Shifts in stream salt loads during and after prolonged droughts

It has been widely assumed that after prolonged droughts, catchment runoff recovers to pre-drought levels. This assumption has recently been evaluated and challenged using empirical observations. However, water quality response and recovery, or otherwise, during and after prolonged droughts remains an open question. Answering this question potentially identifies any changes in catchment hydrological processes and water balance (e.g., the proportion of groundwater contribution to streamflow), thus informing the mechanisms for runoff non-recovery after prolonged drought. Water quality responses to drought can also inform any long-term water quality changes beyond what is observable from trend analyses. Here stream salt load changes were investigated using hidden Markov models (HMMs), where monthly rainfall was included as a predictor of stream salt loads. Monthly riverine salt fluxes at eight sites in Victoria (Australia) were examined before, during and after a prolonged drought in South-East Australia-the Millennium Drought. Two-state models, where salt loads varied between 'normal' and 'low' states, were found to better predict in-stream salt loads compared to single-state models. The results showed that catchments shifted to a low salt load state generally after the catchment changed to a low runoff state. As groundwater is understood to be the major source of salts in these catchments, this suggests that reductions in groundwater flow into rivers occur as a result of the shift to a lower runoff state. Understanding how readily water quality in catchments shift to different states during and after prolonged droughts enables appropriate catchment management based on our understanding of changes to catchment hydrology.

Automated summary

It is not widely accepted that water quality recovers to pre-drought levels after prolonged droughts, and there is still no clear answer to this question. By studying the changes in riverine salt load, it was found that the salt load decreases when the catchment shifts to a low runoff state. This suggests that reduced groundwater flow into rivers occurs as a result of the shift to a lower runoff state.