The Lessons of Mid-Holocene Droughts
We have been told over and over that the buildup of greenhouse gases will vastly alter climate all over the world. The planet will be warmer, precipitation will be greater, droughts and floods will savage civilization, and everything will be worse than we could ever believe. In the case of the central United States, we have been warned repeatedly that higher atmospheric concentrations of greenhouse gases will lead to a substantial increase in the duration, severity, and areal extent of droughts in the American heartland.
A recent issue of Geophysical Research Letters includes two articles that shed light on the future (and past) of droughts in the central United States. The first article was produced by five climatologists from academic units at Purdue, Minnesota, Wisconsin, and Oregon. Diffenbaugh et al. focused on the Mid-Holocene period between 8,000 and 3,000 years ago — a period for which the proxy record clearly shows drier-than-present conditions throughout the central United States. They note that “Proxy data also indicate that changes in summer precipitation played a major role in shaping mid-Holocene moisture balance in North America.” Back then, summers were a lot drier than today, despite any lack of elevated concentration of greenhouse gases.