Effects of future climate change on groundwater in ...

Object Details

View

XVI International Conference on Computational Methods in Water Resources (CMWR-XVI) Ingeniørhuset

Effects of future climate change on groundwater in Denmark
Paper
Author:Lieke van Roosmalen <lvr@geol.ku.dk> (PhD. student Geological Institute, Copenhagen University)
Jens Hesselbjerg Christensen <jhc@dmi.dk> (Senior researcher, Danish Meteorological Institute)
Jens Christian Refsgaard <jcr@geus.dk> (Research professor, Geological Survey of Denmark and Greenland (GEUS))
Karsten Høgh Jensen <khj@geol.ku.dk> (Professor, Geological Institute, Copenhagen University)
Michael Butts <mib@dhi.dk> (Senior hydrologist, Danish Hydrological Institute)
Presenter:Lieke van Roosmalen <lvr@geol.ku.dk> (PhD. student Geological Institute, Copenhagen University)
Date: 2006-06-18     Track: Special Sessions     Session: Global Climate Change and Hydrologic Processes
DOI:10.4122/1.1000000477
DOI:10.4122/1.1000000478

The water supply in Denmark is entirely based on groundwater and it is therefore of concern how climate change will affect the groundwater reserves in the future. We have analyzed this problem by retrieving climatological output data from a regional climate model and using this data in a distributed hydrological model, focusing on a selected watershed in the country. Global climate models simulate the global climate system with greenhouse gas concentrations representing observed and possible future conditions, but their limited regional detail makes them less suitable for hydrological impact studies. Therefore, regional climate models with a limited model domain and higher resolution are utilized. In this study the regional climate model HIRHAM from the Danish Meteorological Institute is used with boundary conditions generated by the global climate model HadAM3H from Hadley Centre. The concentrations of greenhouse gas and aerosols, have been applied based on the IPCC SRES A2 emission scenario. The climate model output consists of data for two time slices, one for a period representing recent climate (1961-1990; control run) and one for the future climate (2071-2100; scenario run). The climate output used is daily precipitation, temperature and potential evapotranspiration, all at a 12x12 km resolution. Climate models are subject to systematic biases, so climate model data cannot be used directly in hydrological models. Different transfer methods exist to transfer the signal of climate change, of which two will be examined in this study. One is the so-called delta change approach, that alters the original hydrological model input data with a factor deduced from the climate model output data to generate the input data for the hydrological simulation of the future scenario. The other method is the direct method, that uses the climate model output directly as input for the hydrological model after correcting the climate output with factors based on the bias between the climate model control scenario data and the original hydrological model input data. We use the so-called DK model as the model for the hydrological analysis. The DK- model divides Denmark into 10 regions and it is based on the distributed hydrological model code MIKE SHE with a horizontal spatial discretization of 1 x 1 km2. One of these regions has been selected as the study area for the impact analysis.