Drivers and projections of ice phenology in mountain lakes in the western United States

Limnology and Oceanography
By: , and 

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Abstract

Climate change is causing rapid warming and altered precipitation patterns in mountain watersheds, both of which influence the timing of ice breakup in mountain lakes. To enable predictions of ice breakup in the future, we analyzed a dataset of mountain lake ice breakup dates derived from remote sensing and historical downscaled climate data. We evaluated drivers of ice breakup, constructed a predictive statistical model, and developed projections of mountain lake ice breakup date with global climate models. Using Random Forest analysis, we determined that winter and spring cumulative snow fraction (portion of precipitation falling as snow) and air temperature are the strongest predictors of ice breakup on mountain lakes. Interactions between precipitation, cumulative winter air temperature and lake surface area indicate that shifts in air temperature and precipitation affect smaller lakes (< 2 km2) more than larger lakes (> 2–10 km2). A linear mixed effects model (RMSE of 18 d), applied with an ensemble of 15 global climate models, projected that end-of-century ice breakup in mountain lakes will be earlier by 25 ± 4 and 61 ± 5 (mean ± SE) days for representative concentration pathways 4.5 and 8.5, respectively.

Study Area

Publication type Article
Publication Subtype Journal Article
Title Drivers and projections of ice phenology in mountain lakes in the western United States
Series title Limnology and Oceanography
DOI 10.1002/lno.11656
Volume 66
Issue 3
Year Published 2021
Language English
Publisher Association for the Sciences of Limnology and Oceanography
Contributing office(s) WMA - Earth System Processes Division
Description 14 p.
First page 995
Last page 1008
Country United States
State California, Idaho, Oregon, Washington
Other Geospatial Cascade Mountains, northern Rocky Mountains, Sierra Nevada Mountains
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