冰川冻土 ›› 2016, Vol. 38 ›› Issue (6): 1666-1678.doi: 10.7522/j.issn.1000-0240.2016.0194
杨康1, 刘巧2
收稿日期:
2016-06-05
修回日期:
2016-10-09
出版日期:
2016-12-25
发布日期:
2017-04-06
作者简介:
杨康(1986-),男,甘肃庆阳人,副研究员,2014年在南京大学获博士学位,从事资源环境遥感方面的研究.E-mail:yangkangnju@gmail.com
基金资助:
国家自然科学基金项目(41501452;41371094)资助
YANG Kang1, LIU Qiao2
Received:
2016-06-05
Revised:
2016-10-09
Online:
2016-12-25
Published:
2017-04-06
摘要:
冰面水文过程是冰川径流过程的重要组成部分,对于冰川运动与物质平衡具有重要影响。冰川表面在太阳辐射、冰川物理性质、冰面地形和成冰带空间分布等多种因素影响下消融,形成以冰面水系为主线,锅穴、冰裂隙、冰面湖等为端点的冰面融水输送与分配体系。深入理解冰面水文过程,掌握冰川表面融水的输送、存储与释放,对于研究短时间尺度的冰川融水径流过程、探索冰川动态响应机理具有重要意义。总结回顾了目前国内外冰面水文过程的研究现状,提出了该领域有待解决的主要科学问题。
中图分类号:
杨康, 刘巧. 冰川表面水文过程研究进展[J]. 冰川冻土, 2016, 38(6): 1666-1678.
YANG Kang, LIU Qiao. Supraglacial drainage system: a review[J]. JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY, 2016, 38(6): 1666-1678.
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