Numerical modeling of glacier flow 冰河流分析
glacier debris flow 冰川泥石流
glacier debris flow deposit 冰川泥石流堆积
The first type of glacier flow is called: basal slip.
第一种冰川流动被称为:基底滑动。
If you have a glacier in a slightly warmer region, it will flow faster than a glacier in a cooler region.
如果你看到一个在稍微温暖的地区的冰川,它会比一个较冷地区的冰川漂动得更快。
During the winter, the rate of iceberg calving usually slows significantly; the glacier tongue advances, and its flow speed drops.
在冬季,冰山的崩离率往往会显着放缓;冰川生长出冰舌,其流动速度随之下降。
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