地理科学进展 ›› 2015, Vol. 34 ›› Issue (3): 389-400.doi: 10.11820/dlkxjz.2015.03.014
• 水文水资源 • 上一篇
胡健, 吕一河
收稿日期:
2014-12-01
修回日期:
2015-02-01
出版日期:
2015-03-25
发布日期:
2015-03-25
作者简介:
作者简介:胡健(1990-),男,四川简阳人,硕士生,主要从事景观格局与过程及生态水文研究,E-mail:
基金资助:
Jian HU, Yihe LÜ
Received:
2014-12-01
Revised:
2015-02-01
Online:
2015-03-25
Published:
2015-03-25
摘要:
土壤水是地球表层系统的重要组成,是水文循环的核心,控制着最基本的陆地生态系统格局与过程,是陆地生态系统健康运行的关键。土壤水分动态是研究水文过程和陆地生态系统过程相互作用及反馈必不可少的一环,是一系列水文、气候和生态过程非线性动态作用的结果。因此,土壤水分动态表现为脉动、无规律和随机的过程,对其研究需要随机方法。本文综述了基于土壤水分平衡的土壤水分动态随机模拟的研究进展,主要关注土壤水分动态随机模型的分类比较和适用性。希望能为国内生态水文学的定量研究提供一些参考,促进对水文循环与陆地生态系统之间相互作用更好的理解,最终有助于水资源和生态系统的可持续管理。
胡健, 吕一河. 土壤水分动态随机模型研究进展[J]. 地理科学进展, 2015, 34(3): 389-400.
Jian HU, Yihe LÜ. Research progress on stochastic soil moisture dynamic model[J]. PROGRESS IN GEOGRAPHY, 2015, 34(3): 389-400.
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