- 1Division of Hydrologic Sciences, Desert Research Institute, Reno, United States of America (beatrice.gordon@dri.edu)
- 2ORISE Postdoctoral Research Fellow, Fort Collins, Colorado, United States of America (joey.blumberg@gmail.com)
- 3Baker School of Public Policy, University of Tennessee, Knoxville, United States of America (dtmanning@utk.edu)
- 4Haub School of Environment and Natural Resources, University of Wyoming, Laramie, United States of America (bleonard@uwyo.edu)
- 5Aythya Analytics, Reno, United States of America (austen@aythyaanalytics.com)
- 6College of Agriculture, Biotechnology, and Natural Resources, University of Nevada-Reno, Reno, United States of America (aharpold@unr.edu)
- 7Director of Prescribed Fire, All Hands Ecology, Petaluma, United States of America (julia.berkey@gmail.com)
Climate change is altering snow accumulation and ablation dynamics in snow-dependent regions worldwide, reshaping runoff timing and water availability for people, ecosystems, and agriculture. As the world’s largest consumer of freshwater, irrigated agriculture is particularly exposed, and these hydrologic changes impose substantial economic costs. Here, we demonstrate how hydrology and economics can be combined to assign costs to snow-driven hydrologic change, using irrigated agriculture in the western United States as a large, snow-dependent test case. By integrating reduced-form economic models with climate model projections spanning approximately 2–5 °C of warming, we estimate that irrigated cropland could decline by 27–46% by the end of the century, while agricultural profitability—proxied using land rental rates—declines by 11–26%, corresponding to annual losses of approximately $8.2–$14.7 billion. Against this economic backdrop, scientists have an opportunity to leverage expanding data and modeling capabilities to provide actionable information about adaptation strategies that can reduce damages.
However, there remains a persistent gap between the scales at which snow loss research is conducted and the scales at which land and water management decisions are made. To address this challenge, we propose that archetypes—drawn from social-ecological systems research—could help accelerate matching adaptation strategies to specific decision-making contexts by explicitly accounting for governance capacity and behavioral dynamics. This approach has not been widely explored in agricultural adaptation to snow hydrology but could enable rapid, locally-relevant guidance.
Yet rapid adaptation without integration across hazards risks unintended consequences. Through analysis of four decades of fire perimeter data (1984-present) and aerial imagery, we show that cropland is 2x less likely to be on the inside of a fire perimeter than any other land-cover type, suggesting an important landscape-scale buffering effect. Using drought and wildfire as an example, this finding demonstrates how cropland abandonment—a strategy that may enhance drought resilience—could amplify fire risk if poorly coordinated, illustrating how rational responses to one hazard can inadvertently increase exposure to others. Results underscore the complexity of adaptation under compounding climate risks and the importance of working in partnership with decision-makers to leverage ever expanding data and modeling capabilities for locally-relevant solutions.
How to cite: Gordon, B., Blumberg, J., Carroll, R., Manning, D., Leonard, B., Boisrame, G., Lorenz, A., Harpold, A., Berkey, J., Cough, C., and Albano, C.: Snow Loss, Economic Cost, and Potential (Mal)Adaptation in Irrigated Agriculture: Case Studies from the Western US, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-15921, https://doi.org/10.5194/egusphere-egu26-15921, 2026.