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本文对１９８２年３月１１～１６日出现在西北太平洋地区的一个强温带海洋气旋的爆发性发展过程进行了诊断分析．重点讨论了斜压不稳定和非绝热加热过程在气旋发展不同阶段的特点和相互作用．分析揭示，在气旋发展初期低层与高层扰动在垂直方向是分离的，尺度和移速都不同．由高低层等熵位涡扰动的相对位相分析发现，在发展初期斜压不稳定条件对发展是不利的，而在爆发阶段则非常有利．由湿位涡和水汽辐合，等熵运动和非地转运动分析指出，非绝热加热过程在前边两个阶段都很重要．在爆发阶段斜压不稳定与非绝热加热过程相互作用，产生正反馈，使气旋得到爆发性发展．
In this paper, a diagnostic analysis was made on the explosive development of a strong temperate oceanic cyclone from March 11 to March 16, 1982 in the western North Pacific. The characteristics and interactions of the baroclinic instability and adiabatic heating processes at different stages of cyclone development are discussed. The analysis reveals that in the early stage of the cyclone the disturbance of the lower and upper layers is separated in the vertical direction, and the scale and velocity are different. The relative phase analysis of the perturbation of the isentropic potential vorticity at the upper and lower levels found that baroclinic instability conditions were unfavorable to development during the initial stage of development and very favorable during the period of the outbreak. From the analysis of the wet-edge vorticity and water vapor convergence, the analysis of isentropic and non-geostrophic motion, the non-adiabatic heating process is very important in the first two stages. Baroclinic instability and non-adiabatic heating process during the explosion phase produce positive feedback, which makes the cyclone get explosive development.