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Author/Chair
Stephen Jackson
University of Wyoming
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Meeting roles in:
Zonal hydroclimate dipole in Central US controlled by North Atlantic Subtropical High over the last 20,000 years
Eastern North American hydroclimate connected to North Atlantic Subtropical High weakening across the most recent deglaciation
Links & Materials
Zonal hydroclimate dipole in Central US controlled by North Atlantic Subtropical High over the last 20,000 years
Eastern North American hydroclimate connected to North Atlantic Subtropical High weakening across the most recent deglaciation
