As a result, regional stakeholders, water managers and researchers have been working to address the failures of past lake level models and implement a new diversion policy. This incredibly difficult task is even further complicated by the uncertainty surrounding the impact of climate change on recent and future hydrological conditions, which current lake level models neglect to consider. In this study, we aim to improve future Mono Lake level predictions through the development of a climate change driven lake level model. We then use this model to implement a flexible policy optimization in order to support decision makers as they balance numerous and often conflicting stakeholder objectives.
To evaluate future conditions, our model predicts annual Mono Lake levels from 2024 to 2100 based on the atmospheric and hydrologic conditions from a suite of downscaled CMIP6 data. Our modeling approach was informed by technical experts from multiple agencies and organization that specialize in Mono Lake hydrology, infrastructure and water management. We use single realizations from 11 GCMs under SSP245, SSP370 and SSP585 to capture a wide range of possible future climates and natural variability sequences. To account for varying water management strategies, we implement flexible diversions based on lake level and hydrologic conditions, which allows us to evaluate a wide range of policies. In collaboration with multiple stakeholders, we select key performance objectives and use an iterative optimization algorithm which generates and tests thousands of potential policies in order to narrow in on the best performing policies. Our approach is designed to optimize performance across several objectives as well as balance conflicting objectives and quantify any compromises. The intention of this is to provide decision makers with a flexible framework to understand the limits of the system and explore different ways of balancing various constraints and priorities.
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