Alan M. Rhoades

Apr 9, 2024 | journals.ametsoc.org | William Rudisill |Alan M. Rhoades |Zexuan Xu |Daniel Feldman

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Oct 30, 2023 | journals.ametsoc.org | Yalan Song |Wen-Ping Tsai |Alan M. Rhoades |Jonah Gluck

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Oct 12, 2023 | agupubs.onlinelibrary.wiley.com | Alan M. Rhoades |Colin Zarzycki |Mohammed Ombadi |Héctor A. Inda-Diaz

1 Introduction California is especially susceptible to major cool season flood events (Kattelmann, 1997). Atmospheric rivers (ARs) are largely responsible, accounting for 84% of flood damages in the western United States (Corringham et al., 2019). The most notable California flood event, measured by its intensity, duration, and inundation area, occurred in 1861/1862 (X. Huang & Swain, 2022; Porter et al., 2011).

Jun 28, 2023 | nature.com | Mohammed Ombadi |Mark D. Risser |Alan M. Rhoades

AbstractThe intensity of extreme precipitation events is projected to increase in a warmer climate1,2,3,4,5, posing a great challenge to water sustainability in natural and built environments. Of particular importance are rainfall (liquid precipitation) extremes owing to their instantaneous triggering of runoff and association with floods6, landslides7,8,9 and soil erosion10,11.