Official name Nihon, or Nippon (Japan)
Form of government constitutional monarchy with a national Diet consisting of two legislative houses (House of Councillors ; House of Representatives )
Symbol of state Emperor: Akihito
Head of government Prime Minister: Abe Shinzo
Official language Japanese
Official religion none
Monetary unit yen (¥)
Population (2013 est.) 127,260,000COLLAPSE
Total area (sq mi) 145,898
Total area (sq km) 377,873
- Urban: (2011) 91.3%
- Rural: (2011) 8.7%
Life expectancy at birth
- Male: (2012) 79.9 years
- Female: (2012) 86.4 years
Literacy: percentage of population age 15 and over literate
- Male: 100%
- Female: 100%
GNI per capita (U.S.$) (2012) 47,870
Background of Japan
Japan, island country lying off the east coast of Asia. It consists of a great string of islands in a northeast-southwest arc that stretches for approximately 1,500 miles (2,400 km) through the western North Pacific Ocean. Nearly the entire land area is taken up by the country’s four main islands; from north to south these are Hokkaido (Hokkaidō), Honshu (Honshū), Shikoku, and Kyushu (Kyūshū). Honshu is the largest of the four, followed in size by Hokkaido, Kyushu, and Shikoku. In addition, there are numerous smaller islands, the major groups of which are the Ryukyu (Nansei) Islands (including the island of Okinawa) to the south and west of Kyushu and the Izu, Bonin (Ogasawara), and Volcano (Kazan) islands to the south and east of central Honshu. The national capital, Tokyo (Tōkyō), in east-central Honshu, is one of the world’s most populous cities.
The Japanese landscape is rugged, with more than four-fifths of the land surface consisting of mountains. There are many active and dormant volcanoes, including Mount Fuji (Fuji-san), which, at an elevation of 12,388 feet (3,776 metres), is Japan’s highest mountain. Abundant precipitation and the generally mild temperatures throughout most of the country have produced a lush vegetation cover and, despite the mountainous terrain and generally poor soils, have made it possible to raise a variety of crops. Japan has a large and, to a great extent, ethnically homogeneous population, which is heavily concentrated in the low-lying areas along the Pacific coast of Honshu.
Complexity and contrast are the keynotes of life in Japan—a country possessing an intricate and ancient cultural tradition yet one that, since 1950, has emerged as one of the world’s most economically and technologically advanced societies. Heavy emphasis is placed on education, and Japan is one of the world’s most literate countries. Tension between old and new is apparent in all phases of Japanese life. A characteristic sensitivity to natural beauty and a concern with form and balance are evident in such cities as Kyōto and Nara, as well as in Japan’s ubiquitous gardens. Even in the countryside, however, the impact of rapid Westernization is evident in many aspects of Japanese life. The agricultural regions are characterized by low population densities and well-ordered rice fields and fruit orchards, whereas the industrial and urbanized belt along the Pacific coast of Honshu is noted for its highly concentrated population, heavy industrialization, and environmental pollution.
Humans have occupied Japan for tens of thousands of years, but Japan’s recorded history begins only in the 1st century bce, with mention in Chinese sources. Contact with China and Korea in the early centuries ce brought profound changes to Japan, including the Chinese writing system, Buddhism, and many artistic forms from the continent. The first steps at political unification of the country occurred in the late 4th and early 5th centuries ce under the Yamato court. A great civilization then developed first at Nara in the 8th century and then at Heian-kyō (now Kyōto) from the late 8th to the late 12th century. The seven centuries thereafter were a period of domination by military rulers culminating in near isolation from the outside world from the early 17th to the mid-19th century.
The reopening of the country ushered in contact with the West and a time of unprecedented change. Japan sought to become a modern industrialized nation and pursued the acquisition of a large overseas empire, initially in Korea and China. By late 1941 this latter policy caused direct confrontation with the United States and its allies and to defeat in World War II (1939–45). Since the war, however, Japan’s spectacular economic growth—one of the greatest of any nation in that period—brought the country to the forefront of the world economy. It now is one of the world’s foremost manufacturing countries and traders of goods and is a global financial leader.
Geography of Japan
Japan is bounded to the west by the Sea of Japan (East Sea), which separates it from the eastern shores of South and North Korea and southeastern Siberia (Russia); to the north by La Perouse (Sōya) Strait, separating it from Russian-held Sakhalin Island, and by the Sea of Okhotsk; to the northeast by the southern Kuril Islands (since World War II under Soviet and then Russian administration); to the east and south by the Pacific; and to the southwest by the East China Sea, which separates it from China. The island of Tsushima lies between northwestern Kyushu and southeastern South Korea and defines the Korea Strait on the Korean side and the Tsushima Strait on the Japanese side.
The mountainous character of the country is the outcome of orogenic (mountain-building) forces largely during Quaternary time (roughly, the past 2.6 million years), as evidenced by the frequent occurrence of violent earthquakes, volcanic activity, and signs of change in sea levels along the coast. There are no sizable structural plains and peneplains (large land areas leveled by erosion), features that usually occur in more stable regions of the Earth.--->>>>>Read On.<<<<
Drainage and soils
The increasing demand for freshwater for use in paddy (wet-rice) cultivation and industry and for domestic consumption is a serious problem. Difficulties of supply lie in the paucity of natural water reservoirs, the swift runoff of the rivers, and the engineering difficulties of constructing large-scale dams in the rugged mountains.
Japan’s rivers are generally short and swift-running and are supplied by small drainage basins. The most significant rivers are the Teshio and Ishikari rivers of Hokkaido; the Kitakami, Tone, Shinano, Kiso, and Tenryū rivers of Honshu; and the Chikugo River of Kyushu. Some of the rivers from the volcanic areas of northeastern Honshu are acidic and are useless for irrigation and other purposes.
Lake Biwa, the largest in Japan, covers 259 square miles (670 square km) of central Honshu. All other major lakes are in the northeast. Most of the coastal lakes, such as Lakes Kasumi and Hamana of Honshu, are drowned former valleys, the bay mouths of which have been dammed by sandbars. Inland lakes such as Biwa, Suwa, and Inawashiro of Honshu occupy tectonic depressions of geologically recent fault origin. Lakes of volcanic origin (e.g., Kutcharo of Hokkaido and Towada and Ashi of Honshu) outnumber all other types.
The soils of Japan are customarily divided from northeast to southwest into a weak podzolic (soils with a thin organic mineral layer over a gray leached layer) zone, a brown earth zone, and a red earth zone. There are some local variations. The northern half of the Tōhoku area of northern Honshu is included in the area of brown forest soils. The northern tip of Hokkaido is classed as a subzone of the podzolic soils; the remainder of the island is included in the subzone of the acidic brown forest soils. Most of western Honshu is a transitional zone. Yellow-brown forest soils extend along the Pacific coast from southern Tōhoku to southern Kyushu, while red and yellow soils are confined to the Ryukyu Islands. The widespread reddish soils are generally regarded as the products of a former warmer, more humid climate. Immature volcanic ash soils occur on the uplands.
Kuroboku soils (black soils rich in humus content) are found on terraces, hills, and gentle slopes throughout Japan, while gley (sticky, blue-gray compact) soils are found in the poorly drained lowlands. Peat soils occupy the moors in Hokkaido and Tōhoku. Muck (dark soil, containing a high percentage of organic matter) and gley paddy soils are the products of years of rice cultivation. Polder soils (those reclaimed from the sea) are widely distributed. Soil fertility increases in the lowlands where agriculture is practiced, the result of a combination of natural alluvium washed down from the uplands and centuries of intense reworking of the soil medium by rice farmers.
In general, Japan’s climate is characterized as monsoonal (i.e., governed by wet and dry seasonal winds). The main influences are the country’s latitudinal extent, the surrounding oceans, and its proximity to the neighbouring Asian landmass. There are numerous local climatic variations, the result of relief features. In winter the high pressure zone over eastern Siberia and the low pressure zone over the western Pacific result in an eastward flow of cold air (the winter monsoon) from late September to late March that picks up moisture over the Sea of Japan. The winter monsoon deposits its moisture as rain or snow on the side of Japan facing the Sea of Japan and brings dry, windy weather to the Pacific side. The pressure systems are reversed during the summer, and air movements from the east and south (the summer monsoon) from mid-April to early September bring warmer temperatures and rain. Cyclonic storms and frequent and destructive typhoons (tropical cyclones) occur during late summer and early fall, especially in the southwest.
The warm waters of the Kuroshio (Japan Current), which corresponds in latitude and general directional flow to the Gulf Stream of the Atlantic, flow northward along Japan’s Pacific coast as far as latitude 35° N. The Tsushima Current branches westward from the Kuroshio off southern Kyushu and washes the coasts of Honshu and Hokkaido along the Sea of Japan; it is this current that lends moisture to the winter monsoon. The Pacific counterpart of the Atlantic’s Labrador Current, the cold Oya (Kuril) Current, flows southeastward from the Bering Sea along the east coast of Hokkaido and northeastern Honshu. Its waters meet those of the Kuroshio, causing dense sea fogs in summer, especially off Hokkaido.
The physical feature that most affects climate is the mountainous backbone of the islands. The ranges interrupt the monsoonal winds and cause the gloomy weather and heavy snows of winter along the Sea of Japan coast and the bright and windy winter weather along the Pacific. Temperatures and annual precipitation are about the same on both coasts, but they drop noticeably in the mountainous interior.
Temperatures are generally warmer in the south than in the north, and the transitional seasons of spring and fall are shorter in the north. At Asahikawa, in central Hokkaido, the average temperature in January, the coldest month, is 18 °F (−8 °C), and the average temperature in August, the warmest month, is 70 °F (21 °C), with an annual average temperature of 44 °F (7 °C). At Tokyo the average temperature for January is 42 °F (6 °C), the average for August 81 °F (27 °C), and the annual average 61 °F (16 °C). Inland from Tokyo, Nagano is cooler, with an annual average temperature of 53 °F (12 °C), whereas an annual average of 57 °F (14 °C) occurs on the Sea of Japan coast at Kanazawa. The warmest temperatures occur on Kyushu and the southern islands; at Kagoshima, the mean temperature for January is 46 °F (8 °C), the mean for August is 82 °F (28 °C), and the average is 64 °F (18 °C).
Precipitation in the form of rain and snow is plentiful throughout the islands. Maximum precipitation falls in the early summer, and the minimum occurs in winter—except on the Sea of Japan coast, which receives the country’s highest snowfall. The summer rainy season occurs through June and July; it is known as the baiu (“plum rain”) because it begins when the plums ripen. Torrential rains accompany the typhoons.
Precipitation patterns vary with topography, but most of the country receives more than 40 inches (1,020 mm) annually, mainly as rain during the summer. The smallest amount of precipitation occurs on eastern Hokkaido, where only 36 inches (920 mm) fall annually at Obihiro, whereas the mountainous interior of the Kii Peninsula of central Honshu receives more than 160 inches (4,060 mm) annually. Varying amounts of snow fall on Japan. From November to April snow blankets Hokkaido, northern and interior Honshu, and the northwest coast.
Plant and animal life
Much of the original vegetation has been replaced by agriculture or by the introduction of foreign species to the islands. Semitropical rainforest prevails in the Ryukyu and Bonin archipelagoes and contains various kinds of mulberries, camphor, oaks, and ferns (including tree ferns); madder and lianas are found as undergrowth. In the Amami Islands this type of plant life occurs only on lowlands, but it grows at higher elevations to the south. There are a few mangrove swamps along the southern coast of Kyushu.
The laurel forest zone of evergreen, broad-leaved trees extends from the southwestern islands northward to the lowlands of northern Honshu. Camphor, pasanias, Japanese evergreen oaks, camellias, and hollies are typical trees, with various kinds of ferns as undergrowth. In Kyushu, the evergreen zone reaches elevations above 3,300 feet (1,000 metres), but its vertical limit decreases northeastward across Honshu. In general, camphor dominates in the littoral lowlands, pasania in sunny and well-drained sites, and Japanese evergreen oak in the foggy and cloudy inlands. In the southwestern Hondo region (western Honshu, Shikoku, and Kyushu) are ficus and fan palm. The coastal dunes are dominated by pine trees. Natural stands of Japanese cedars, some containing trees that are more than 2,000 years old, occur above 2,300 feet (700 metres) on Yaku Island, south of Kyushu.
Deciduous broad-leaved forests develop in the higher and more northerly portions of the laurel forest zone. In Kyushu, this type of forest occurs above 3,300 feet, but it gradually descends northward to sea level in northern Honshu. Its upper limit reaches 6,000 feet (1,800 metres) in Shikoku and 5,000 feet (1,500 metres) in central Honshu. Representative trees are beeches, katsura trees, maples, oaks, and birches, rising above an undergrowth of various species of bamboo. All these trees, but especially the maples, are admired for their beautiful fall colours. The deciduous trees have been occasionally replaced by larches, false cypresses, false arborvitaes, Japanese cedars, Japanese red pines, Japanese black pines, and other coniferous species. The deciduous zone extends into western Hokkaido, where beeches terminate at the southwestern peninsula and further northeastward are replaced by basswoods and maples. Some stands of conifers are mixed with the representative forests of this zone.
Coniferous trees are numerous in the north and eastern periphery of Hokkaido up to elevations of 2,300 feet. Sakhalin spruces, Sakhalin firs, blue firs, and Yezo spruces are mixed with such deciduous trees as birches, oaks, and maples and dense undergrowth of mosses and lichens. Coniferous trees are mixed with deciduous vegetation in southwestern Hokkaido and occur in the higher portion of central Honshu and Shikoku. High-elevation small shrubs, creeping pines, and alpine plants grow in the high mountain knots of central Honshu above 8,000 feet (2,400 metres). This zone gradually descends northward to the Hakkōda Mountains, in northern Honshu, at 4,600 feet (1,400 metres) and to the Daisetsu Mountains, in central Hokkaido, at about 3,600 feet (1,100 metres).
The cherry tree (sakura), celebrated for its spring blossoms, long one of the symbols of Japan, is planted throughout the country. Many varieties have been cultivated, and natural stands are also found in the mountains.
Despite the country’s large human population, the land mammals of Japan are relatively numerous in the remote, heavily forested mountain regions. These animals include bears, wild boars, raccoon dogs (tanuki), foxes, deer (including sikas), antelope, hares, and weasels; some species are distinct from those of the neighbouring Asian continent. Wild monkeys (the Japanese macaque) inhabit many places; those found at the northern tip of Honshu represent the northern limit of monkey habitation in the world.
Reptiles include sea turtles, freshwater tortoises, sea snakes, and lizards. There are two species of poisonous snakes, but most of the snakes, including the 5-foot- (1.5-metre-) long Japanese rat snake, are harmless. Toads, frogs, and newts are common, and the endemic Japanese giant salamander of Kyushu and western Honshu can attain a length of four feet or more. Insect life is typical of a temperate humid climate; several species have seasonal associations in literature and popular culture, such as cicadas and dragonflies (summer) and crickets (autumn).
The Japanese archipelago constitutes a major East Asian flyway, and some 600 bird species are either resident or transitory. Water birds are abundant and include gulls, auks, grebes, albatrosses, shearwaters, herons, ducks, geese, swans, and cranes. The cormorant is sometimes trained to catch fish. There are about 150 species of songbirds, as well as eagles, hawks, falcons, pheasant, ptarmigan, quail, owls, and woodpeckers.
The confluence of cold and warm ocean currents near Japan has produced a rich sea life. Japanese waters are inhabited by whales, dolphins, porpoises, and fish such as salmon, sardines, sea bream, mackerel, tuna, trout, herring, gray mullet, smelts, and cod. Crustaceans and mollusks include crabs, shrimp, prawns, clams, and oysters. The rivers and lakes abound in trout, salmon, and crayfish. Carp (koi) are often kept in ponds, both for commercial food production and for decorative purposes.
The tremendous growth in population from the late 19th to the mid-20th century and the rapid industrialization after 1945 put increased pressure on Japan’s natural plant and animal communities, primarily through loss of habitat and environmental pollution. Once-abundant creatures, such as the eastern white stork (kōnotori) and the Japanese crested ibis (toki), have become extinct. Awareness of pollution grew from the 1960s, and after 1970 a number of strict measures were taken. Although domestic air and water quality improved, air pollution from the East Asian mainland increased the incidence of acid rain in Japan.
Demography of Japan
- Ethnic groups
The Japanese people constitute the overwhelming majority of the population. They are ethnically closely akin to the other peoples of eastern Asia. During the Edo (Tokugawa) period (1603–1867), there was a social division of the populace into four classes—warrior, farmer, craftsman, and merchant—with a peer class above and an outcast class below. With the exception of the burakumin (literally, “people of the hamlet”), the descendants of the former outcast class, this social class system has almost disappeared. The burakumin, however, are still subject to varying degrees of discrimination.
Insofar as a social class system does persist, it does not have the ethnic basis that can exist in multiracial societies, since the Japanese regard themselves as belonging to a single ethnic group. The few exceptions include those classified as resident aliens (particularly Koreans) and Japanese citizens of Ainu and, to a lesser degree, Okinawan origin. Japan also has a small population of Chinese descent.
Hundreds of thousands of Koreans migrated to Japan (a great many against their will) before and during World War II, when Korea was a Japanese colony, and worked mainly as labourers; those remaining after the war and their descendants, the latter born and raised in Japan, do not have Japanese citizenship and face considerable discrimination.
Both Ainu and Okinawans are often relegated to a second-class status. The indigenous Ainu largely were assimilated into the general population centuries ago; a few small, scattered groups, however, have maintained their identity in Hokkaido. Before the war there was a tendency to distinguish the people of Okinawa from other Japanese because of perceived physical and cultural differences; this tendency has diminished but not disappeared. Okinawan culture, including its dialect and religion, is now recognized as sharing many traits with Japanese culture.
Japanese is the national language, and Ainu is almost extinct. The Japanese language is generally included in the Altaic linguistic group and is especially akin to Korean, although the vocabularies differ. Some linguists also contend that Japanese contains elements of Southeast Asian languages. The introduction of the Chinese writing system and of Chinese literature about the 4th century ce enriched the Japanese vocabulary. Until that time Japanese had no written form, and at first Chinese characters (called kanji in Japanese) were used to write Japanese; by the 9th century two syllabaries, known collectively as kana (katakana and hiragana), were developed from them. Since then, a combination of kanji and kana has been used for written Japanese. Although some 3,000 to 5,000 kanji are in general use, after World War II the number of characters necessary for a basic vocabulary was reduced to about 2,000, and the writing of these characters was simplified. Tens of thousands of Western loanwords, principally from English, also have been adopted.
The distribution of Japanese nearly coincides with the territory of Japan. Standard Japanese, based on the dialect spoken in Tokyo, was established in the late 19th century through the creation of a national educational system and through more widespread communication. There are many local dialects, which are often mutually unintelligible, but standard Japanese, widely used in broadcasting, is understood nationwide.
Japanese is broadly divided linguistically into the two major dialects of Hondo and Nantō. The Hondo dialect is used throughout Japan and may be divided into three major subdialects: Eastern, Western, and Kyushu. The Eastern subdialects were established in the 7th and 8th centuries and became known as the Azuma (“Eastern”) language. After the 17th century there was a vigorous influx of the Kamigata (Kinai) subdialect, which was the foundation of standard Japanese. Among the Western subdialects, the Kinki version was long the standard language of Japan, although the present Kamigata subdialect of the Kyōto-Ōsaka region is of relatively recent origin. The Kyushu subdialects have been placed outside the mainstream of linguistic change of the Western dialects and retain some of the 16th-century forms of the latter. They extend as far south as Tanega and Yaku islands. The Nantō dialects are used by Okinawa islanders from the Amami Islands in Kagoshima prefecture to Yonaguni Island at the western end of the archipelago. Long placed outside the mainstream of linguistic change, they strongly retain their ancient forms.
The indigenous religion of Japan, Shintō, coexists with various sects of Buddhism, Christianity, and some ancient shamanistic practices, as well as a number of “new religions” (shinkō shukyō) that have emerged since the 19th century. Not one of the religions is dominant, and each is affected by the others. Thus, it is typical for one person or family to believe in several Shintō gods and at the same time belong to a Buddhist sect. Intense religious feelings are generally lacking except among the adherents of some of the new religions. Japanese children usually do not receive formal religious training. On the other hand, many Japanese homes contain a Buddhist altar (butsudan), at which various rituals—some on a daily basis—commemorate deceased family members.
Shintō is a polytheistic religion. People, commonly major historical figures, as well as natural objects have been enshrined as gods. Some of the Hindu gods and Chinese spirits were also introduced and Japanized. Each rural settlement has at least one shrine of its own, and there are several shrines of national significance, the most important of which is the Grand Shrine of Ise in Mie prefecture. Many of the ceremonies associated with the birth of a child and the rites of passage to adulthood are associated with Shintō. After the Meiji Restoration (1868), Shintō was restructured as a state-supported religion, but this institution was abolished after World War II.
Buddhism, which claims the largest number of adherents after Shintō, was officially introduced into the imperial court from Korea in the mid-6th century ce. Direct contact with central China was maintained, and several sects were introduced. In the 8th century Buddhism was adopted as the national religion, and national and provincial temples, nunneries, and monasteries were built throughout the country. The Tendai (Tiantai) and Shingon sects were founded in the early 9th century, and they have continued to exert profound influence in some parts of Japan. Zen Buddhism, the development of which dates to the late 12th century, has maintained a large following. Most of the major Buddhist sects of modern Japan, however, have descended from those that were modified in the 13th century by monks such as Shinran, who established an offshoot of Pure Land (Jōdo) Buddhism called the True Pure Land sect (Jōdo Shinshū), and Nichiren, who founded Nichiren Buddhism.
Christianity was introduced into Japan by first Jesuit and then Franciscan missionaries in the mid- to late 16th century. It initially was well received, both as a religion and as a symbol of European culture. After the establishment of the Tokugawa shogunate (1603), Christians were persecuted, and Christianity was totally banned in the 1630s. Inaccessible and isolated islands and the peninsula of western Kyushu continued to harbour “hiding Christian” villages until the ban was lifted by the Meiji government in 1873. Christianity was reintroduced by Western missionaries, who established a number of Russian Orthodox, Roman Catholic, and Protestant congregations. Practicing Christians account for only a tiny fraction of the total population.
The great majority of what are now called the “new religions” were founded after the mid-19th century. Most have their roots in Shintō and shamanism, but they also were influenced by Buddhism, Neo-Confucianism, and Christianity. One of the largest, the Sōka Gakkai (“Value Creation Society”), is based on a sect of Nichiren Buddhism. Another new Nichiren sect to attract a large following is the Risshō Kōsei-kai. New Shintō cults include Tenrikyō and Konkōkyō.
- TRADITIONAL REGIONS
The concept of regions in Japan is inseparable from the historical development of administrative units. Care was always taken to include various physical features in the larger administrative units so as to create a well-balanced geographic whole. Many of the ancient terms for administrative units have survived in the form of place-names.--->>>>>Read More<<<
- Demographic trends
Japan’s population distribution is highly variable. The mountainous character of the country has caused the population to concentrate within the limited plains and lowlands—notably along the Pacific littoral. The increased population there, however, was absorbed into the expanding urban areas, while the population of rural districts declined considerably; this had the effect of further concentrating population in a limited area.
Japan experienced spectacular population growth after 1868; the population increased nearly fourfold since then. This increase was directly related to slow but steady urban growth; the development of Hokkaido, Tōhoku, and southern Kyushu; and the introduction of commercial agriculture. In 1897, when industrialization first began, the population numbered more than 42 million. From 1898 to 1918, growing industrial cities and mining towns absorbed a large population, as did Hokkaido and the sericultural (silkworm-raising) rural districts.
In 1920, when the first precise census was conducted, the population was nearly 57 million. Between 1919 and 1945 Tokyo-Yokohama (Keihin), Ōsaka-Kōbe-Kyōto (Keihanshin), Nagoya (Chūkyō), and northern Kyushu developed as the country’s four major industrial districts. At the same time, some of the smaller cities lost their ability to sustain a growing population, and some of them declined. By 1940 the population had grown to more than double that of 1868. During World War II there was a marked migration to the rural areas to avoid aerial bombing; some cities, such as Ōsaka, were reduced to one-third their previous size. After 1945 the repatriated population of nearly 9 million and the temporarily explosive increase in the birth rate caused abnormally high growth.
The rapid rehabilitation of industry after 1950 resulted in the continued concentration of population in the Pacific coastal areas. The expansion of the Keihin area was not confined to Tokyo, Yokohama, and their adjacent suburbs but extended to a much wider circle. The same was true of the Keihanshin and Chūkyō areas. Rural areas outside the direct influence of urbanization were subjected to a marked decline. Adult males migrated to the Pacific coast, and many of those who remained at home periodically left as temporary labourers, creating a constant outflow of population from the mountainous areas and isolated islands. In many places, emigration was so marked that the remaining population could not maintain a balanced community, and whole settlements were abandoned. These trends continued in the early 21st century, although rural-to-urban migration slowed somewhat, and people have been leaving city centres for outlying districts and suburbs.
The striking demographic feature in post-World War II Japan is the decline of birth and death rates, the result of families having fewer children and of health conditions improving markedly. Japan’s rate of population increase slowed dramatically at the end of the 20th century and became essentially stagnant in the first decade of the 21st century. Japan now has one of the world’s lowest birth rates, and its life expectancy is among the world’s highest. Consequently, the country has a rapidly aging population, a circumstance that at times has created severe labour shortages for its vast economy. During periods when labour is scarce, low-skilled job needs at least have been met by a growing number of temporary foreign workers, though such arrangements are suspended during economic downturns.
Economy of Japan
Government and Society of Japan
Culture Life of Japan
History of Japan
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