[1] STEPPELER J, HESS R, DOMS G, et al. Review ofnumerical methods for nonhydrostatic weather predictionmodels [J]. Meteor. Atmos. Phys., 2003, 82(4): 287-301.
[2] WANG Y, WU C C. Current understanding of tropicalcyclone structure and intensity changes [J]. Meteor. Atmos.Phys., 2004, 87(4): 257-278.
[3] DEMARIA M, KAPLAN J. An updated statisticalhurricane intensity prediction scheme (SHIPS) for theAtlantic and eastern North Pacific basins [J]. Wea.Forecasting, 1999, 14(3): 326-337.
[4] WANG Chen-xi. Comparison experiments on the effectsof different cumulus parameterization scheme in MM5 onprecipitation prediction [J]. Sci. Meteor. Sinica, 2004,24(2): 168-176.
[5] LOU Xiao-feng, ZHOU Xiu-ji, HU Zhi-jin, et al.Comparison of explicit Microphysical schemes in MM5 [J].Meteor. Sci. Technol., 2004, 32(1): 6-12.
[6] ZHANG Ji-jia. Scientific foundation of medium andlong range weather forecasting [M]. Beijing: ChinaMeteorological Press, 1982.
[7] WU Di-sheng, WEI Jian-su, ZHOU Shui-hua, et al.Subsurface sea temperature in north and middle SouthChina Sea, monsoon, drought and flood in Guangdong [J].J. Trop. Meteor. (in Chinese), 2007, 23(6): 581-586.
[8] LIN Hui-juan, ZHANG Yao-cun. Climatic features ofthe tropical cyclone influencing China and its relationshipwith the sea surface temperature in the Pacific Ocean [J]. J.Trop. Meteor. (in Chinese), 2004, 20(2): 218-224.
[9] JIANG Ying, ZHAI Pan-mao. Intercomparation andmergence of some global SST datasets [J]. Meteor. Mon.,2000, 26(7): 3-8.
[10] YUAN Jin-nan, XIAO Wei-sheng. The influence ofSST variation on Typhoon track [J]. J. Guangdong Meteor.,2002, 3: 1-2.
[11] BENDER M A, GINIS I. Real-case simulations ofhurricane-ocean interaction using a high-resolutioncoupled model: effects on hurricane intensity [J]. Mon.Wea. Rev., 2000, 128(4): 917-946.
[12] CHEN S S, ZHAO W, TENERELLI J E, et al. Impactof the AVHRR sea surface temperature on atmosphericforcing in the Japan/East Sea [J]. Geophys. Res. Lett.,2001, 28(24): 4539-4542.
[13] GRELL G, DUDHIA J, STAUFFER D R. A descriptionof the fifth-generation Penn State/NCAR mesoscale model(MM5) [Z]. NCAR Technical Note, 1994, NCAR/tn- 398+STR, 138pp.
[14] GAO Shan-hong, XIE Hong-qin, WU Zeng-mao, et al.A simulation analysis of the evolution of the surface windfield of Bohai Sea and the vicinity area under the influenceof Typhoon Tai-Tak with MM5 [J]. J. Ocean Univ. Qingdao,2001, 31(3): 325-331.
[15] WANG Peng-yun, LIU Cun-tao. Numerical study onthe mesoscale structure of Typhoon Herb 1996 [J]. ActaMeteor. Sinica, 1998, 56(3): 296-311.
[16] ZHU Pei-jun, CHEN Min, TAO Zu-yu, et al.Numerical simulation of Typhoon Winnie (1997) after landfall, Part I: Model verification and model clouds [J]. ActaMeteor. Sinica, 2002, 60(5): 553-559.
[17] YUAN Jin-nan, LIU Cun-xia. Improved scheme ofaxisymmetric typhoon bogus model and its impact onnumerical simulation of No.0425 Typhoon [J]. J. Trop.Meteor. (in Chinese), 2007, 23(3): 237-245.
[18] LIN I I, LIU W T, WU C C, et al. Satelliteobservations of modulation of surface winds bytyphoon-induced upper ocean cooling [J]. Geophys. Res.Lett., 2003, 30(3): 1131-1134.
[19] SHAY L K, GONI G J, BLACK P G. Effects of a warmoceanic feature on Hurricane Opal [J]. Mon. Wea. Rev.,2000, 128(5): 1366- 1383.
[20] XIE S P. Satellite observations of coolocean-atmosphere interaction [J]. Bull. Amer. Meteor. Soc.,2004, 85(2): 195-208.