1. Up to the recent time, climate has been defined as the average state of the atmosphere expressed as a combination of the mean values of its individual elements such as temperature and precipitation. The geographical and statistical study of these characters has therefore been the principal occupation of the climatologist. Nearly all the studies on the climatic change, however, have been directed toward fluctuation of the individual elements and not toward that of a combination of these elements in the pure definition of climate. In this paper, the secular change of climate is expressed by the shifting movements of the major climatic areas instead of the fluctuation of individual elements and for this purpose Köppen's climatic types are adopted. In other words, Köppen's formula is used for individual years as long as possible for many stations surrounding the North Pacific Ocean and the fluctuations of each climatic type are determined. In its basic application, the Köppen system should be applied to the mean values of normal conditions at certain places, and never to calculations for individual years. It is not inappropriate, however, to use Köppen's rule to express the climatic tendencies of respective years compared to normal conditions. In this way, Russel once described the dry climate of the United States, calling it “year climate”.
2. Generally, the normal or average climate does not coincide with the mode or the most frequently experienced climate. For example, Cf a is the normal climate at Pusan in South Korea, but this was experienced only once for the period 1905 to 1944 or 3 % of the total years, while for the remaining 97% the climate was Cwa. A similar condition is found in the lower stream area of the Yangtse Valley in China. In the extreme cases, the normal type to be obtained by the use of mean temperature and precipitation has never been experienced actually at a few places. At Maku in the Pescadores Islands, for instance, year climates were completely occupied by Cwa, BS and Aw notwithstanding the normal type is Cfa. Among 300 stations in a whole area under consideration, number of places where the normal climate does not coincide with their most frequently experienced types counts forty-five. In Japan proper with the normal type of Cfa, Cwa climate is liable to occur at many places.
This fact presents a serious problem for the definition and fundamental system of climatology and in such a reason several types of climatology not based on the combination of the averaged values of their elements have been established. Dynamic climatology is one of them and this is often called the modern or recent climatology against the classical climatology for the former type.
In my opinion, however, this appelation is sometimes not adequate because the so-called classical climatology built on the average state of the atmosphere is still promising for its further development with a practical application to geography and other areal sciences.
3. Basing on the frequency of year climates, stability of climate is determined. To express the degree of climatic stability and instability, the number of Köppen's climatic types that have been actually occurred during the period of observation is taken as an index.
Now the climate is considered to be stable at the places where the number of climatic types actually occurred is less than three, and unstable when it is more than five. According to this criterion, the tropical region is generally most stable and it gradually becomes less stable toward the subarctic regions. On the other hand, the unstable climate is characterized by its peculiar distribution. Fig. 1. shows the area of climatic instability indicating that the tonal pattern is prevalent excepting the Great Basin district in the United States.
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