Geographical Review of Japan
Online ISSN : 2185-1719
Print ISSN : 0016-7444
ISSN-L : 0016-7444
Volume 35, Issue 5
Displaying 1-4 of 4 articles from this issue
  • Hideo SUZUKI
    1962 Volume 35 Issue 5 Pages 205-211
    Published: May 01, 1962
    Released on J-STAGE: December 24, 2008
    JOURNAL FREE ACCESS
    Many attempts have been made to classify the climates of Japan by means of mean values of the official meteorological stations, as, for example, by the January mean temperature. In fact climatic pheno-mena are too small to be revealed by the above-mentioned method, since the stations average 100 kilometre' distance from each other. Besides, regional differences tend to disappear in a calculation of mean values.. Thus this method defines the climatic boundaries too vaguely. The author of this article, in an attempt to avoid these errors, has made daily precipitation charts (scale: 1/1, 500, 000) for a year using all the non-official meteorological stations whose average distance apart is only 15 kilometers. The weather differences were then analysed. The analysis reveals that the most characteristic difference is in air masss prevalence. In Summer the polar front reaches as far north as Hokkaido and moves to the south again in winter. Over North Hokkaido a warm tropical air mass cannot be expected to stay at all during the year.
    Thus, by means of this difference of air mass prevalence, the climate of Japan is divided into two primary zones. A second division is made by the regional difference of winter precipitation. A third division is created by the concentration of heavy rainfall in certain areas.
    A detailed study of the daily precipitation chart shows that there is no other important difference of climate in Japan. Using the method described above, the author classifies the climate of Japan into nine categories as below.PPIa PTIa
    PPIb PTIb
    — PTIIa
    PPIIb PTIIb
    — PTIIIa
    — PTIIIb
    PP=Polar air mass both in Summer and Winter.
    PT=Tropical air mass in Summer and polar air mass in Winter.
    I=Precipitation in Winter monsoon.
    II=Transition from I to III.
    III=No precipitation from the Winter monsoon.
    a=Heavy rain in cyclone.
    b=Normal rain in cyclone.
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  • THE STRUCTURE OF A MODERN CASTLE-TOWN AND ITS TRANSFORMATION (2)
    Toyotoshi MATSUMOTO
    1962 Volume 35 Issue 5 Pages 212-223
    Published: May 01, 1962
    Released on J-STAGE: December 24, 2008
    JOURNAL FREE ACCESS
    In the latter part of the modern castle-town (Zyoka-machi) there was a great change from the feudal society to the economic one. This means loosening and dissolution of an urban organization in the feudal society.
    With the advent of the 18 th century, the nature of the castle-town as a feudal town became clear. Retainers and merchants lived together, and part of “Samurai-machi” began to function like “Chonin-machi.” Thus the castle-town composed of “Samurai-machi” and “Chonin-machi” began to crumble down, and the monopolistic trade system was replaced by a free trade system, and the castle-town was gradually turned into an economic town.
    The abolition of the special rights changed the nature of the feudal town-center and resulted in its transference, and the new town-center has become the center of the present-day city. The change in the character of the feudal town meant the modernization of the castle-town and prepared the way for the development of the so-called lord-town into a citizen-town. In this process the regional difference between north-eastern Japan and south-western Japan becomes a problem, which has still many points to be solved.
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  • Hiroshi MARUI
    1962 Volume 35 Issue 5 Pages 224-241
    Published: May 01, 1962
    Released on J-STAGE: December 24, 2008
    JOURNAL FREE ACCESS
    The amount of consumption of the coal produced in Japanese coal fields is about 46.87 million tons in 1958. Large fields are generally found in Kyushu and Hokkaido. Honshu, the main island of Japan, however, has only two large ones, Joban and Yamaguchi. The number of coal mining companies is great, but only 18 of them are of large-scale. 700 collieries laid down by them in all fields produced in the aggregate 27.91 million tons in Kyushu, 16.19 million tons in Hokkaido, and 8 million tons in Honshu in 1957. In this fashion, Japanese coal production can be said to show a maldistribution. 63 per cent of the coal consumption in all Japan was, however, concentrated in Honshu, especially in the manufactoring belts along the Pacific. Hence a large volume of coal is transported by sea from the coal fields in Kyushu and Hokkaido to the comsumption markets in Honshu.
    Fig. 1 shows the regional pattern of demand and supply of coal in Japan. The purpose of this study is to analyze the pattern in relation to the regional differences which the writer recognized in the consumption and the supply system of Japanese coal market. After dividing up the coal market into 16 coal market areas (Fig. 2), the writer cleared up the phases of coal supply to the coal market areas (Tab. 3) and also the connection the phases with the 16 sections of consumption such as the thermal power generation, coal-gas industry, iron and steel industry, cement industry, chemical industry, paper industry, transportation, heating, and so on (Tab. 6 and 7).
    The results of this study are as follows: 1) The 4 big coal markets areas of the above 16 are found in the central and western parts of Hokkaido, the southern part of Kanto District, including Tokyo, Yokohama, and Kawasaki, the Hanshin Region, including Osaka, Kobe, and Kyoto, and also the nothern part of Kyushu. All of these four areas correspond to great manufacturing belts of Japan, and over 60 per cent of the total coal consumption in Japan has been demanded by these areas. The coal produced in Kyushu has been supplied to the western Japan, to the west of the line connecting Nagoya with Tsuruga, while the coal produced in Hokkaido to the eastern Japan. The Kyushu coal and the Hokkaido coal, therefore, divide Japanese markets into two spheres of influence, and they are in a keen competition for spreading their markets in Tokai and Hokuriku Districts near the dividing line.
    2) The Hokkaido coal mainly comes from the Ishikari coal field, and the Kyushu coal consists of the Chikuho one to a large extent. While the natural conditions for mining in the Chikuho coal field has become worsened because of the century-long mining, the Ishikari coal field is still developing, resulting in cheaper cost of mining than in the case of the Chikuho field. Therefore, the Chikuho coal is inferior to the Ishikari coal with regard to a competition force in the market in general. Thus, coking coal of an over 2000km haul has been transported from the Ishikari field to the northern Kyushu, though the Chikuho field is located there.
    3) Today, the characters of a coal market in Japan are decided by the scale and type of the industries in the relevant coal maket area, especially of the thermal power generation, iron and steel, cement, chemical, and coal-gas.
    4) From which coal field will the coal be transported to a coal market is first decided by the distance from a coal field to a market, and then by the scale of production in a coal field, quantity of coal demand in a market, and quality of coal.
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  • 1962 Volume 35 Issue 5 Pages 242-250
    Published: May 01, 1962
    Released on J-STAGE: December 24, 2008
    JOURNAL FREE ACCESS
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