In view of the loess plateau features of basin, modified the Distributed Time-Variant Gain Hydrological Model (DTVGM), and expanded the model to month, daily and real time scales. The DTVGM, coupling the advantages of both nonlinear and distributed hydrological models, can simulate variant hydrological processes under different environment conditions. Then, three models are applied to three catchments, which are Dali River, Xiaoli River, and Chabagou catchments. The three catchments area is different; there are different spatial scales. The result of simulation is very good. Last, the model can be used to analyze the temporal and spatial change of hydro-cycle and human activity effect. Satisfactory results were obtained in forecasting the t...
The Loess Plateau is the main source of water in Yellow River, China. After 1980s, the Yellow river ...
A spatial distributed hydrological forecasting system was developed to promote the analysis of river...
Runoff at the three time scales (non-flooding season, flooding season and annual period) was simulat...
In this paper, a rainfall-runoff modeling system is developed based on a nonlinear Volterra function...
High-resolution data on the spatial pattern of water use are a prerequisite for appropriate and sust...
The development of western China is confronted with serious challenges on water resources due to the...
For the purpose of water resources management in the Yellow River Basin with highly spatial differen...
Nowadays, great efforts have been made on distributed hydrological modeling. It is believed that, di...
Hydrologic cycle is changing under the impacts of climate change and intensifying human activities. ...
Regional hydrological modeling in ungauged regions has attracted growing attention in water resource...
Affected by intensive human activities, basin hydrologic systems show characteristics of a dualistic...
The Chaobai River basin in northern China consists of two major tributaries, the Chao River and Bai ...
AbstractThis study evaluated the application of the European flood forecasting operational real time...
Study region: Upper Yangtze River Basin, China. Study focus: The intensification of climate change a...
The Huolin River is located in the monsoon marginal zone in Northeast China. It is an important sour...
The Loess Plateau is the main source of water in Yellow River, China. After 1980s, the Yellow river ...
A spatial distributed hydrological forecasting system was developed to promote the analysis of river...
Runoff at the three time scales (non-flooding season, flooding season and annual period) was simulat...
In this paper, a rainfall-runoff modeling system is developed based on a nonlinear Volterra function...
High-resolution data on the spatial pattern of water use are a prerequisite for appropriate and sust...
The development of western China is confronted with serious challenges on water resources due to the...
For the purpose of water resources management in the Yellow River Basin with highly spatial differen...
Nowadays, great efforts have been made on distributed hydrological modeling. It is believed that, di...
Hydrologic cycle is changing under the impacts of climate change and intensifying human activities. ...
Regional hydrological modeling in ungauged regions has attracted growing attention in water resource...
Affected by intensive human activities, basin hydrologic systems show characteristics of a dualistic...
The Chaobai River basin in northern China consists of two major tributaries, the Chao River and Bai ...
AbstractThis study evaluated the application of the European flood forecasting operational real time...
Study region: Upper Yangtze River Basin, China. Study focus: The intensification of climate change a...
The Huolin River is located in the monsoon marginal zone in Northeast China. It is an important sour...
The Loess Plateau is the main source of water in Yellow River, China. After 1980s, the Yellow river ...
A spatial distributed hydrological forecasting system was developed to promote the analysis of river...
Runoff at the three time scales (non-flooding season, flooding season and annual period) was simulat...