Intensive pumping of groundwater for irrigated agriculture is causing high water level decline rates in many regions (Alley & Alley, 2017;Bierkens & Wada, 2019), threatening both potable water supplies and agricultural production (Khan et al., 2016;Scanlon et al., 2012). Effective tools are required to support decisions related to the management of groundwater resources in these regions. A conventional approach to providing such decision support would be to build a groundwater flow model representing the subsurface system, calibrate it to match historical groundwater level responses and other targets (e.g., streamflows), and then use it to predict responses to proposed future pumping and climate scenarios. However, this process is both time-consuming and fraught with uncertainty (Anderson et al., 2015;Hill & Tiedeman, 2007). Moreover, in their quest to build accurate models of complex hydrogeological systems, investigators may lose sight of the need for providing timely information that is pertinent to the decision at hand (Doherty & Moore, 2020;Ferré, 2017). In that vein, some have advocated seeking more direct means to link historical data and forecasts of interest (Hermans, 2017;Satija & Caers, 2015). A recently developed water balance method (Butler et al., 2016(Butler et al., , 2018 provides a direct means for forecasting the near-term impact of changes in total pumping on areally averaged water level changes, based on the premise that, due to the slowly changing nature of