Abstract

Increasing meteorological drought frequency and rising water demand drive groundwater exploitation beyond sustainable limits. In heavily-stressed aquifers mitigation strategies, such as Managed Aquifer Recharge (MAR), are needed to restore depleted groundwater storage. MAR is also designed to overcome short dry periods. However, wider impacts of MAR as a drought mitigation strategy remain to be quantified. The objective of this study is to assess impacts of MAR in heavily-stressed aquifers using a case study of the Central Valley in California (USA). The novelty of this study lies in its analytical approach based on long-term observational data of precipitation, groundwater levels, and MAR operations. The impact of MAR operations is assessed regionally and for different temporal scales. Results show spatially-coherent clusters of groundwater level time series in the Central Valley representing three main patterns that manifest themselves in different groundwater drought characteristics and long-term trends. The first regional pattern shows lengthened groundwater droughts and declining groundwater levels over time, indicating effects of over abstraction in aquifer sections without MAR. The second regional pattern shows reduced groundwater drought duration and magnitude related to periodically rising groundwater levels, showing short-term MAR impacts. The third regional pattern shows alleviated groundwater droughts and groundwater levels show a long-term rise, representing long-term MAR impacts. Mitigated groundwater droughts and long-term rise in groundwater levels reveal the value of long-term MAR operations and their contribution toward sustainable groundwater management. Increased institutional support is recommended to ensure longevity of MAR and thereby amplify its success as regional drought mitigation strategy in heavily-stressed aquifers.

Highlights

  • Groundwater resources are increasingly pressured due to growing domestic, industrial, and agricultural water demand (Siebert et al 2010, Döll et al 2012)

  • Shortterm and long-term (35-year) patterns in precipitation and groundwater time series are shown, and lastly, groundwater drought characteristics are presented for the 35-year period and the 2012–2015 meteorological drought event

  • RP1 is represented by cluster 1 (CL1) that consists of 31% of all monitoring sites in the northern counties of the Tulare Basin (Kings, Kaweah, and Tulare Lake counties)

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Summary

Introduction

Groundwater resources are increasingly pressured due to growing domestic, industrial, and agricultural water demand (Siebert et al 2010, Döll et al 2012). Few aquifers show decreasing groundwater depletion rates that are realised due to reduced withdrawals (mandatory or voluntarily), improved groundwater management, conjunctive use of surface water and groundwater, and enhanced groundwater recharge (Konikow 2011, Scanlon et al 2016, Dillon et al 2019). These exceptional examples show the potential of mitigation strategies to ensure sustainable groundwater use and avoid maladaptation to meteorological droughts in heavily-stressed aquifers. One of these regions is the Central Valley in California (USA) that has a long history of MAR and is classified as a heavily-stressed aquifer (DWR 2016)

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