Japan technically has two primary rainy periods, but the most distinct is the "Tsuyu" (plum rain) season. This early summer phenomenon usually lasts from early June to mid-July for most of the country (occurring about a month earlier in Okinawa). It is caused by the collision of cold northerly and warm southerly air masses, resulting in a stable weather front that brings high humidity and frequent, though not always constant, rainfall. Following this, the late summer and early autumn (August to September) bring a second peak in precipitation due to typhoon season. While Tsuyu is characterized by persistent drizzle and gray skies, the autumn rain often comes in the form of intense, tropical-storm-level downpours. Hokkaido, the northernmost island, is the only region largely unaffected by the Tsuyu front, making it a popular refuge for travelers during the damp summer months.