Abstract
The altitudinal vegetation belts of Japan are divided into four: (1) the hilly belt, (2) the montane belt, (3) the subalpine belt, and (4) the alpine belt. In Central Japan, the montane belt occurs between elevations of 500 to 1500 m, the subalpine belt, between 1500 to 2500 m, and the alpine belt, over 2500 m. In winter, the Japan Sea side of the islands has heavy snow accumulation in contrast to the Pacific side which is snow-free. The effects of
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