搜索结果: 1-15 共查到“水文地理学 Modelling”相关记录23条 . 查询时间(0.131 秒)
Sediment management modelling in the Blue Nile Basin using SWAT model
Sediment management modelling Blue Nile Basin SWAT model
font style='font-size:12px;'>
2011/3/15
Soil erosion/sedimentation is an immense problem that has threatened water resources development in the Nile river basin, particularly in the Eastern Nile (Ethiopia, Sudan and Egypt). An insight into ...
Climatology-based regional modelling of potential vegetation and average annual long-term runoff for Mesoamerica
Climatology-based regional modelling potential vegetation long-term runoff Mesoamerica
font style='font-size:12px;'>
2010/12/22
Mean annual cycles of runoff, evapotranspiration, leaf area index (LAI) and potential vegetation were modelled for Mesoamerica using the SVAT model MAPSS with different climatology datasets. We calibr...
Wolf Creek Cold Regions Model Set-up, Parameterisation and Modelling Summary
Wolf Creek Cold Regions Model Set-up Parameterisation Modelling Summary
font style='font-size:12px;'>
2014/4/2
Wolf Creek Research Basin is in the Upper Yukon River Basin near Whitehorse, Yukon and is representative of headwaters in the northern Coast Mountains. It was established in 1993 to better develop nor...
Modelling the inorganic nitrogen behaviour in a small Mediterranean forested catchment,Fuirosos (Catalonia)
inorganic nitrogen behaviour Mediterranean forested catchment Fuirosos
font style='font-size:12px;'>
2010/3/5
The aim of this work was to couple a nitrogen (N) sub-model to already existent hydrological lumped (LU4-N) and semi-distributed (LU4-R-N and SD4-R-N) conceptual models, to improve our understanding o...
“Blueprint”for the UP Modelling System for Large Scale Hydrology
UP Modelling System Large Scale Hydrology
font style='font-size:12px;'>
2009/6/8
There are at least two needs to be met by the current research efforts on large scale hydrological modelling. The first is for practical conceptual land-surface hydrology schemes for use with existing...
Modelling rainfall interception in unlogged and logged forest areas of Central Kalimantan, Indonesia
rainfall interception logged forest areas Central Kalimantan
font style='font-size:12px;'>
2009/6/5
Rainfall interception losses were monitored for twelve months and related to vegetation and rainfall characteristics at the Wanariset Sangai on the upper reaches of the Mentaya river, Central Kalimant...
The role of spatial variability of soil moisture for modelling surface runoff generation at the small catchment scale
soil moisture surface runoff generation small catchment scale
font style='font-size:12px;'>
2009/5/27
A Bayesian approach is described for dealing with the problem of infilling and generating stochastic flow sequences using rainfall data to guide the flow generation process, and including bounded (ce...
National flood modelling for insurance purposes：using IFSAR for flood risk estimation in Europe
digital terrain models Flood risk flood events
font style='font-size:12px;'>
2009/5/18
Flood risk poses a major problem for insurers and governments who ultimately pay the financial costs of losses resulting from flood events. Insurers therefore face the problem of how to assess their ...
Rainfall-runoff modelling in a catchment with a complex groundwater flow system：application of the Representative Elementary Watershed (REW) approach
Representative Elementary Watershed Rainfall-runoff groundwater flow system
font style='font-size:12px;'>
2009/5/18
Based on the Representative Elementary Watershed (REW) approach, the modelling tool REWASH (Representative Elementary WAterShed Hydrology) has been developed and applied to the Geer river basin. REWAS...
Modelling subsurface storm flow with the Representative Elementary Watershed (REW) approach：application to the Alzette River Basin
Alzette River Basin subsurface storm flow Representative Elementary Watershed
font style='font-size:12px;'>
2009/5/15
A new domain, the macropore domain describing subsurface storm flow, has been introduced to the Representative Elementary Watershed (REW) approach. The mass balance equations have been reformulated an...
Physically-based modelling of hydrological processes in a tropical headwater catchment (West Africa) – process representation and multi-criteria validation
soil moisture West Africa tropical headwater catchment
font style='font-size:12px;'>
2009/5/15
The aim of the study was to test the applicability of a physically-based model to simulate the hydrological processes in a headwater catchment in Benin. Field investigations in the catchment have sho...
Distributed hydrological modelling of total dissolved phosphorus transport in an agricultural landscape, part I: distributed runoff generation
Soil Moisture Distribution and Routing distributed runoff generation
font style='font-size:12px;'>
2009/5/13
Successful implementation of best management practices for reducing non-point source (NPS) pollution requires knowledge of the location of saturated areas that produce runoff. A physically-based, full...
Is the groundwater reservoir linear? Learning from data in hydrological modelling
groundwater reservoir linear hydrological modelling catchment behaviour
font style='font-size:12px;'>
2009/5/13
Although catchment behaviour during recession periods is better identifiable than in other periods, the representation of hydrograph recession is often weak in hydrological simulations. Among the vari...
Neural network modelling of non-linear hydrological relationships
Neural network modelling non-linear hydrological relationships
font style='font-size:12px;'>
2009/5/13
Two recent studies have suggested that neural network modelling offers no worthwhile improvements in comparison to the application of weighted linear transfer functions for capturing the non-linear na...
Modelling the spatial variability of snow water equivalent at the catchment scale
snow water equivalent catchment scale
font style='font-size:12px;'>
2009/5/13
The spatial distribution of snow water equivalent (SWE) is modelled as a two parameter gamma distribution. The parameters of the distribution are dynamical in that they are functions of the number of ...