
氷河のカービング(calving)は,末端が流出する水域が海か湖(真水)かによって,そのメカニズムや動的特性が異なる.カービングを支配する要素は,氷河の形態,動的状態,水深,底面地形,水文環境(融水の滲透,潮汐,潮流,波浪,対流等),大気および水との熱交換と多岐にわたる.山岳氷河のカービングの基礎的なしくみと特性について解説する.
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| popularity This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network. | Average | |
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| impulse This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network. | Average |
