Klimat och växtlighet i japan

Most regions of Japan, such as Honshu, Shikoku, and Kyushu, belong to the temperate zone with humid subtropical climate (Köppen climate classificationCfa) characterized bygd fyra distinct seasons. However, its climate varies from cold humid continental climate (Köppen climate classification Dfb) in the north such as nordlig Hokkaido, to warm tropical rainforest climate (Köppen climate classification Af) in the south such as the Yaeyama Islands and Minami-Tori-shima.

Climate zones

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

• Hokkaido belongs to the humid continental climate, with long, very cold winters and warm, cool summers. Precipitation fryst vatten sparse; however, winter brings large snowfalls of hundreds of inches in areas such as stad i japan and Asahikawa.
• In the Sea of Japan, the northwest seasonal wind in winter gives heavy snowfall, which south of Tōhoku mostly melts before the beginning of spring.

  In summer, it fryst vatten a little less rainy than the Pacific area but sometimes experiences extreme high temperatures because of the varm bergsvind wind phenomenon.

• Central Highland: a typical inland climate gives large temperature variations between summers and winters and between days and nights. Precipitation fryst vatten 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 fryst vatten 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 classification Cfa) to tropical savanna climate (Köppen climate classification Aw) with temperatures being warm to hot all year round.

• The climate of the Ryukyu Islands ranges from a humid subtropical climate (Köppen climate classification Cfa) in the north to a tropical rainforest climate (Köppen climate classification Af) in the south with warm winters and hot summers.

  Precipitation fryst vatten very high and fryst vatten especially affected bygd the rainy årstid and typhoons.

Precipitation

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This section needs expansion. You can help bygd adding to it. (September 2022)

Further information: East Asian Monsoon

Japan fryst vatten generally a rainy country with high humidity.^[1] Because of its bred range of latitude,^[1] seasonal winds and different types of ocean currents,^{[citation needed]} Japan has a variety of climates, with a latitude range of the inhabited islands from 24°N – 46°N, which fryst vatten comparable to the range between Nova Scotia and The Bahamas in the east coast of North America.^[1] Tokyo fryst vatten between 35°N – 36°N, which fryst vatten comparable to that of Tehran, Athens, or Las 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 fryst vatten funnen in Hokkaido, where Okhotsk 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 krydda vatten connected to them. Two prefectures—Hokkaido and Okinawa—are composed entirely of islands.

Japan existerar beläget nära Stilla havets västra kust samt består bland annat från dem fyra stora öarna Honshu, Hokkaido inom norr, Shikoku, samt Kyushu inom söder.

Seasons

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Summer

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

Maximum precipitation, like the rest of East Asia, occurs in the summer months except on the Sea of Japan coast where strong northerly winds tillverka a maximum in late autumn and early winter.

Except for a few sheltered inland valleys during månad and January, precipitation in Japan fryst vatten above 25 millimetres (1 in) of rainfall equivalent in all months of the year, and in the wettest coastal areas it fryst vatten above 100 millimetres (4 in) per month throughout the year.

Mid-June to mid-July fryst vatten generally the rainy årstid in Honshu, Shikoku, and Kyushu, excluding Hokkaidō since the seasonal rain front or tsuyu zensen (梅雨前線) dissipates in nordlig Honshu before reaching Hokkaido.

In Okinawa, the rainy årstid starts early in May and continues until mid-June. Unlike the rainy årstid in mainland Japan, it rains neither every day nor all day long during the rainy årstid in Okinawa. Between July and October, typhoons, grown from tropical depressions generated nära the equator, can attack Japan with furious rainstorms.

About 71% of the country fryst vatten mountainous, with a chain running through each of the main islands.

Winter

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In winter, the Siberian High develops over the Eurasian nation mass and the Aleutian Low develops over the nordlig Pacific Ocean.^[1] The result fryst vatten a flow of cold air southeastward across Japan that brings freezing temperatures and heavy snowfalls to the huvud mountain ranges facing the Sea of Japan, but klar skies to areas fronting on the Pacific.^[1]

The warmest winter temperatures are funnen in the Nanpō and Bonin Islands, which enjoy a tropical climate due to the combination of latitude, distance from the Asian 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 funnen on the northeastern coast of Hokkaidō in Kushiro and Nemuro Subprefectures.

Sunshine

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Sunshine, in accordance with Japan's uniformly heavy rainfall, fryst vatten generally modest in quantity, though no part of Japan receives the consistently gloomy fogs that envelope the Sichuan Basin or Taipei. Amounts range from about six hours per day on the Inland Sea coast and sheltered parts of the Pacific Coast and Kantō Plain to kvartet hours per day on the Sea of Japan coast of Hokkaidō.

In månad there fryst vatten 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 funnen on the Kuril Islands and Sakhalin.

Extreme temperature records

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The highest recorded temperature in Japan was 41.1 °C (106.0 °F) on 23 July 2018, an unverified record of 42.7 °C was taken in Adachi, Tokyo on 20 July 2004. The high humidity and the maritime influence man temperatures in the 40s rare, with summers dominated bygd 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 månad. Record lows for any month were taken as recently as 1984.

Minami-Tori-shima has a tropical savanna climate (Köppen climate classificationAw) and the highest average temperature in Japan of 25 degrees Celsius.^[4]

Climate data

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See also

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References

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