A BTOP model to extend TOPMODEL for distributed hydrological simulation of large basins
A BTOP model to extend TOPMODEL for distributed hydrological simulation of large basins
复制标题
DOI：
10.1002/hyp.6910
复制
发表时间：
2008-08-15
影响因子：
3.2
通讯作者：
Magome, Jun
中科院分区：
文献类型：
--
作者：
Takeuchi, Kuniyoshi;Hapuarachchi, Prasantha;Magome, Jun
地形是山坡水文学的主导因素。TOPMODEL在这方面有许多优势，它使用了一个地形指数，该指数来自于一个简化的稳态质量平衡假设和山坡上的经验运动方程。在许多小流域(集水区2-500公里(2))中已经证明了它的用途，但在大流域(集水区10 000-100 000公里(2))中没有。本文的目的是在一个基于网格的大流域分布式水文模拟框架中引入块状TopModel(BTOP)作为TopModel概念的所有扩展。该扩展是通过使用有效贡献面积af(A)(0)重新定义地形指数来实现的
Topography is a dominant factor in hillslope hydrology. TOPMODEL, which uses a topogaphical index derived from a simplified steady state assumption of mass balance and empirical equations of motion over a hillslope, has many advantages in this respect. Its use has been demonstrated in many small basins (catchment areas of the order of 2-500 km(2)) but not in large basins (catchment areas of the order of 10 000-100 000 km(2)). The objective of this paper is to introduce the Block-wise TOPMODEL (BTOP) as all extension of the TOPMODEL concept in a grid based framework for distributed hydrological simulation of large river basins. This extension was made by redefining the topographical index by using an effective contributing area af(a) (0