Most regions ofJapan, such asHonshu,Shikoku, andKyushu, belong to the temperate zone withhumid subtropical climate (Köppen climate classificationCfa) characterized by four distinct seasons. However, its climate varies from coldhumid continental climate (Köppen climate classificationDfb) in the north such as northernHokkaido, to warmtropical rainforest climate (Köppen climate classificationAf) in the south such as theYaeyama Islands andMinami-Tori-shima.

Japan's varied geographical features divide it into six principal climatic zones.

• Hokkaido belongs to thehumid continental climate, with long, very cold winters and warm, cool summers. Precipitation is sparse; however, winter brings large snowfalls of hundreds of inches in areas such asSapporo andAsahikawa.
• In the Sea of Japan, the northwest seasonal wind in winter gives heavy snowfall, which south ofTōhoku mostly melts before the beginning of spring. In summer, it is a little less rainy than the Pacific area but sometimes experiences extreme high temperatures because of thefoehn wind phenomenon.
• Central Highland: a typical inland climate gives large temperature variations between summers and winters and between days and nights. Precipitation is lower than on the coast because of rain shadow effects.
• Seto Inland Sea: the mountains in the Chūgoku and Shikoku regions block the seasonal winds and bring mild climate and many fine days throughout the year.
• Pacific Ocean: the climate varies greatly between the north and the south, but generally winters are significantly milder and sunnier than those of the side that faces the Sea of Japan. Summers are hot because of the southeast seasonal wind. Precipitation is very heavy in the south and heavy in the summer in the north. The climate of the Ogasawara Islands ranges from a humid subtropical climate (Köppen climate classificationCfa) totropical savanna climate (Köppen climate classificationAw) with temperatures being warm to hot all year round.
• The climate of the Ryukyu Islands ranges from a humid subtropical climate (Köppen climate classificationCfa) in the north to a tropical rainforest climate (Köppen climate classificationAf) in the south with warm winters and hot summers. Precipitation is very high and is especially affected by the rainy season and typhoons.

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Japan is generally a rainy country with high humidity.^[1] Because of its wide range of latitude,^[1] seasonal winds and different types of ocean currents,{^[2]} Japan has a variety of climates, with a latitude range of the inhabited islands from24°N –46°N, which is comparable to the range betweenNova Scotia andThe Bahamas in the east coast of North America.^[1] Tokyo is between35°N –36°N, which is comparable to that ofTehran,Charlotte, orLas Vegas.^[1]

As Mount Fuji and the Japanese coastal Alps provide a rain shadow, Nagano and Yamanashi Prefectures receive the least precipitation in Honshu, though it still exceeds 900 millimetres (35 in) annually. A similar effect is found in Hokkaido, whereOkhotsk Subprefecture receives as little as 750 millimetres (30 in) per year. All other prefectures have coasts on the Pacific Ocean, Sea of Japan, and Seto Inland Sea, or have a body of salt water connected to them. Two prefectures—Hokkaido andOkinawa—are composed entirely of islands.

The climate from June to September is marked by hot, wet weather brought by tropical airflows from the Pacific Ocean and Southeast Asia.^[1] These air flows are full of moisture and deposit substantial amounts of rain when they reach land.^[1] There is a marked rainy season, beginning in early June and continuing for about a month.^[1] It is followed by hot, sticky weather.^[1] Five or six typhoons pass over or near Japan every year from early August to early October, sometimes resulting in significant damage.^[1] Annualprecipitation averages between 1,000 and 2,500 mm (40 and 100 in) except for the areas such asKii Peninsula andYakushima Island which is Japan's wettest place^[3] with the annual precipitation is one of the world's highest at 4,000 to 10,000 mm.^[4]

Maximum precipitation, like the rest of East Asia, occurs in the summer months except on the Sea of Japan coast where strong northerly winds produce a maximum in late autumn and early winter. Except for a few sheltered inland valleys during December and January, precipitation in Japan is above 25 millimetres (1 in) of rainfall equivalent in all months of the year, and in the wettest coastal areas it is above 100 millimetres (4 in) per month throughout the year.

Mid-June to mid-July is generally therainy season in Honshu, Shikoku, and Kyushu, excluding Hokkaidō since the seasonal rain front ortsuyu zensen (梅雨前線) dissipates in northern Honshu before reaching Hokkaido. In Okinawa, the rainy season starts early in May and continues until mid-June. Unlike the rainy season in mainland Japan, it rains neither every day nor all day long during the rainy season in Okinawa. Between July and October, typhoons, grown from tropical depressions generated near the equator, can attack Japan with furious rainstorms.

In winter, theSiberian High develops over the Eurasian land mass and theAleutian Low develops over the northern Pacific Ocean.^[1] The result is a flow of cold air southeastward across Japan that brings freezing temperatures and heavy snowfalls to the central mountain ranges facing the Sea of Japan, but clear skies to areas fronting on the Pacific.^[1]

The warmest winter temperatures are found in theNanpō andBonin Islands, which enjoy a tropical climate due to the combination of latitude, distance from theAsian continent, and warming effect of winds from the Kuroshio, as well as the Volcano Islands (at the latitude of the southernmost of the Ryukyu Islands, 24° N). The coolest summer temperatures are found on the northeastern coast of Hokkaidō inKushiro andNemuro Subprefectures.

Sunshine, in accordance with Japan's uniformly heavy rainfall, is generally modest in quantity, though no part of Japan receives the consistently gloomy fogs that envelope theSichuan Basin orTaipei. Amounts range from about six hours per day on the Inland Sea coast and sheltered parts of the Pacific Coast and Kantō Plain to four hours per day on the Sea of Japan coast of Hokkaidō. In December there is a very pronounced sunshine gradient between the Sea of Japan and the Pacific coasts, as the former side can receive less than 30 hours and the Pacific side as much as 180 hours. In summer, however, sunshine hours are lowest on exposed parts of the Pacific coast where fogs from the Oyashio current create persistent cloud cover similar to that found on the Kuril Islands and Sakhalin.

The highest recorded temperature in Japan was 41.8 °C (107.2 °F) on 5 August 2025; an unverified record of 42.7 °C was taken in Adachi, Tokyo on 20 July 2004. The high humidity and the maritime influence make temperatures in the 40s rare, with summers dominated by a more stable subtropical monsoon pattern through most of Japan. The lowest was −41.0 °C (−41.8 °F) in Asahikawa on 25 January 1902. However an unofficial −41.5 °C was taken in Bifuka on 27 January 1931. Mount Fuji broke the Japanese record lows for each month except January, February, March, and December. Record lows for any month were taken as recently as 1984.

Minami-Tori-shima has atropical savanna climate (Köppen climate classificationAw) and the highest average temperature in Japan of 25 degrees Celsius.^[5]

• Climate of China
• East Asian Monsoon

• Geography of Japan
• Climate

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