Published June 2, 2026 | Version v1
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Anthropogenic Climate Forcing in the American Southwest: From the Colorado River Compact to the Modern Megadrought

Description

The American Southwest entered a new climate era approximately 1900 AD when industrial-scale water management began to reshape the region's hydrology. This paper examines how anthropogenic interventions—including the 1922 Colorado River Compact, construction of Hoover Dam, California's Central Valley irrigation system, and massive groundwater extraction—have inadvertently replicated geological processes that operated during the Pliocene. We demonstrate four key anthropogenic climate forcings: (1) the Colorado River Compact allocated water based on measurements from the wettest period in 1,300 years, creating a structural deficit that persists today; (2) Central Valley irrigation strengthens the southwestern U.S. water cycle by ~15% and increases Colorado River streamflow by ~30%, while simultaneously depleting 160 km³ of groundwater that produces measurable crustal uplift and modulates San Andreas Fault seismicity; (3) Hoover Dam and Lake Mead created reservoir-induced seismicity on the same fault systems affected by Pliocene mass transfer; and (4) Las Vegas grew from 8,000 to 2.2 million people drawing on the same karst aquifer system drained by Grand Canyon incision over 5 million years. Tree-ring reconstructions show the current megadrought (2000–present) is the most severe since at least 800 AD, raising the question of whether the region is returning to Medieval Climate Anomaly conditions amplified by anthropogenic warming. The Nile Delta provides a global analog: three major deltas (Nile, Mississippi, Gulf of California) demonstrate that sediment-loading subsidence is a universal phenomenon with civilization-scale consequences, from the documented submersion of ancient Alexandria to modern coastline loss and sediment starvation. These findings demonstrate that modern water management decisions are inseparable from the geological forces that shaped the region.

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