Even from the proxy data that exist, one thing is relatively certain: our climate system is not always well-behaved. It can, and often does, change in surprising ways. Positive feedbacks are a key ingredient for this behavior, amplifying a small change or perturbation in the climate system. Paleo records also show that abrupt changes happen during both glacial and interglacial periods, although they may take on different characteristics when large ice sheets exist on Earth. During the Holocene, for example, regional-scale droughts have been very important, while weakening of the meridional overturning circulation had consequences on the hemispheric-to-global scale during the last glacial period.
The perspective of the paleo record suggests that future climate change will also contain some surprises. Currently, global mean temperature is rising due to emissions of greenhouse gases by humans (see the Paleo Perspective on Global Warming). It is possible that this climate perturbation will be amplified by some of the positive feedbacks that operated during past abrupt events. The Arctic, for example, might become a locus of abrupt change due to the ice-albedo feedback (Holland et al., 2006).
Should I Worry?
It is important not to be fatalistic about the threats posed by abrupt climate change.
At this point, we know that abrupt climate change is a reality. It has happened before and will happen again. How and why it happened in the past are still open questions, as are how, why, and when it might happen in the future. The information found in natural archives of climate and environmental change such as ice cores, lake and ocean sediments, tree rings, and other proxies can be of profound benefit to society in understanding and predicting future climate change.
The goal of the World Data Center for Paleoclimatology is to provide easy access to high quality scientific information derived from rigorous studies of past climate changes. We believe, as do most climate scientists, that the topic of abrupt climate change is worthy of further study, and needs more information before predictions can be made about future events. Several national and international initiatives, such as the U.S. Climate Change Science Plan, have targeted this topic as a priority for scientific research.
Downloaded Thursday, 31-Jul-2014 16:28:23 EDT
Last Updated Wednesday, 20-Aug-2008 11:21:31 EDT by firstname.lastname@example.org
Please see the Paleoclimatology Contact Page or the NCDC Contact Page if you have questions or comments.