Status: this preprint was under review for the journal HESS but the revision was not accepted.
Catchment-scale groundwater recharge and vegetation water use efficiency
Peter A. Troch,Ravindra Dwivedi,Tao Liu,Antonio Alves Meira Neto,Tirthankar Roy,Rodrigo Valdés-Pineda,Matej Durcik,Saúl Arciniega-Esparza,and José Agustín Breña-Naranjo
Abstract. Precipitation undergoes a two-step partitioning when it falls on the land surface. At the land surface and in the shallow subsurface, rainfall or snowmelt can either runoff as infiltration/saturation excess or quick subsurface flow. The rest will be stored temporarily in the root zone. From the root zone, water can leave the catchment as evapotranspiration or percolate further and recharge deep storage. It was recently shown that an index of vegetation water use efficiency, the Horton index (HI), could predict deep storage dynamics. Here we test this finding using 247 MOPEX catchments across the conterminous US. Our results show that the observed HI is indeed a reliable predictor of deep storage dynamics. We also find that the HI can reliably predict the long-term average recharge rate. Our results compare favorably with estimates of average recharge rates from the US Geological Survey. Previous research has shown that HI can be estimated based on aridity index, mean slope and mean elevation of a catchment (Voepel et al., 2011). We recalibrated Voepel’s model and used it to predict the HI for our catchments. We then used these predicted values of the HI to estimate average recharge rates for our catchments, and compared them with those estimated from observed HI. We find that the accuracies of our predictions based on observed and predicted HI are similar. This provides a novel estimation method of catchment-scale long-term average recharge rates based on simple catchment characteristics, such as climate and topography, and free of discharge measurements.
How to cite. Troch, P. A., Dwivedi, R., Liu, T., Meira Neto, A. A., Roy, T., Valdés-Pineda, R., Durcik, M., Arciniega-Esparza, S., and Breña-Naranjo, J. A.: Catchment-scale groundwater recharge and vegetation water use efficiency, Hydrol. Earth Syst. Sci. Discuss. [preprint], https://doi.org/10.5194/hess-2018-449, 2018.
Received: 24 Aug 2018 – Discussion started: 17 Sep 2018
Recharge to bedrock aquifers is an important source of water availability and sustains streamflow during long dry periods. It is therefore an important component in the catchment water balance that sustains aquatic ecosystems. Our study shows that it is possible to predict average recharge rates at the catchment scale using only climate and landscape properties. This is an important finding as it is notoriously difficult to measure and/or estimate recharge rates at large spatial scales.
Recharge to bedrock aquifers is an important source of water availability and sustains...