The climatic changes in southwestern Asia were more subtle, in that they involved shifts in mountain snow lines, rainfall patterns, and vegetation cover.
亚洲西南部的气候变化更为微妙,因为它们涉及到山地雪线、降雨模式和植被覆盖率的变化。
Though it is di? Cult to grow trees in the saline-alkali soil, the ground cover and wetland vegetation are rich and vary in response to subtle changes in the water table and PH values.
尽管难以在盐碱地里栽种树木,但覆盖地表和湿地的植被异常丰富,随着地下水位和PH值的细微变化而呈现不同的形态。
The discrepancy can be explained by long term changes in vegetation and ice cover.
植被和冰层覆盖的长期变化能够说明这种差异。
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