✔ 最佳答案
North the climate because Japan's islands assume east to extend very much long, the north and south surmount latitude approximately 20, therefore has the many kinds of temperature bands. The weather pattern majority is the temperate zone monsoon climate, the south Nine Provinces, four countries, the Ryukyu Islands archipelago (ownership existence dispute) has subtropics monsoon climate. North islands summer warm, the winter natural law extremely long, is cold, but also often has massively snows. But mid-west area then the winter compares 乾燥, very little snows, summer is moist. Japan is the island country, also deeply the Japan Current influence, oceanity is revealed. From March to April is the spring, from May to the beginning of September is the summer, from September to November is the autumn, at the end of November to February is a winter. Midsummer often receives the tropical cyclone to the early fall (typhoon) to make a sneak attack. Temperate zone monsoon climate Japan's weather pattern majority is the temperate zone monsoon climate Characteristic summer high temperature multi- rain: Summer the solar elevation angle increases, daytime long, the temperature is higher, 洋面 blows the southeast monsoon from the tropics to bring the abundant copious precipitation. The winter is cold 乾燥: The coldest month 均溫 below 0 degree Celsius, the winter is cold, the origin includes: Local latitude higher, is near to the winter wind source area, west the terrain comparatively 低平 Tanzania topography Gao Tungti enables the winter monsoon to strengthen. The monsoon reveals. Xia Ch'iuch'ang tropical cyclone influence. South subtropics monsoon climate Nine Provinces, four countries, the Ryukyu Islands archipelago (ownership existence dispute) has subtropics monsoon climate. Characteristic summer high temperature multi- rain: Summer solar elevation angle big, the temperature is higher, 洋面 blows the southeast monsoon from the tropics to bring the abundant copious precipitation. Winter temperate few rain: The coldest month 均溫 above 0 degree Celsius, the winter is more temperate, the origin includes: Local latitude lower, the Japan Current influence, is been far to the winter wind source area, the hypsography causes the winter monsoon to weaken. The monsoon reveals. Xia Ch'iuch'ang tropical cyclone influence. The Japanese national territory is continuous distributes in north latitude 24 □46, between east longitude 129 □146; Capital Tokyo is located 35 N, probably is similar Qingdao of with the mainland China. Of weather pattern Japan 變化多端, subtropics of from 南端 the Ryukyu Islands archipelago, temperate zone of after the Honshu, has to subfrigid zone of climate the Hokkaido. Speaking of Tokyo, summer compared to Taibei or Hong Kong approximately low 2 — 3, the winter must lower about 10, Hokkaido winter even 均溫 in Celsius below zero, sometimes falls to below zero ten, but south Nine Provinces winter average temperature, then above six, thus it may be known, because Japanese terrain long, also islands Guang Buyu in ocean, so that the climate has reveals the change and is different. Generally speaking, summer humidity high, winter humidity low, the four seasons are distinct, spectacular. The Japanese climate still had two special times, namely about June about plum rain spell and September typhoon time; The annual mean rainfall approximately is 1,,405 male thousandths of a Yuan, concentrates in 6 to September. In addition, the Japanese entire boundary is located on the earthquake belt, the earthquake number of times is frequent, only is in the majority by 微震 and the non- feeling earthquake.
2007-05-29 12:13:30 補充:
乾燥=Dry洋面=Surface of the sea均溫=Average temperature低平= low and level變化多端= changeable南端= south tip of微震= microseism