Capturing hydrological variability : Spatio-temporal aspects of the Rhine basin

Abstract

Introduction 2 | Hydrological systems complexity and a drought frequency paradox 3 | Interaction between soil moisture and vegetation during drought 4 | The role of model resolution during seasonal hydrological extremes 5 | A new hydrological model for high resolution simulations 6 | The response of snow, evaporation, and discharge to higher temperatures 7 | Sensitivity of evaporation and low flows to CO 2 -induced changes in temperature and vegetation 8 | Synthesis 9 | Appendices Bibliography Summary Samenvatting Dankwoord List of publications Graduate school certificate v "I know the falls that the water face I know it's over, an ocean awaits for a storm The sun on snow, rivers in rain Crystal ball can foresee a change" -Coldplay, Fun (2015) Hydrological systems complexity and a drought frequency paradoxThis chapter is based on: