Atmospheric rivers produce more heavy precipitation on western coasts due to prevailing westerlies and topography
Atmospheric rivers frequently drive heavy precipitation along western coasts as moisture-laden winds interact with coastal mountain ranges.
The retrieved literature consistently confirms that atmospheric rivers, steered by prevailing westerlies, encounter coastal topography and produce heavy orographic precipitation along western coasts such as western North America and New Zealand.
L. Ruby Leung, Yun Qian. Atmospheric rivers induced heavy precipitation and flooding in the western U.S. simulated by the WRF regional climate model. 2009. https://doi.org/10.1029/2008gl036445
Simulations demonstrate how atmospheric rivers cause heavy precipitation and flooding in the western U.S.
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Aseem R. Sharma, S. Déry. Contribution of Atmospheric Rivers to Annual, Seasonal, and Extreme Precipitation Across British Columbia and Southeastern Alaska. 2020. https://doi.org/10.1029/2019JD031823
Shows that prevailing midlatitude westerlies drive atmospheric rivers that produce heavy coastal precipitation in British Columbia and Alaska.
R. Mo, M. Brugman, J. Milbrandt, J. Goosen, Qu Geng, Chris Emond, Jonathan Bau, A. Erfani. Impacts of Hydrometeor Drift on Orographic Precipitation: Two Case Studies of Landfalling Atmospheric Rivers in British Columbia, Canada. 2019. https://doi.org/10.1175/WAF-D-18-0176.1
Examines how landfalling atmospheric rivers interact with topography to produce orographic precipitation in British Columbia.
Shu J, Shamseldin AY, Weller E. The impact of atmospheric rivers on rainfall in New Zealand.. 2021. https://doi.org/10.1038/s41598-021-85297-0
Quantifies how atmospheric rivers generate heavy rainfall totals and extreme events on the western side of mountainous areas in New Zealand.
Tamar S. Richards-Thomas, Stephen J. Déry. Moisture transport to British Columbia’s upper Nechako Watershed associated with three atmospheric rivers. 2025. https://doi.org/10.1007/s44292-025-00035-9
Demonstrates that moisture transport from atmospheric rivers undergoes orographic lifting over coastal mountains to produce intense precipitation.
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