... The loess plateau now 现在的黄土的高原 the Loess Plateau of China 黄土高原 the Loess Plateau Gully Region 高原沟壑区 ...
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The Loess Plateau of China is located at a transitional area where the semi-humid climate is changing into the semi-arid and arid climate. This makes the eco-environment of the plateau very fragile.
黄土高原地处半干旱半湿润向干旱荒漠的过渡地带，生态环境十分脆弱。
参考来源 - 黄土高原植被恢复的土壤水分生态环境·2,447,543篇论文数据，部分数据来源于NoteExpress
The mountainous area of North China is surrounded by the North China Plain, Shanxi Gansu Loess Plateau and Inner Mongolia Plateau.
华北山区位于华北平原与陕甘黄土高原以及内蒙古高原之间，是我国经济欠发达地区之一。
Loess Plateau is a kind of peculiar relief unit in China and in the world, attracting strong attentions for its various and complex morphologies.
黄土高原是我国乃至全世界的一个十分独特的地貌单元，对其复杂多样的地貌形态的研究和可视化表达一直备受关注。
Semi arid climate, poor vegetation cover and highly erodible loess can be regarded as the main natural factors responsible for the formation of hyperconcentrated flows in the Loess Plateau, China.
黄土高原半干旱的气候条件、稀疏的植被和疏松易蚀的黄土物质，是该地区高含沙水流形成的自然地理因素。
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