Attributing the Causes of a Century of Hydroclimatic Change in the United States
Hydroclimate in the United States (US) is climatologically divided by the 100th meridian. The semi-arid western US has experienced high-amplitude multidecadal swings in drought and soil moisture variability over the last millennium, culminating in anthropogenic warming-driven drying into the early p...
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| Language: | English |
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2021
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| Online Access: | https://doi.org/10.7916/d8-cwj0-2058 |