A solidification analysis method of a cast that can predict a molten temperature drop history with fine precision is disclosed. The analysis is performed by considering different latent heat emitting patterns according to the differences of the cooling speeds. An analysis model having a plurality of elements is used. A cooling speed is calculated in each element by performing a calculation of heat transfer between the elements adjacent to each other. A temperature fluctuation range is revised in each element when a temperature fluctuates from emission of solidification latent heat based on the calculated cooling speed and a predetermined fraction solid-temperature curve of a molten alloy. A solidification analysis of the analysis model is performed by using the revised temperature fluctuation range.