[1] 陶诗言等.东亚的梅雨与亚洲上空环流变化的关系.气象学报,1958,(29):119 -134.

[2] 叶笃正等.在六月和十月大气环流的突变现象.气象学报,1958, (29):249-263.

[3] Lau K-M and M-T Li. The monsoon of East Asia and its global association-A. survey. Bull Amer Meteor Soc,1984, (65):114-125.

[4] 斯公望.论东亚梅雨锋的大尺度环流及其次天气尺度扰动.气象学报,1989,(47):312-323.

[5] Lau K-M, G J Yang and S H Shen. Seasonal and intraseasonal climatology of summer monsoon rainfall over East Asia.Mon Wea Rev,1988,(116):18-37.

[6] Ninomiya K. Characteristics of the Baiu front as a predominant subtropical front in the summer Northern Hemisphere. J Meteor Soc.Japan,1984,(62):880-894.

[7] Kato K. Airmass transformation over the semiarid region around North China and abrupt Change in the structure of the Baiu front in early summer. J Meteor Soc Japan,1987, (65):737-750.

[8] Kato K and Y Kodama. Formation of the quasi-stationary Baiu front to the south of the Japan Island in early May of 1979.J Meteor Soc Japan,1992,(70):631-647.

[9] Parsons D B. An explanation for intense frontal updraft and narrow cold-frontal rainbands. J Atmos Sci,1992,(49):1810-1825.

[10] Shapiro M A et al. The frontal hydraulic head: A micro-alpha scale(~l km) triggering mechanism for meso-α convective Systems. Mon. Wea Rev, 1985,(113):1166-1183.

[11] Trier S B et al. Observations of a subtropical cold front in a region of complex terrain. Mon Wea Rev, 1990,(118) :2449-2470.

[12] Lin Y-J et al. The Structure of a subtropical prefrontal convective rainband. Part I: Mesoscale kinematic structure determined from Dual-Doppler measurements. Mon Wea Rev,1992,(120):1816-1836.

[13] Ray S R et al. Radar analysis of a TAMEX frontal system. Mon Wea Rev, 1991,(119):2519-2539.

[14] Kuo Y-H and G T-J Chen. The Taiwan Area Mesoscale Experiment(TAMEX):An overview. Bull Amer Meteor Soc,1990,(71):488-503.

[15] Ma K-Y and L F Bosart. A synoptic overview of a heavy rain event in southern China. Wea Forecasting,1987,(2):89-112.

[16] Matsumoto S et al. Characteristic features of "Baiu" front associated with heavy rainfall. J Meteor Soc Japan,1971，(49): 267-281.

[17] Matsumoto S and K Ninomiya. On the mesoscale and medium-scale structure of a cold front and the relevant vertical circulation. J Meteor Soc Japan,1971,(49)Special issue:648-662.

[18] Matsumoto S. Unbalance low-level jet and solenoidal circulation associated with heavy rainfall. J Meteor Soc Japan, 1972,(5):194-203.

[19] Takahashi M. A note on 2-dimensional simulations of the low-level jet associated with the Baiu front using a nonhydrostatic convection model. J Meteor Soc Japan,1989,(67):937-948.

[20] Uccellini L W and D R Johnson. The coupling of upper and lower tropospheric jet streaks and implication for the development of severe storms. Mon Wea Rev,1979,(107):682-703.

[21] 斯公望等.一次梅雨锋低空急流形成的分析.大气科学,1982,(6):165-17 0.

[22] 肖文俊等.高空和低空急流和暴雨关系的天气分析.大气科学,1984,(8):83-88.

[23] Chou L C et al. A numerical simulation of the Mei-Yu front and the associated low-level jet. Mon Wea Rev, 1990,(118):1408-1428.

[24] 杨文民.副高西侧低空急流地转偏差和湿度场的个例分析.山东海洋学院学报,1982,(14):44-52.

[25] Si G-W and J-B Dong. Geostrophic imbalance and development of the tow-level jet associated with the Mei-Yu front over East Asia. Beitr Phys Atmosph, 1992,(64):273-283.

[26] Akiyama T. Frequent occurrence of heavy rainfall along the north side to the low-level jet stream in the Baiu season. Paper Meteor Geophys,l973,(24):379-388.

[27] 杨金锡.梅汛期暴雨的诊断和预报.安徽气象,1983, (3): 17-20.

[28] Chcn. G T-J et al. Study of low-level jet and extremely heavy rainfall over northern Taiwan in the Mei-Yu season. Mon Wea Rev,1988,(116):88 4-891.