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The Yunnan–Guizhou Plateau or Yungui Plateau () is a plateau located in the provinces of Yunnan and Guizhou in southwest China. There are two distinct areas of this plateau: an area of high plateau averaging about with mountain peaks as high as in northern Yunnan, and an area of rolling hills, deep river-carved gorges, and mountains marked with geologic faults in western Guizhou.〔(【引用サイトリンク】title=Yunnan-Guizhou Plateau ) 〕 Easily eroded limestone underlies the plateau, allowing for spectacular karsts.〔 (【引用サイトリンク】title=Chinese History and Statistics - Yunnan-Guizhou Plateau Upland ) 〕 ==Temperature== Due to its high elevation and low latitude, the climate of the plateau is subject to intense solar radiation and cool temperatures with a large daily fluctuation and little yearly variation. The climate is divided into dry and wet seasons. Overall, the description of the climate is complicated on the Plateau as the temperature varies from place to place. The height of the Plateau accounts for approximately one-third of the troposphere on earth due to its high elevation, since as height rises, troposphere drops. For every rise, in general there is a fall in temperature. In north Tibet the atmospheric temperatures are in closed temperature isolines showing the distinct impact of high elevation on temperature.〔 〕 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Yunnan–Guizhou Plateau」の詳細全文を読む スポンサード リンク
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