LAMONT-DOHERTY EARTH OBSERVATORY
THE EARTH INSTITUTE
AT COLUMBIA UNIVERSITY
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Global Decadal Hydroclimate
Western North American Climate
In Depth Discussions on Drought Research
Causes and Dynamics of the Early 20th Century North American Pluvial
Thermodynamic and dynamic mechanisms for large-scale changes in the hydrological cycle in response to global warming
Greenhouse warming and the 21st century hydroclimate of Southwestern North America
Was the recent drought in the southeastern United States exceptional, typical, a result of anthropogenic climate change, etc.?
Why does the North Pacific storm track move south during El Niño winters?
Mexican drought: natural variability and climate change from the Medieval period to the greenhouse future
Did dust storms make the Dust Bowl drought worse?
An imminent transition to a more arid climate in southwestern North America
Was the Dust Bowl predictable?
Causes and consequences of nineteenth century droughts in North America
The characteristics and likely causes of the Medieval megadroughts in North America
Maintained by:
Virginia DiBlasi
, Lamont-Doherty Earth Observatory of Columbia University
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