摘要
借助Shannon熵和最大熵原理提出了熵理论,并基于此理论,提出了一种水文模拟方法,结合两个实例阐述了该方法在下渗和流速分布模拟中的应用.
Using the Shannon entropy and the principle of maximum entropy, an entropy theory is presented. Based on this theory, a methodology is outlined for hydrologic modeling and is illustrated with two example applications one involving infiltration and the other involving velocity distribution.
出处
《北京师范大学学报（自然科学版）》
CAS
CSCD
北大核心
2010年第3期229-240,共12页
Journal of Beijing Normal University(Natural Science)
关键词
熵
最大熵原理
水文模拟
entropy
principle of maximum entropy
hydrologic modeling
