[1] KURIHARA Y, BENDER M A, TULEYA R E, et al. Aninitialization scheme of hurricane models by vortexspecification [J]. Monthly Weather Review, 1993, 121(6):2030-2045.
[2] WAN Qi-lin, HE Xi-cheng. A scheme of TC bogusingcorresponding the satellite-observed TBB [J]. Journal ofTropical Meteorology, 2003, 19 (suppl.): 37-44.
[3] ZOU Xiaolei, XIAO Qingnong. Studies on the initializationand simulation of a mature hurricane using a variational bogusdata assimilation scheme [J]. Journal of the AtmosphericSciences, 1999, 57(7): 836-860.
[4] FUJITA T. Pressure distribution within a typhoon [J].Geophysical Magazine, 1952, 23(4): 437-451.
[5] CHAN J C L, WILLIAMS R T. Analytical and numericalstudies of the beta effect in tropical cyclone motion. Part 1:zero mean flow [J]. Journal of the Atmospheric Sciences, 1987,44(9): 1257-1265.
[6] GRAY W M. Summary of ONR sponsored tropical cyclonemotion research and future plans[R]. Appendix D of Tech Rep,NPS63-89-002, Naval Postgraduate School, Monterey, CA93943, 1989. 68-79.
[7] ZOU Xiao-lei, VANDENBERGHE F, PONDEAR M, et al.Introduction to adjoint techniques and the MM5 adjointmodeling system [R]. NCAR Technical Note, 1997,NCAR/TN-435-STR.
[8] HOSKINS B J, et al. On the use and significance ofisentropic potential vorticity maps [J]. Quarterly Journal of theRoyal Meteorological Society, 1985, 111(2): 877-946.
[9] WANG Bin, ZOU Xiaolei, ZHU Jiang. Data assimilationand its applications [J]. PNAS, 2000, 97(21): 11143-11144.