170 likes | 301 Views
Modelling of streamflow reduction due to climate change in the Murray-Hotham River catchment. Oral Presentation by Ryan Want Supervisor: Dr Faisal Anwar. Background. Streamflow generation. Climate change The South West of Western Australia (SWWA). 800 600 400 200. May – October.
E N D
Modelling of streamflow reduction due to climate change in the Murray-Hotham River catchment Oral Presentation by Ryan Want Supervisor: Dr Faisal Anwar
Background Streamflow generation
Climate change • The South West of Western Australia (SWWA) 800 600 400 200 May – October Annual Rainfall (mm) May – July August – October 1952 1962 1972 1982 1992 Year
Towns Murray Basin Rivers WA Coastline Murray-Hotham Catchment Murray Basin Murray-Hotham River catchment
Methodology • LUCICAT Modelling Input Data Modelled Streamflow Future Calibrated LUCICAT Model GCM Rainfall Data Modelled Streamflow Current
Input data: - Response units - Attributes & land uses - Channel and node network - Global parameters - Rainfall & evaporation
Calibration of the LUCICAT model - Carried out at 5 gauging stations - Calibrated to within ±5%
General Circulation Models (GCMs) - Future rainfall datasets - 11 different models • Emission Scenarios - Intergovernmental Panel on Climate Change (IPCC) - A2 and B1 emission scenarios 2046 2065 2081 2100
Results • Rainfall Projections Rainfall Reduction (%)
Streamflow Projections Streamflow Reduction (%)
Conclusions • Significant rainfall reductions forecast over the next century • Streamflow response projected to be even more dramatic
GCM Variation • Modelling Uncertainty • Projections are not predictions • SWWA faces huge challenge
Recommendations • Further research into modelling uncertainty • Rainfall data sourced by several different methods to eliminate bias • Further research into pan evaporation levels is needed
Significance • Up to date and accurate projections • Current data up to 2010 • Water Resource Managers: - Catchment management strategies - Plan for the future