Abstract
On the basis of observations for 52 years since 1891, some investigations were made to predict the deepest snow-cover at Fushiki from the data of late Autumn or early winter in the previous year.
The deepest snow-cover has some relations with the barometric gradient between Fushiki and the continent, and has a negative correlation with the atmospheric departure in November and December of Hokkaido and Tohoku District.
The pariod of about 10 years was found in 5 years running mean of the deepest snow-lying amount
