Abstract
A tropical cyclone (TC) vortex is considered to be embedded in and steered by a large-scale environmental flow. The environmental flow can be decomposed into two parts: temporal climatic flow and anomaly. The former is defined according to the calendar climatology with a diurnal cycle and a seasonal cycle. Thus, the temporal climatic flow of the atmosphere, which can be estimated using reanalysis data, varies with regions, altitudes, and hours. The impact of different climatic flows on TC tracks in the Northwest Pacific is examined using a simple generalized beta-advection model. Results show that the predicted tracks of two TC cases have large deviations from their best tracks in the following 1–2 days if the temporal climatic wind is replaced by other hourly climatic winds on the same calendar day or by a several-day-mean climatic wind. The track deviation is more significant when the climatic wind difference is larger than 2 m s−1. This experiment reconfirms that a TC track is influenced by temporal climatic flow and interaction with other disturbances in the vicinity.
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References
Asai T, Ke S, Kodama Y (1998) Diurnal variability of cloudiness over East Asia and the western Pacific Ocean as revealed by GMS during the warm season. J Meteorol Soc Japan 76:675–684
Chan JCL, Gray WM (1982) Tropical cyclone movement and surrounding flow relationship. Mon Weather Rev 110:1354–1374
Chan JCL, Ko FMF, Lei YM (2002) Relationship between potential vorticity tendency and tropical cyclone motion. J Atmos Sci 59:1317–1336
Chen LS, Ding YH (1979) An introduction to the Western Pacific Typhoons. Science Press, Beijing (in Chinese)
Chen G, Sha W, Iwasaki T (2009) Diurnal variation of precipitation over southeastern China: spatial distribution and its seasonality. J Geophys Res. doi:10.1029/2008JD011103
Chen G, Sha W, Sawada M, Iwasaki T (2013) Influence of summer monsoon diurnal cycle on moisture transport and precipitation over eastern China. J Geophys Res Atmos. doi:10.1002/jgrd.50337
Chu JH, Sampson CR, Levine AS, Fukada E (2002) The Joint Typhoon Warning Center tropical cyclone best tracks 1945–2000. Joint Typhoon Warning Cent, Hawaii
Dai A, Deser C (1999) Diurnal and semidiurnal variations in global surface wind and divergence fields. J Geophys Res 104:31109–31125
Davis C, Snyder C, Didlake AC (2008) A vortex-based perspective of eastern Pacific tropical cyclone formation. Mon Weather Rev 136:2461–2477
Dee DP et al (2011) The ERA-Interim reanalysis: configuration and performance of the data assimilation system. Q J R Meteorol Soc 137:553–597
den Dool Van (2007) Empirical methods in short-term climate prediction. Oxford University Press, Oxford
Deng G, Zhou YS, Liu LP (2010) Use of a new steering flow method to predict tropical cyclone motion. J Trop Meteorol 16:154–159
Dong K, Neumann CJ (1986) The relationship between tropical cyclone motion and environmental geostrophic flows. Mon Weather Rev 114:115–122
Franklin JL (1990) Dropwindsonde observations of the environmental flow of hurricane Josephine (1984), relationships to vortex motion. Mon Weather Rev 118:2732–2744
Galarneau TJ, Davis CA (2013) Diagnosing forecast errors in tropical cyclone motion. Mon Weather Rev 141:405–430
George JE, Gray WM (1976) Tropical cyclone motion and surrounding parameter relationships. J Appl Meteorol 15:1252–1264
Hirose M, Nakamura K (2005) Spatial and diurnal variation of precipitation systems over Asia observed by the TRMM Precipitation Radar. J Geophys Res. doi:10.1029/2004JD004815
Holland GJ (1984) Tropical cyclone motion: a comparison of theory and observation. J Atmos Sci 41:68–75
Huang W, Chan J, Wang S (2010) A planetary-scale land-sea breeze circulation in East Asia and the western North Pacific. Q J R Meteorol Soc. doi:10.1002/qj.663
Huang J, Du J, Qian WH (2015) A comparison between Generalized Beta-Advection Model and classical Beta-Advection Model in predicting and understanding unusual typhoon tracks in eastern China seas. Weather Forecast 30:771–792
Mao JY, Wu GX (2011) Barotropic process contributing to the formation and growth of tropical cyclone Nargis. Adv Atmos Sci 28:483–491
Marks DG (1992) The beta and advection model for hurricane track forecasting. NOAA Tech. Memo. NWS NMC 70. National Meteorological Center, Camp Springs
Monaghan AJ, Rife DL, Pinto JO, Davis CA, Hannan JR (2010) Global precipitation extremes associated with diurnally varying low-level jets. J Clim. doi:10.1175/2010JCLI3515.1
Ohsawa T, Ueda H, Hayashi T, Watanabe A, Matsumoto J (2001) Diurnal variations of convective activity and rainfall in tropical Asia. J Meteorol Soc Japan 79:333–352
Parker DJ, Burton RR, Diongue-Niang A, Ellis RJ, Felton M, Taylor CM, Thorncroft CD, Bessemoulin P, Tompkins AM (2005) The diurnal cycle of the west African monsoon circulation. Q J R Meteorol Soc. doi:10.1256/qj.04.52
Qian WH, Li J, Shan XL (2013) Application of synoptic-scale anomalous winds predicted by medium-range weather forecast models on the regional heavy rainfall in China in 2010. Sci China Earth Sci 56:1059–1070
Qian WH, Shan XL, Liang HY, Huang J, Leung CH (2014) A generalized beta advection model to improve unusual typhoon track prediction by decomposing total flow into climatic and anomalous flows. J Geophys Res Atmos 119:1097–1117
Qian WH, Zhang GW, Huang J (2015) Intensity evolution of typhoon Megi (2010) revealed from anomaly-based atmospheric variables. Meteorol Mon 41(7):806–815
Qian WH, Huang J, Zhang GW (2016a) Reexamining the binary interaction of four pairs of tropical cyclones in the Northwest Pacific. J Meteorol Soc Japan. doi:10.2151/jmsj.2016-016
Qian WH, Wu KJ, Leung CH (2016b) Three-dimensional structure and long-term trend of heat wave events in western Eurasia revealed with an anomaly-based approach. Int J Clim. doi:10.1002/joc.4634
Qian WH, Huang J, Du J (2016c) Examination of hurricane Sandy’s (2012) structure and intensity evolution from full-field and anomaly-field analyses. Tellus-A 68
Ramage CS (1952) Diurnal variation of summer rainfall over east China, Korea and Japan. J Meteorol 9:83–86
Rife DL, Pinto JO, Monaghan AJ, Davis CA, Hannan JR (2010) Global distribution and characteristics of diurnally varying low-level jets. J Clim. doi:10.1175/2010JCLI3514.1
Roy C, Kovordanyi R (2012) Tropical cyclone track forecasting techniques—a review. Atmos Res 104–105:40–69
Sanders F, Adams AL, Gordon NJB, Jensen WD (1980) Further development of a barotropic operational model for predicting paths of tropical storms. Mon Weather Rev 108:642–654
Simpson RH (2003) Hurricane: Coping with Disaster: Progress and Challenges since Galveston, 1900. American Geophysical Union, Washington
Velden CS, Leslie LM (1991) The basic relationship between tropical cyclone intensity and the depth of the environmental steering layer in the Australian region. Weather Forecast 6:244–253
Wang B, Elsberry RL, Wang YQ, Wu LG (1998) Dynamics in tropical cyclone motion: a review. Chin J Atmos Sci 22:535–547
Wu DH, Shen TL, Wu QS, Huang YY, Lian DY (2008) Analyzing the structure of typhoon “Longwang” before and after landing in Fujian coast. J Oceanogr Taiwan Strait 27:243–249
Yang S, Smith EA (2006) Mechanisms for diurnal variability of global tropical rainfall observed from TRMM. J Clim. doi:10.1175/JCLI3883.1
Yu R, Zhou T, Xiong A, Zhu Y, Li J (2007) Diurnal variations of summer precipitation over contiguous China. Geophys Res Lett. doi:10.1029/2006GL028129
Yu R, Li J, Chen H (2009) Diurnal variation of surface wind over central eastern China. Clim Dyn 1:1. doi:10.1007/s00382-008-0478-3
Yuan W, Yu R, Zhang M, Lin W, Chen H, Li J (2012) Regimes of diurnal variation of summer rainfall over subtropical East Asia. J Clim. doi:10.1175/JCLI-D-11-00288.1
Zebiak ES, Cane MA (1987) A model El Niño-Southern Oscillation. Mon Weather Rev 115:2262–2278
Acknowledgements
The work is supported by the National Natural Science Foundation of China (41375073) and the Global Change and Air-Sea Interaction Program (GASI-03-02-01-02).
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Qian, Wh., Huang, J. Impact of different climatic flows on typhoon tracks. Meteorol Atmos Phys 130, 137–152 (2018). https://doi.org/10.1007/s00703-017-0515-z
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DOI: https://doi.org/10.1007/s00703-017-0515-z