Journal
WEATHER AND CLIMATE EXTREMES
Volume 32, Issue -, Pages -Publisher
ELSEVIER
DOI: 10.1016/j.wace.2021.100326
Keywords
Atmospheric rivers; Western United States; Climate change; Societal impacts; Detection and attribution; Stabilized warming scenarios
Categories
Funding
- Office of Biological and Environmental Research of the U.S. Department of Energy
- Regional and Global Climate Modeling Program (RGCM) program under the Calibrated and Systematic Characterization, Attribution and Detection of Extremes (CASCADE) Science Focus Area [DE-AC02-05CH11231]
- A Framework for Improving Analysis and Modeling of Earth System and Intersectoral Dynamics at Regional Scales project [DESC0016605]
- Aotearoa New Zealand Ministry of Business, Innovation and Employment's Endeavour Fund
- National Energy Research Scientific Computing Center (NERSC) [DEAC0205CH11231]
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The study shows that as global warming intensifies, the number of landfalling atmospheric rivers (ARs) and the amount of water they transport will increase. The proportion of beneficial ARs will decrease, while the proportion of hazardous ARs will increase. This shift will result in a gradual increase in flood damages, highlighting the importance of climate mitigation efforts.
Atmospheric rivers (ARs) are critical to the hydrological cycle of the western United States with both favorable and formidable impacts to society based on their landfalling characteristics. In this study, we provide a first-of-its-kind evaluation of how landfalling ARs may respond to several stabilized warming scenarios. To do this we combine a recently developed AR detection workflow with an ensemble of uniform high-resolution (0.25 degrees degrees) Community Earth System Model simulations designed to facilitate detection and attribution of extreme events with global warming. These simulations include a world that might have been in the absence of anthropogenic warming (+0 degrees C), a world that corresponds to present day warming (+0.85 degrees C), and several future worlds corresponding to +1.5 degrees C, +2 degrees C and +3 degrees C global warming. We show that warming increases the number of water management relevant landfalling ARs from 19.1 ARs per year at +0 degrees C to 23.6 ARs per year at +3 degrees C. Additionally, this warming intensifies the amount of water transported by landfalling ARs resulting in a decrease in the fraction of ARs that are mostly to primarily beneficial to water resource management (i.e., 91% of ARs at +0 degrees C to 78% at +3 degrees C) and an increase in the fraction of ARs that are mostly or primarily hazardous to water resource management (i.e., 2% of ARs at +0 degrees C to 8% at +3 degrees C). Shifts in AR character also have important ramifications on flood damages, whereby for every +1 degrees C of additional warming from present conditions annual average flood damages increase by similar to$1 billion. These findings highlight the pragmatic implications of climate mitigation aimed at limiting global warming to under +2 degrees C.
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