| 1. |
- Singh, V.P., et al.
(författare)
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Kinematic wave modelling of saturated basal flow in a snowpack
- 1997
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Ingår i: Hydrological Processes. - 0885-6087 .- 1099-1085. ; 11:2, s. 177-187
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Tidskriftsartikel (refereegranskat)abstract
- Movement of snowmelt water through a thin saturated layer at the infiltrating base of a snowpack is modelled by applying the kinematic wave theory. Analytical solutions are obtained for flow depth, velocity and discharge assuming that the rate of input to the saturated layer due to vertical percolation is constant. This assumption results in a linear rise and recession of the snowmelt hydrograph. The solutions are extended to the case of time-varying input. An explicit consideration of infiltration leads to a free boundary problem.
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| 2. |
- Singh, V.P., et al.
(författare)
-
Kinematic wave modelling of vertical movement of snowmelt water through a snowpack
- 1997
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Ingår i: Hydrological Processes. - 0885-6087 .- 1099-1085. ; 11:2, s. 149-167
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Tidskriftsartikel (refereegranskat)abstract
- Vertical movement of snowmelt water through snowpacks is modelled by applying the kinematic wave theory. Analytical solutions are obtained for moisture flux, particle velocity, time history and velocity of meltwater front and total moisture content for a single melt event assuming that the melt rate is constant. These solutions are extended to the case involving more than one event.
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| 3. |
- Bobba, A. G., et al.
(författare)
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Application of a watershed runoff model to north-east pond river, Newfoundland: To study water balance and hydrological characteristics owing to atmospheric change
- 1997
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Ingår i: Hydrological Processes. - 1099-1085. ; 11:12, s. 1573-1593
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Tidskriftsartikel (refereegranskat)abstract
- The hydrological sensitivities to long-term climate change of a watershed in Eastern Canada were analysed using a deterministic watershed runoff model developed to simulate watershed acidification. This model was modified to study atmospheric change effects in the watershed. Water balance modelling techniques, modified for assessing climate effects, were developed and tested for a watershed using atmospheric change scenarios from both state of the art general circulation models and a series of hypothetical scenarios. The model computed daily surface, inter- and groundwater hows from the watershed. The moisture, infiltration and recharge rate are also computed in the soil reservoirs. The thirty years of simulated data can be used to evaluate the effects of climatic change on soil moisture, recharge rate and surface and subsurface flow systems. The interaction between surface and subsurface water is discussed in relation to climate change. These hydrological results raise the possibility of major environmental and socioeconomic difficulties and have significant implications for future water resource planning and management. (C) 1997 John Wiley & Sons, Ltd.
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