杰莱斯尼安斯基[43,44]没有谈到他的方法是否适用于温带风暴;但事实上,他在定义他的标准风暴的幅度时,似乎排除了该方法用于温带风暴情形的考虑。然而已经发现,如果考虑热带和温带系统之间的某些差异,那么这种方法的若干技术也是可以采用的。温带风暴其形状必须多少是呈园形的(至少其中央部分必须有一个园形封闭的等压线),否则,就应该选择其他预报风暴增水的方法。温带风暴中的气压梯度通常比热带气旋 Jeansneanski [43,44] did not talk about whether his method is applicable to temperate storms; in fact, however, he seems to rule out the use of this method for temperate storms in defining the magnitude of his standard storms consider. However, it has been found that several techniques of this approach are also applicable if certain differences between tropical and temperate systems are considered. A temperate storm must be somewhat circular in shape (at least its central part must have a closed, closed isobaric line), or else other means of forecasting the storm should be chosen. Pressure gradients in temperate storms are usually greater than tropical cyclones