph.D. thesis, Departament of Information and Computer Science. University of California, Irvine, CAGoogle Scholar
  15. Galarneau TJ, Bosart LF, Schumacher RS (2010) Predecessor rain events ahead of tropical cyclones. Mon Wea Rev 138: 3272–3297CrossRefGoogle Scholar
  16. Huang DQ, Zhu J, Zhang YC, Huang AN (2014) The different configurations of the East Asian polar front jet and subtropical jet and the associated rainfall anomalies over eastern China in summer. J Clim 27:8205–8220. doi: 10.1175/JCLI-D-14-00067.1 CrossRefGoogle Scholar
  17. Kalnay E, Kanamitsu M, Kistler R et al (1996) The NCEP/NCAR 40-Year Re-analysis Project. Bull Am Meteor Soc 77: 437–472CrossRefGoogle Scholar
  18. Kistler R, Kalnay E, Collins W et al (2001) The NCEP–NCAR 50-Year Reanalysis: Monthly means CD-ROM and documentation. Bull Am Meteor Soc 82:247–267CrossRefGoogle Scholar
  19. Kummerow C, Barnes W, Kozu T et al (1998) The tropical rainfall measuring mission sensor package. J Atmos Ocean Technol 15:809–817CrossRefGoogle Scholar
  20. Li CY, Zhou W (2015) Multiscale control of summertime persistent heavy precipitation events over South China in association with synoptic, intraseasonal, and low-frequency background. Clim Dyn 45: 1043–1057CrossRefGoogle Scholar
  21. Li XZ, Zhou W (2016) Modulation of the interannual variation of the India–Burma trough on the winter moisture supply over Southwest China. Clim Dyn 46 (1): 147–158Google Scholar
  22. Lü AM, Wen Y, Li (2013) Study of the impact of tropical cyclone Akash (0701) over the Bay of Bengal on a heavy rainfall event in Southwest China. Chin J Atmos Sci 37(1):160–170 (Chinese)Google Scholar
  23. Maddox RA, Chappell CF, Hoxit LR (1979) Synoptic and meso-a scale aspects of flash flood events. Bull Am Meteor Soc 60: 115–123CrossRefGoogle Scholar
  24. Moore BJ, Bosart LF, Keyser D, Jurewicz ML (2013) Synoptic-scale environments of predecessor rain events occurring east of the rocky mountains in association with Atlantic basin tropical cyclones. Mon Wea Rev 141(3): 1022–1047CrossRefGoogle Scholar
  25. Ninomiya K (1984) Characteristics of Baiu front as a predominant subtropical front in the summer northern hemisphere. J Meteor Soc Jpn 62:880–893CrossRefGoogle Scholar
  26. Petterssen S (1936) Contribution to the theory of frontogenesis. Geofys Publ 11(6): 1–27Google Scholar
  27. Pierce CH (1939) The meteorological history of the New England hurricane of Sept. 21, 1938. Mon Wea Rev 67: 237–285CrossRefGoogle Scholar
  28. Qin J, Ju JH, Xie ME (1997) The climate and weather of low-latitude highland. China Meteorological Press, Beijing (In Chinese) Google Scholar
  29. Schumacher RS, Galarneau TJ (2012) Moisture transport into midlatitudes ahead of recurving tropical cyclones and its relevance in two predecessor rain events. Mon Wea Rev 140: 1810–1827CrossRefGoogle Scholar
  30. Schumacher RS, Galarneau TJ, Bosart LF (2011) Distant effects of a recurving tropical cyclone on rainfall in a midlatitude convective system: a high-impact predecessor rain event. Mon Wea Rev 139: 650–667CrossRefGoogle Scholar
  31. Srock AF, Bosart LF (2009) Heavy precipitation associated with southern Appalachian cold-air damming and Carolina coastal frontogenesis in advance of weak landfalling Tropical Storm Marco (1990). Mon Wea Rev 137: 2448–2470CrossRefGoogle Scholar
  32. Tao Y, Cao J, Hu J, Dai Z (2013) A cusp catastrophe model of mid–long-term landslide evolution over low latitude highlands of China. Geomorphology 187:80–85. doi: 10.1016/j.geomorph.2012.12.036 CrossRefGoogle Scholar
  33. Wang YQ, Wang Y, Fudeyasu H (2009a) The role of Typhoon Songda (2004) in producing distantly located heavy rainfall in Japan. Mon Wea Rev 137: 3699–3716CrossRefGoogle Scholar
  34. Wang M, Li H, Duan X (2009b) Structure analysis and numerical simulation of a landing bengal storm. Meteorol Sci Technol 37(1): 12–18 (in Chinese) Google Scholar
  35. Wang ZQ, Zhu WJ, Duan AM (2010) A case study of snowstorm in Tibetan Plateau induced by Bay of Bengal storm: Based on the theory of slantwise vorticity development. Plateau Meteorol 29(3): 703–711 (in Chinese) Google Scholar
  36. Wang M, Duan X, Li HH, Liu JY, Fu R (2011) A sensitivity experiment to the orographic effect on the Bengal storm of Mala during its landing. Acta Meteorologica Sinica 69(3): 486–495 (In Chinese)Google Scholar
  37. Webster PJ (2008) Myanmar’s deadly daffodil. Nat Geosci 1:488–490CrossRefGoogle Scholar
  38. Xiao J, Pu G, Li Y, Lü X, Wang Z (2011) Comparative analysis of cyclone Akash and Nargis. J Yunnan Univ 33(s1): 111–117 (in Chinese) Google Scholar
  39. Xu ML, Liang HL, Duan X et al (2014) Comparative analysis of precipitation difference over yunnan influenced by Bengal Bay storm in autumn. Plateau Meteorol 33(5): 1229–1239 (in Chinese) Google Scholar
  40. Yang ZQ, Song Y, Yang RW, Liu YP (2014) The variation and influence to droughts of different intensity precipitation days during 2009 and 2011 in low-latitude highlands. J Yunnan Univ 36(5):704–714 (Chinese)Google Scholar
  41. Yatagai A, Arakawa O, Kamiguchi K, Kawamoto H, Nodzu MI, Hamada A (2009) A 44-year daily gridded precipitation dataset for Asia based on a dense network of rain gauges SOLA 5: 137–140. doi: 10.2151/sola.2009-035 CrossRefGoogle Scholar
  42. Zheng JM, Ma T, Zhang WC (2013) Climate characteristics of water vapor resource over China’s low-latitude highlands. J Tropical Meteorol 29(2):291–298 (Chinese)Google Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 2017

Authors and Affiliations

  • Junpeng Yuan
    • 1
  • Di Zhao
    • 1
  • Ruowen Yang
    • 1
    • 2
  • Hongfei Yang
    • 3
  1. 1.Department of Atmospheric SciencesYunnan UniversityKunmingChina
  2. 2.Key Laboratory of Meteorological Disaster of Ministry of EducationNanjing University of Information Science and TechnologyNanjingChina
  3. 3.Meteorological Bureau of Honghe County in Yunnan provinceHongheChina

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