The problem of analyzing and estimating transmission losses in ephemeral streams with compound channels was the focus of this research. The Kinematic Runoff and Erosion model KINEROS (Woolhiser et al., 1990) and the Soil Conservation Service SCS model (Lane, 1983) were employed in this study as they represent a range in model complexity. Initial soil moisture and channel wetness conditions were employed to modify channel infiltration capacity in the SCS model and the saturated hydraulic conductivity in KINEROS. Numerically both models have been improved to treat compound channel routing with differential over-bank and main channel infiltration. The KINEROS model was extended by coupling the over-bank and channel one-dimensional kinematic an...
A number of methods and formulae has been proposed in the literature to estimate the discharge capac...
A number of methods and formulae has been proposed in the literature to estimate the discharge capac...
Flow volumes in ephemeral streams in and regions decrease significantly in magnitude downstream. The...
Streamflow in semi-arid lands commonly occurs in the form of flash floods in dry-bed ephemeral strea...
Transmission losses along ephemeral channels are an important, yet poorly understood, aspect of rain...
From the Proceedings of the 1980 Meetings of the Arizona Section - American Water Resources Assn. an...
The relationship of water infiltration into stream channel bed to texture, structure, and moisture c...
A simplified approach for modeling transmission losses in a stream is presented. A theory relating s...
Transmission losses along ephemeral channels are an important, yet poorly understood, aspect of rain...
From the Proceedings of the 1972 Meetings of the Arizona Section - American Water Resources Assn. an...
A distributed hydrologic model for application on small, semiarid watersheds is developed. The distr...
From the Proceedings of the 1972 Meetings of the Arizona Section - American Water Resources Assn. an...
Energy losses along a channel reach occur from friction along the channel boundaries and bed surface...
Hydrographs of ephemeral streams in an arid region usually decrease significantly in magnitude, down...
This numerical study is divided into two main parts: In the first part a model for routing unsteady ...
A number of methods and formulae has been proposed in the literature to estimate the discharge capac...
A number of methods and formulae has been proposed in the literature to estimate the discharge capac...
Flow volumes in ephemeral streams in and regions decrease significantly in magnitude downstream. The...
Streamflow in semi-arid lands commonly occurs in the form of flash floods in dry-bed ephemeral strea...
Transmission losses along ephemeral channels are an important, yet poorly understood, aspect of rain...
From the Proceedings of the 1980 Meetings of the Arizona Section - American Water Resources Assn. an...
The relationship of water infiltration into stream channel bed to texture, structure, and moisture c...
A simplified approach for modeling transmission losses in a stream is presented. A theory relating s...
Transmission losses along ephemeral channels are an important, yet poorly understood, aspect of rain...
From the Proceedings of the 1972 Meetings of the Arizona Section - American Water Resources Assn. an...
A distributed hydrologic model for application on small, semiarid watersheds is developed. The distr...
From the Proceedings of the 1972 Meetings of the Arizona Section - American Water Resources Assn. an...
Energy losses along a channel reach occur from friction along the channel boundaries and bed surface...
Hydrographs of ephemeral streams in an arid region usually decrease significantly in magnitude, down...
This numerical study is divided into two main parts: In the first part a model for routing unsteady ...
A number of methods and formulae has been proposed in the literature to estimate the discharge capac...
A number of methods and formulae has been proposed in the literature to estimate the discharge capac...
Flow volumes in ephemeral streams in and regions decrease significantly in magnitude downstream. The...