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Hydrologic mechanisms for 2022 Yellowstone River flood and comparisons to recent historic floods

Jeremy Giovando·Wyatt Reis·Wei Zhang·Nancy A. Barth
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Abstract

In June 2022, a historic flood event occurred in the headwaters of the Yellowstone River Basin. The flood resulted in millions of dollars in damages and substantial interruptions to Yellowstone National Park. The 2022 flood event was substantially higher in magnitude than other high-peak flow events over the last 30 years. The high discharge was primarily due to the combination of hydrologic mechanisms initiated by rain-on-snow, including a high-elevation snowpack that peaked later than average. However, the contributions of each hydrologic driver, rain and snow, have not been quantified and could be important for understanding future flood events in the region. The contribution of snowmelt to the total terrestrial water input (TWI) varied throughout the area, yet was concentrated in the headwaters of the Yellowstone, Stillwater, and Boulder rivers, along with the headwaters of Rock Creek in Wyoming and Montana. The primary atmospheric contributions to the TWI during the 2022 event were precipitation from moisture transported from the Pacific Ocean that converged over the Greater Yellowstone Area (GYA) and snowmelt from residual snowpack in the northeast part of Yellowstone National Park.

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Hydrological ProcessesArticle
90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 43.909029192960446° to 45.53668572000356° latitude; -111.8645863474894° to -108.86233230449172° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Jeremy Giovando, Wyatt Reis, Wei Zhang, Nancy A. Barth. 2025-03-13. Hydrologic mechanisms for 2022 Yellowstone River flood and comparisons to recent historic floods. https://doi.org/10.1002/hyp.70099

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