走廊南山河流纵剖面高海拔裂点的成因
陈苗,胡小飞,王维

The cause of high-altitude knickpoints on river longitudinal profiles along the Zoulang Nan Shan
CHEN Miao,HU Xiaofei,WANG Wei
图4 高海拔裂点上游流域面积与裂点海拔对比关系
注:图中编号的裂点表示摆浪河上游流域的河道,参考图2,编号61河流上游对应摆浪河14号冰川,摆浪河现代冰川和古冰川范围参考Zhou等[29]的研究。
Fig. 4 The relationship between the drainage area of the upper knickpiont and the elevation of the high altitude knickpiont. Knickpionts in the drainage basin of the Bailang River are marked by numbers (refer to Fig. 2, No.61 stream is correspon-ding to Glacier No. 14), and the extents for the modern glacier and the ancient glacier are referenced to Zhou et al[29]