The introduction of stochastic streamflow models by Fiering (1967), Maass et al. (1962), and others led to a revolution in water resources planning, design, and management. These models enabled hydrologists to generate representative streamflow ensembles over future planning horizons, needed to explore the consequences of future hydrologic conditions not experienced historically, and formally characterize the reliability, vulnerability, and resilience of water resource systems (Hashimoto et al., 1982;Loucks & van Beek, 2017). Traditional stochastic streamflow models are typically statistical models rather than mechanistically driven hydrologic models. Such stochastic streamflow models may be adjusted to reflect changes in seasonality or other statistical properties of flow (e.g., Quinn et al., 2018), but tying statistical hydrologic changes to climate and land use change is