| Name of Spa. | Prefecture. | Quality. | Temp., F°. |
| Nasu | Tochigi | Sulphurous | 162—172 |
| Noboribetsu | Ishikari | Sulphurous | 125 |
| Shibu | Nagano | Salt | 98—115 |
| Chiuzenji | Shizuoka | Carbonate of Soda and Sulphur | 114—185 |
| Takarazuka | Hiogo | Carbonic Acid | Cold |
| Ureshino | Saga | Carbonic Acid | 230 |
| Unzen | Nagasaki | Sulphurous | 158—204 |
| Wagura | Ishikawa | Salt | 180 |
| Yamashiro | Ishikawa | Salt | 165 |
| Yunoshima | Hiogo | Salt | 104—134 |
Climate.—The large extension of the Japanese islands in a northerly and southerly direction causes great varieties of climate. General characteristics are hot and humid though short summers, and long, cold and clear winters. The equatorial currents produce conditions differing from those existing at corresponding latitudes on the neighbouring continent. In Kiūshiū, Shikoku and the southern half of the main island, the months of July and August alone are marked by oppressive heat at the sea-level, while in elevated districts a cool and even bracing temperature may always be found, though the direct rays of the sun retain distressing power. Winter in these districts does not last more than two months, from the end of December to the beginning of March; for although the latter month is not free from frost and even snow, the balminess of spring makes itself plainly perceptible. In the northern half of the main island, in Yezo and in the Kuriles, the cold is severe during the winter, which lasts for at least four months, and snow falls sometimes to great depths. Whereas in Tōkyō the number of frosty nights during a year does not average much over 60, the corresponding number in Sapporo on the north-west of Yezo is 145. But the variation of the thermometer in winter and summer being considerable—as much as 72° F. in Tōkyō—the climate proves somewhat trying to persons of weak constitution. On the other hand, the mean daily variation is in general less than that in other countries having the same latitude: it is greatest in January, when it reaches 18° F., and least in July, when it barely exceeds 9° F. The monthly variation is very great in March, when it usually reaches 43° F.
During the first 40 years of the Meiji era numerous meteorological stations were established. Reports are constantly forwarded by telegraph to the central observatory in Tōkyō, which issues daily statements of the climatic conditions during the previous twenty-four hours, as well as forecasts for Meteorology. the next twenty-four. The whole country is divided into districts for meteorological purposes, and storm-warnings are issued when necessary. At the most important stations observations are taken every hour; at the less important, six observations daily; and at the least important, three observations. From the record of three decades the following yearly averages of temperature are obtained:—
| F°. | |
| Taihoku (in Formosa) | 71 |
| Nagasaki (Kiūshiū) | 60 |
| Kōbe (Main Island) | 59 |
| Osaka (Main Island) | 59 |
| Okayama (Main Island) | 58 |
| Nagoya (Main Island) | 58 |
| Sakai (Main Island) | 58 |
| Tōkyō (Capital) | 57 |
| Kiōto (Main Island) | 57 |
| Niigata (Main Island) | 55 |
| Ishinomaki (Main Island) | 52 |
| Aomori (Main Island) | 50 |
| Sapporo (Yezo) | 44 |
The following table affords data for comparing the climates of Peking, Shanghai, Hakodate, Tōkyō and San Francisco:—
| Longitude. | Latitude. | Mean Temp., F°. | |
| Peking | 116° 29′ E. | 39° 57′ N. | 53 |
| Shanghai | 121° 20′ E. | 31° 12′ N. | 59 |
| Hakodate | 140° 45′ E. | 41° 46′ N. | 47 |
| Tōkyō | 138° 47′ E. | 35° 41′ N. | 57 |
| San Francisco | 122° 25′ E. | 37° 48′ N. | 56 |
| Hottest Month. | Mean Temp. of Hottest Month. | |
| Peking | July | 80 |
| Shanghai | July | 84 |
| Hakodate | August | 71 |
| Tōkyō | August | 79 |
| San Francisco | September | 63 |
| Coldest Month. | Mean Temp. of Coldest Month. | |
| Peking | January | 22 |
| Shanghai | January | 26 |
| Hakodate | January | 28 |
| Tōkyō | January | 36 |
| San Francisco | January | 49 |
There are three wet seasons in Japan: the first, from the middle of April to the beginning of May; the second, from the middle of June to the beginning of July; and the third, from early in September to early in October. The dog days (doyō) are from the middle of July till the second half of August. September Rainfall. is the wettest month; January the driest. During the four months from November to February inclusive only about 18% of the whole rain for the year falls. In the district on the east of the main island the snowfall is insignificant, seldom attaining a depth of more than four or five inches and generally melting in a few days, while bright, sunny skies are usual. But in the mountainous provinces of the interior and in those along the western coast, deep snow covers the ground throughout the whole winter, and the sky is usually wrapped in a veil of clouds. These differences are due to the action of the north-westerly wind that blows over Japan from Siberia. The intervening sea being comparatively warm, this wind arrives at Japan having its temperature increased and carrying moisture which it deposits as snow on the western faces of the Japanese mountains. Crossing the mountains and descending their eastern slopes, the wind becomes less saturated and warmer, so that the formation of clouds ceases. Japan is emphatically a wet country so far as quantity of rainfall is concerned, the average for the whole country being 1570 mm. per annum. Still there are about four sunny days for every three on which rain or snow falls, the actual figures being 150 days of snow or rain and 215 days of sunshine.
During the cold season, which begins in October and ends in April, northerly and westerly winds prevail throughout Japan. They come from the adjacent continent of Asia, and they develop considerable strength owing to the fact that there is an average difference of some 22 mm. between the Wind. atmospheric pressure (750 mm.) in the Pacific and that (772 mm.) in the Japanese islands. But during the warm season, from May to September, these conditions of atmospheric pressure are reversed, that in the Pacific rising to 767 mm. and that in Japan falling to 750 mm. Hence throughout this season the prevailing winds are light breezes from the west and south. A comparison of the force habitually developed by the wind in various parts of the islands shows that at Suttsu in Yezo the average strength is 9 metres per second, while Izuhara in the island Tsushima, Kumamoto in Kiūshiū and Gifu in the east centre of the main island stand at the bottom of the list with an average wind velocity of only 2 metres. A calamitous atmospheric feature is the periodical arrival of storms called “typhoons” (Japanese tai-fu or “great wind”). These have their origin, for the most part, in the China Sea, especially in the vicinity of Luzon. Their season is from June to October, but they occur in other months also, and they develop a velocity of 5 to 75 m. an hour. The meteorological record for ten years ended 1905 shows a total of 120 typhoons, being an average of 12 annually. September had 14 of these phenomena, March 11 and April 10, leaving 85 for the remaining 9 months. But only 65 out of the whole number developed disastrous force. It is particularly unfortunate that September should be the season of greatest typhoon frequency, for the earlier varieties of rice flower in that month and a heavy storm does much damage. Thus, in 1902—by no means an abnormal year—statistics show the following disasters owing to typhoons: casualties to human life, 3639; ships and boats lost, 3244; buildings destroyed wholly or partially, 695,062; land inundated, 1,071,575 acres; roads destroyed, 1236 m.; bridges washed away, 13,685; embankments broken, 705 m.; crops damaged, 8,712,655 bushels. The total loss, including cost of repairs, was estimated at nearly 3 millions sterling, which may be regarded as an annual average.
Flora.—The flora of Japan has been carefully studied by many scientific men from Siebold downwards. Foreigners visiting Japan are immediately struck by the affection of the people for flowers, trees and natural beauties of every kind. In actual wealth of blossom or dimensions of forest trees the Japanese islands cannot claim any special distinction. The spectacles most admired by all classes are the tints of the foliage in autumn and the glory of flowering trees in the spring. In beauty and variety of pattern and colour the autumnal tints are unsurpassed. The colours pass from deep brown through purple to yellow and white, thrown into relief by the dark green of non-deciduous shrubs and trees. Oaks and wild prunus, wild vines and sumachs, various kinds of maple, the dōdan (Enkianthus Japonicus Hook.)—a wonderful bush which in autumn develops a hue of ruddy red—birches and other trees, all add multitudinous colours to the brilliancy of a spectacle which is further enriched by masses of feathery bamboo. The one defect is lack of green sward. The grass used for Japanese lawns loses its verdure in autumn and remains from November to March a greyish-brown blot upon the scene. Spring is supposed to begin in February when, according to the old calendar, the new year sets in, but the only flowers then in bloom are the camellia japonica and some kinds of daphne. The former—called by the Japanese tsubaki—may often be seen glowing fiery red amid snow, but the pink (otome tsubaki), white (shiro-tsubaki) and variegated (shibori-no-tsubaki) kinds do not bloom until March or April. Neither the camellia nor the daphne is regarded as a refined flower: their manner of shedding their blossoms is too unsightly. Queen of spring flowers is the plum (ume). The tree lends itself with peculiar readiness to the skilful
