What Have We Learned from Paleoclimatology?

Image of Quelccaya ice cap

The distinct seasonality of precipitation at locations like the Quelccaya ice cap, pictured here, results in dry-season dust bands in some ice cliffs. These layers are extremely useful to paleoclimatologists because they allow ice core records to be dated very accurately. Photo Credits: Lonnie Thompson, Byrd Polar Research Center, Ohio State University

To understand and predict changes in the climate system, we need a more complete understanding of seasonal-to-century scale climate variability than can be obtained from the instrumental climate record. So, several decades ago, paleoclimatologists began constructing a blueprint of how the Earth's temperature changed over the centuries before 1850 and the widespread use of thermometers. Out of this initial work emerged a view of the past climate based on limited data from tree rings, historical documents, sediments, and other proxy data sources. Today, many more paleoclimate records are available from around the world, providing a much improved view of past changes in the Earth's temperature.

From the paleoclimate perspective, climate change is normal and part of the Earth's natural variability related to interactions among the atmosphere, ocean, and land as well as changes in the amount of solar radiation reaching Earth. The geologic record also includes a variety of evidence for large-scale climate changes. For example, warm climate vegetation, dinosaurs, and corals living at high latitudes about 90–120 million years ago indicate globally warm conditions at that time.

Paleoclimate data has also shown that glacial cycles, a pattern of ice ages and glacial retreats lasting thousands of years, dominated the climate of the past two million years. During the peak of the most recent glacial cycle, about 21,000 years ago, massive terrestrial ice sheets extended over large parts of North America and Europe and global temperature was about 9°F colder than today. Since the end of the last ice age over 10,000 years ago, the planet has undergone many changes in climate. Warming during medieval times and cooling during the “Little Ice Age” a few centuries ago dominate the last millennia.

Paleoclimatology also puts recent changes in the atmosphere and climate into perspective. For example, gas bubbles trapped in ice cores tell us that atmospheric carbon dioxide levels are now significantly higher than they have been over at least the last 800,000 years. Prior to the Industrial Revolution, when humans began burning large amounts of fossil fuels, carbon dioxide levels varied within an envelope of 180 to 280 parts per million across glacial and interglacial cycles. Today, in 2014, carbon dioxide levels have reached nearly 400 parts per million. (Learn more about the Carbon Tracker and see how NOAA tracks carbon dioxide levels today.)

Paleoclimate records from multiple proxies also indicate that global temperatures, which have risen with atmospheric carbon dioxide levels, are now higher than at any point in the last 1,500 years. Our planet has likely not been as warm as it is today since over 5,000 years, when changes in the Earth’s orbit increased temperature in some parts of the world. What is especially remarkable is that the long-term cooling trend that has existed over the past 5,000 or more years has reversed abruptly and global temperatures have risen from the coldest to near the warmest levels of our current interglacial period within the last century.

Visit the Paleoclimatology Data page to learn more about and access all of the historical data NCDC’s Paleoclimatology Program stewards.