Selected challenges in runoff generation research in forests from the hillslope to headwater drainage basin scale

被引:108
作者
Bonell, M [1 ]
机构
[1] UNESCO, Climate Change & Hydrol Proc Sect, Div Water Sci, F-75732 Paris 15, France
来源
JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION | 1998年 / 34卷 / 04期
关键词
runoff generation; hillslope hydrology; hydrometric-hydrochemistry studies; topographic-wetness models; catchment scale metric-conceptual models; field parameterization issues; forests (humid tropics; semi-arid tropics; humid temperate;
D O I
10.1111/j.1752-1688.1998.tb01514.x
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
When faced with practical forest land management issues such as the impacts of logging or forest conversion to other land uses, planners ideally require a comprehensive understanding of within drainage basin hydrological processes to determine the most vulnerable areas to increased storm runoff and erosion. Land managers in particular need to know the source areas and magnitude of inputs to the storm hydrograph, in terms of water quantity, sediment and solute transport; and the routing of such hydrographs from headwater to larger drainage basins. The latter includes an overall assessment at various scales of the impacts of forest disturbance and conversion on the water balance. This paper will focus on runoff generation in terms of identifying the various pathways and source areas. Such aspects will be linked with the need for a more comprehensive effort towards the field testing of so-called 'physically based' models of runoff generation. Some of the controversial issues arising from the difficulties in reconciling results from hydrochemical investigations with complementary hydrometric studies will be highlighted. Subsequently, attention will be given to topographic-wetness models, which have promising applications in forestland management. In addition, alternative simple models for application at the catchment scale will be assessed. The latter is in recognition that at smaller scales, heterogeneity both in time and space of soil hydraulic properties demand a greater number of parameters in modelling. Such considerations can even prove an obstacle in terms of the confident application of 'physically bases models.
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页码:765 / 785
页数:21
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