Climate of japan wikipedia

The Japanese temperate rainforest is located in the Japanese archipelagoin small batches over a wide range of islands, climate of japan wikipedia, from Kyushu in the South to Hokkaido in the North. Due to its geographic features and climate, the Japanese temperate rainforest is very different from other temperate rainforests in the world.

Japan is home to nine forest ecoregions , which reflect its climate and geography. Japan lies at the convergence of three terrestrial realms , the Palearctic , Indomalaya , and Oceania , and its flora and fauna combine elements from all three. The island arcs of southern Japan, the Ryukyu Islands to the southwest and the Ogasawara Islands to the southeast, are home to subtropical moist broadleaf forest ecoregions; the Nansei Islands subtropical evergreen forests ecoregion is part of the Indomalayan realm , while the Ogasawara subtropical moist forests of the Ogasawaras is part of the Oceanian realm. Tropical and subtropical moist broadleaf forests. Temperate broadleaf and mixed forests. Temperate coniferous forests. Contents move to sidebar hide.

Climate of japan wikipedia

The snowfall in Japan is remarkable not only in quantity but also in reliability; you can certainly get much bigger and deeper snow dumps in coastal systems such as Whistler or New Zealand…. Cold, dry Siberian air picks up great amounts of moisture before being dumped on coastal mountains as high quality powder snow. Lake effect snow occurs when cold, dry air passes over a relatively warm water body. Water evaoporates, saturating the air and also warming it. As the air rises, often helped by flowing up and over hills or mountains, it cools and precipitates the moisture as snow. The source of the cold dry air is the Siberian High. This is a large high pressure system over Siberia. In the atmosphere, a high pressure system is generally caused by masses of cold air descendning from higher altitudes. In our case we see this cold air descending and flowing out from Siberia and across the Sea of Japan. The intensity, coverage and variability of the Siberian High is in turn heavily influenced by snow cover across the region see The role of the Siberian high in northern hemisphere climate variability , Cohen, Saito and Entekhabi, Geophysical Research Letters Volume 28 Issue 2. The average temperature in Niigata on the east coast of Honshu never drops much below 10 degrees celsius! This large temperature differential with the cool, dry air coming off Siberia allows the air to pickup significant moisture. The term fetch is used to describe the length of the water over which the wind blows unobstructed. The fetch across the Sea of Japan is anywhere from about km between Russia and Hokkaido all the way up to about km between China and Honshu. Generally, the greater the fetch the more potential for the evaporation of moisture into the air.

The Oxford Companion to Sugar and Sweets.

Japan [a] is an island country in East Asia. Japan is a part of the Ring of Fire , and spans an archipelago of 14, islands , with the five main islands being Hokkaido , Honshu the "mainland" , Shikoku , Kyushu , and Okinawa. Japan has over million inhabitants and is the 11th most populous country in the world, as well as one of the most densely populated. About three-fourths of the country's terrain is mountainous, concentrating its highly urbanized population on narrow coastal plains. Japan is divided into 47 administrative prefectures and eight traditional regions. The Greater Tokyo Area is the most populous metropolitan area in the world. Japan has the world's highest life expectancy , although it is experiencing a population decline due to its very low birth rate.

Japan has four distinct seasons with a climate ranging from subarctic in the north to subtropical in the south. Conditions are different between the Pacific side and the Sea of Japan side. Northern Japan has warm summers and very cold winters with heavy snow on the Sea of Japan side and in mountainous areas. Eastern Japan has hot and humid summers and cold winters with very heavy snow on the Sea of Japan side and in mountainous areas. Western Japan has very hot and humid summers with temperatures sometimes reaching 35 o C or above and moderate cold winters. Okinawa and Amami have a subtropical oceanic climate.

Climate of japan wikipedia

Japan Glances. Stretching like a bow off the east of the Eurasian continent, the Japanese archipelago shows great climatic variation within its approximately 3, kilometers of length from northeast to southwest. In winter, winds from Siberia pick up moisture as they cross the water, bringing rain and snow to the Japan Sea side of the country. Buffered by the central mountain ranges, the Pacific side of Japan enjoys fine weather in winter. By contrast, in summer the Pacific side of the country is rainier, due in part to typhoons, while the Japan Sea side has mostly sunny days. List created by Nippon. The first strong south wind of the year heralds the coming of spring to people on the Pacific side of Japan. Cherry blossom season with its hanami picnics under the trees starts in Okinawa in January. As well as the standard four seasons, most of Japan has a rainy season known as tsuyu , lasting around six weeks from late spring or early summer, depending on the area.

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The average rate of CO 2 emissions per person in Japan is almost double the global average. Main articles: Japanese literature , Japanese poetry , and Japanese philosophy. Now we have to add in the specific month-day pairs for each of the years. After three years, however, you may have had enough nature to last you a lifetime. How about we take a look at the prefectures with the highest average temperatures throughout the summer months? Sabaj Perez, and P. Japan has pledged to become carbon neutral by The World Bank. Retrieved October 22, Retrieved September 26, Please help improve this article by introducing citations to additional sources. Stanford University Press. Total Baseball 4th ed. World Rally Championship. The Pursuit of Power in Modern Japan —

Beautiful Four Distinct Seasons of Japan Japan is an island country with long archipelago extending from south to north; its climate varies from subtropical zone to sub-polar zone, while major part of Japan belongs to temperate zone with four distinct seasons. In regard to the Monsoon, southeasterly wind comes from the Pacific Ocean side in summer time, and northwesterly wind comes from the Siberian continent side in winter time. Also, the warm Kuroshio Current also known as the Japan Current flows northward on the Pacific side, warming areas as far north as Tokyo, and the cold Oyashio Current also known as the Okhotsk Current flows southward along the northern Pacific, cooling adjacent coastal areas.

September 29, Library of Congress. Frames of Anime: culture and image-building. Climate system Causes of climate change Effects of climate change Climate change mitigation Climate change adaptation By country and region. The Cambridge History of Japan. Attribution: Synysee on Wikipedia. Skelton, G. Yamanashi Nikkei Asian Review. Journal of the Faculty of Science, Hokkaido University.