冰川冻土 ›› 2016, Vol. 38 ›› Issue (1): 248-258.doi: 10.7522/j.isnn.1000-0240.2016.0028
尹振良1,2, 冯起1,2, 刘时银3, 邹松兵1
收稿日期:
2015-10-19
修回日期:
2015-12-18
出版日期:
2016-02-25
发布日期:
2016-05-30
作者简介:
尹振良(1985-),山东安丘人,助理研究员,2013年在中国科学院寒区旱区环境与工程研究所获博士学位,从事分布式水文模型研究.E-mail:yinzhenliang@lzb.ac.cn.
基金资助:
YIN Zhenliang1,2, FENG Qi1,2, LIU Shiyin3, ZOU Songbing1
Received:
2015-10-19
Revised:
2015-12-18
Online:
2016-02-25
Published:
2016-05-30
摘要: 冰川径流估算是气候变化风险评估和水资源可持续管理的重要内容.冰川径流估算方法主要包括:直接观测法、冰川物质平衡法、水量平衡方程法、水化学示踪法和水文模型法.本文首先对五种方法的应用情况进行简要总结,进而重点阐述水文模型法在估算冰川径流研究中的应用现状.水文模型法是冰川径流估算研究中使用最频繁的方法,使用方式主要包括耦合冰川模块和开发新的冰川水文模型.冰川水文模型中的消融算法主要包括温度指数模型(度日因子法)、修正的温度指数模型、能量平衡模型.受当前观测条件限制,修正的温度指数模型兼顾能量平衡模型和温度指数模型的优势而成为冰川水文模型中最流行的方法.随着学科的发展进步,能量平衡模型与水文模型的耦合将会成为未来的研究重点,发展大尺度分布式冰川水文模型是冰川水文学的未来发展方向之一.
中图分类号:
尹振良, 冯起, 刘时银, 邹松兵. 水文模型在估算冰川径流研究中的应用现状[J]. 冰川冻土, 2016, 38(1): 248-258.
YIN Zhenliang, FENG Qi, LIU Shiyin, ZOU Songbing. The application progress of hydrological model in quantifying the contribution of glacier runoff to total watershed runoff[J]. JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY, 2016, 38(1): 248-258.
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