Abstract
The author of the present paper investigated the monsoon-precipitation in Kanazawa and the following results were obtained.
(1) The monsoon-precipitation of showery nature occurs in Kanazawa when the Siberian high pressure develops.
(2) The precipitation is expected when the air temperature at Gensan is lower than that over the Tusima Stream, and not expected when it is higher. Generally speaking, the amount of precipitation is greater when the difference of temperature at both places is larger.
