Amplification of Cretaceous Warmth by Biological Cloud Feedbacks
- 1 Department of Geosciences and Earth System Science Center, Pennsylvania State University, University Park, PA 16802, USA.
- 2 Earth and Environmental Systems Institute, Pennsylvania State University, University Park, PA 16802, USA.
- ↵* To whom correspondence should be addressed. E-mail: lkump{at}psu.edu
Abstract
The extreme warmth of particular intervals of geologic history cannot be simulated with climate models, which are constrained by the geologic proxy record to relatively modest increases in atmospheric carbon dioxide levels. Recent recognition that biological productivity controls the abundance of cloud condensation nuclei (CCN) in the unpolluted atmosphere provides a solution to this problem. Our climate simulations show that reduced biological productivity (low CCN abundance) provides a substantial amplification of CO2-induced warming by reducing cloud lifetimes and reflectivity. If the stress of elevated temperatures did indeed suppress marine and terrestrial ecosystems during these times, this long-standing climate enigma may be solved.
- Received for publication 7 December 2007.
- Accepted for publication 19 February 2008.
