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Preface | |
List of Contributors | |
Hydrological Processes | |
Doogeology - Linear Theory of Open Channel Flow | |
Abstract | |
Introduction | |
Linearization of the St. Venant Equations | |
Solution for Finite Channel Reach | |
The Generalized Linear Channel Response | |
Simplified Forms of St. Venant Equations | |
Conclusions | |
References | |
Analytical and Numerical Modelling of Unsaturated Flow | |
Abstract | |
Introduction | |
Physics of Soil Moisture Flow | |
Reduced Form of Richards' Equation | |
Closed Form Solutions for ConstantDand LinearK | |
Model | |
Effect of Assumptions onDandK | |
Functions | |
A Proposed Hybrid Solution Scheme for Future Research | |
References | |
The Hydrology of Milled Peat Production | |
Abstract | |
Introduction | |
The Peat-Water System | |
Water Movement in a Peat Column | |
Boundary Conditions at the Pedon Scale | |
The Drying of a Layer of Milled Peat | |
Conclusions | |
Acknowledgements | |
References | |
Role of Active-Passive Scalar Relationships in Evaporation from Vegetated Surfaces | |
Abstract | |
Introduction | |
Efficiency of Evaporation | |
Concept of Active and Passive Scalars | |
Impact of K E /K H Ratio on Traditional Methods of Estimating Evaporation from Vegetated Surfaces | |
Concluding Remarks | |
References | |
On the Weights of Precipitation Stations | |
Abstract | |
The Thiessen Polygon Method is Illogical | |
Weights Should be Determined Considering the Reliability of Observed Data | |
Weights of Precipitation Stations Should be Determined to Obtain Good Results in Discharge Calculation or Flood Forecasting | |
How to Determine the Weights of Precipitation Stations | |
The Problem | |
The Singular Matrix | |
The Method of Principal Axis Transformation | |
Factor Analysis | |
Orthogonal Expansion of the Runoff | |
The Precipitation Weights | |
The Determination of the Cut-Off Pointk 1 | |
References | |
A Neyman-Scott Shot Noise Model for the Generation of Daily Streamflow Time Series | |
Abstract | |
Introduction | |
Definition of a Second Order Neyman-Scott Shot Noise (NSSN) Model | |
Some Moments of the Neyman-Scott Shot Noise Model | |
Some Special Cases | |
Fitting the NSSN Model to Historical Daily Flows | |
Model Validation | |
Discussion and Epilogue | |
Acknowledgements | |
References | |
Large-Scale Hydrology | |
Criteria for a Hydrologically Sound Structuring of Large Scale Land Surface Process Models | |
Abstract | |
Introduction | |
Scales in Hydrology and Related Categories of Hydrological Models | |
Critical Concepts in Macroscale Hydrological Modelling at Land Surfaces | |
Hydrologically Sound Structuring of Macroscale Models | |
Basic Types of Areal Heterogeneity at Land Surfaces and Assessment of Landscape Patchiness | |
Hierarchy in the Areal Discretization of Land Surfaces for Modelling | |
Criteria to Delineate Zones of Uniform Climate Forcing | |
References | |
The Construction of Continental Scale Models of the Terrestrial Hydrological Cycle: An Analysis of the State of-the-Art and Future Prospects | |
Introduction | |
Time-Space Scales and Main Research Directions | |
Continental Scale Hydrological Models with Present-Day Space Resolution of GCMs (100-300 km) | |
Modelling of the Terrestrial Hydrological Cycle for a Horizontal Scale of 30-100 km | |
Opportunities for Developing Parameterisations of the Hydrological Cycle for Horizontal Resolutions of Less than 30km | |
Acknowledgements | |
References | |
A Rainfall-Runoff Scheme for Use in the Hamburg Climate Model | |
Abstract | |
Introduction | |
Runoff in the Context of General Circulation Models | |
Description of the Arno Scheme | |
The Simulated Hydrological Cycle | |
Conclusions | |
Acknowledgement | |
References | |
Transient Response of a Coupled Ocean-Atmosphere-Land Surface Model to Increasing Atmospheric Carbon Dioxide | |
Abstract | |
Introducti | |
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