HIGH DEMAND AND CLIMATE CHANGE: PROMINENT CHALLENGES FOR FUTURE WATER RESOURCES IN NORTH TEXAS
Simultaneously, the surface water resources that supply most of North Texas are likely to decline as a result of climate change. IPCC climate change models indicate an initial ~20-year period of slightly wetter conditions, which appears to have begun in the 1990's, (e.g. observed 1.5 inch increase in annual precipitation in the region vs. pre-1975 values). After 2020 predictions indicate minor drying accompanied by major warming. The net climate effect is readily illustrated by monthly Palmer Drought Severity Indices (PDSI) based on predicted temperature and precipitation. An ensemble mean of PDSI calculated from intermediate severity warming models (IPCC-SRESa1b) indicates initially wet conditions transitioning to permanent moderate drought after 2050. Values are: observed PDSI 1980-2000: +1.1, predicted 2000-2020: +0.26, 2040-2060: -0.57, 2080-2100: -1.4. Strong correlation of annual mean stream discharge with PDSI (Spearman rank indicates 99.9% confidence) allows prediction of future streamflow given PDSI. Doing this for streams supplying major reservoirs in North Texas indicates a climate-related decline in average streamflow of 30%-50% by 2050. Increased precipitation variability may allow reservoirs to moderate the short-term effects of such a decline, but in the long run, reliability of reservoirs may be threatened.