根据水源的特征，冰川成因的湖泊也可以分为冰川冲积湖泊和非冰川冲积湖泊。
Glaciogenetic lakes can also be classified, according to the characteristics of water supply, into glaciofluvial lake and non-glaciofluvial lake.
结果表明，这里盛行来自冰川区的风，在冰川区与非冰川区之间风向有明显的切变，并形成一些小的辐合辐散区。
The results show that the wind from the glacier region is prevailing and there are wind shear, convergence and divergence zones between the glacial and the non-glacierized area.
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