Modeling of bore hydrographs to determine the impact of climate and land-use change in a temperate subhumid region of southeastern AustraliaModélisation d’hydrogrammes de puits pour déterminer l’impact des variations climatiques et modes d’utilisation du sol dans une région tempérée semi-humide d’Australie du SudModelado de hidrogramas de pozos para determinar el impacto del clima y el cambio del uso de la tierra en una región templada subhúmeda en el sudeste de Australia钻孔水位模拟确定澳东南部温带半湿润地区气候和土地利用变化的影响Modelação dos hidrogramas de furos para determinação do impacte das alterações climáticas e de uso do solo numa região temperada sub-húmida do sudeste da Austrália

To determine the relative impact of climate and human intervention on groundwater elevations in western Victoria, southeast Australia, bore hydrograph fluctuations in three aquifers were modelled using a transfer function noise model (PIRFICT) and an auto-regressive model (HARTT), which give generally comparable results. Most of the groundwater-level fluctuations (>90%) are explained by climatic variation, particularly rainfall. The overall non-climate-related trend in groundwater level is downward and small but statistically significant (−0.04 to −0.066 m/yr), and is probably due to the widespread replacement of grazing land by wheat and canola cultivation, as these crops use more water than pasture. A large non-climate-related trend (−0.30 m/yr) for bores in an irrigation area is mainly related to groundwater extraction. The response time of the system is rapid (only 4.85 years on average), much faster than previously estimated. Rates of groundwater flow are much slower; groundwater ages are up to ~35,000 years. Response times effectively represent the time for the system to move to a new state of hydrologic equilibrium; this prediction of the time scale of the impacts of land-use change on groundwater resources will allow the development of better strategies for groundwater management.