冰进
冰盖边缘、山麓冰川尾部和山谷冰川冰舌末端的位置向前移动称冰进，向后退缩时称冰退(glacier regression)，当冰川积累大于损耗时，发生冰进；反之则造成冰退。多年平均气温的变化是造成冰进和冰退的主要原因，而季节性的气候变化对此影响很小。对冰川进退的观察和研究，可以了解古气候变化的规律。
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contributed at 2011-12-23
Classification(s)
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Earth System(in Chinese) Glacial geology
Detailed Description
| English |
|---|
| Name | glacier advance |
| Chinese |
|---|
| Name | 冰进 |
| Description | 冰盖边缘、山麓冰川尾部和山谷冰川冰舌末端的位置向前移动称冰进，向后退缩时称冰退(glacier regression)，当冰川积累大于损耗时，发生冰进；反之则造成冰退。多年平均气温的变化是造成冰进和冰退的主要原因，而季节性的气候变化对此影响很小。对冰川进退的观察和研究，可以了解古气候变化的规律。 |
How to Cite
NNU_Group (2011). 冰进, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/024a089a-e79e-4f7b-a9f7-51a2ffe70805
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