Synthesis and Assessment: Abrupt Climate Change
The U.S. Geological Survey has led an assessment authored by a team of climate scientists from the Federal government and academe. The report (Synthesis and Assessment Product 3.4: Abrupt Climate Change) was commissioned by the U.S. Climate Change Science Program with contributions from the National Oceanic and Atmospheric Administration and the National Science Foundation.
The assessment notes that the United States faces the potential for abrupt climate change in the 21st century that could pose clear risks to society in terms of our ability to adapt. “Abrupt” changes can occur over decades or less, persist for decades more, and cause substantial disruptions to human and natural systems.
The report, based on an assessment of published science literature, makes the following conclusions about the potential for abrupt climate changes from global warming during this century:
- Climate model simulations and observations suggest that rapid and sustained September arctic sea ice loss is likely in the 21st century.
- The southwestern United States may be beginning an abrupt period of increased drought.
- It is very likely that the northward flow of warm water in the upper layers of the Atlantic Ocean, which has an important impact on the global climate system, will decrease by approximately 25–30 percent. However, it is very unlikely that this circulation will collapse or that the weakening will occur abruptly during the 21st century and beyond.
- An abrupt change in sea level is possible, but predictions are highly uncertain due to shortcomings in existing climate models.
- There is unlikely to be an abrupt release of methane, a powerful greenhouse gas, to the atmosphere from deposits in the earth. However, it is very likely that the pace of methane emissions will increase.
Of course, further research is needed to improve our understanding of the potential for abrupt changes in climate. For example, the report’s scientists found that such processes as interaction of warm ocean waters with the periphery of ice sheets and ice shelves have a greater impact than previously known on the destabilization of ice sheets that might accelerate sea-level rise.
A Summary Brochure on Abrupt Climate Change is available.