I’ve been digging a little deeper into the report released at last week’s meeting of the American Geophysical Union. The report, commissioned by the U.S. Climate Change Science Program, warns that the United States could suffer the effects of abrupt climate changes within decades - much sooner than previously thought.
Abrupt Climate Change: Final Report, Synthesis and Assessment Product 3.4 recognizes that four types of abrupt change in the geologic record are so rapid and large in their impact that, if they were to recur, they would pose clear risks to society in terms of our ability to adapt:
- Rapid change in glaciers, ice sheets, and hence sea level.
- Widespread and sustained changes to the hydrologic cycle, including drought and flooding.
- Abrupt change in the Atlantic Meridional Overturning Circulation (AMOC), a critical component of global climate, characterized by the northward flow of warm, salty water in the upper layers of the Atlantic Ocean.
- Rapid release to the atmosphere of methane, a powerful greenhouse gas, trapped in permafrost and in ocean sediments.
The report reaches the following conclusions about the potential for abrupt climate changes from global warming during this century:
- The southwestern United States may be beginning an abrupt period of increased drought, as subtropical drying will likely intensify and persist in the future due to greenhouse warming. This drying is predicted to move northward into the southwestern United States.
- It is very likely that the northward flow of warm water in the upper layers of the Atlantic Ocean will decrease by approximately 25–30 percent. While a collapse of the AMOC is unlikely, the possibility of collapse cannot be entirely excluded.
- An abrupt change in sea level is possible, but predictions are highly uncertain due to shortcomings in existing climate models. Inclusion of ice-sheet and glacier processes into future modeling experiments will likely lead to sea-level rise projections for the end of the 21st century that substantially exceed those presented in the Intergovernmental Panel on Climate Change fourth assessment report.
- it is very likely that climate change will accelerate the pace of methane emissions from both hydrate sources and wetlands. A catastrophic release of methane to the atmosphere in the next century appears very unlikely in the near term (1-100 years). However, changes in climate, including warmer temperatures and more precipitation in some regions, will likely increase the chronic emissions of methane from both melting hydrates and natural wetlands over the next century. The magnitude of this effect cannot be predicted with great accuracy yet, but is likely to be equivalent to the current magnitude of many anthropogenic methane sources, which have already more than doubled the levels of methane in the atmosphere since the start of the Industrial Revolution.
The chapter on methane presents puzzles that are new to me. Its conclusion that a catastrophic methane release triggering a rapid global warming event is unlikely - at least not in the next 100 years - is only mildly comforting.
Methane (CH4) is the second most important greenhouse gas that humans directly influence, carbon dioxide (CO2) being first. Atmospheric CH4 has a lifetime of ~9 years (±10%). In other words, at steady state, each year one ninth of the total amount of methane in the atmosphere is removed by oxidation, and replaced by emissions to the atmosphere. Methane oxidation products stratospheric water (H2O) vapor, tropospheric ozone (O3), and CO2 contribute indirectly to methane’s radiative forcing. Over a 100-year time horizon, the direct and indirect effects on RF of emission of 1 kilogram (kg) CH4 are 25 times greater than for emission of 1 kg CO2. While concentrations of methane in the atmosphere are much lower than carbon dioxide (700 ppb & 487 ppm, respectively), its potency as a greenhouse gas means its radiative impact is almost 1/3 (.289) that of CO2.
The authors note that current methane levels ~1775 ppb - are “anomalous” (i.e., extremely high by historical levels and more than 2 1/2 times the ~700 ppb at the start of the Industrial Revolution). But since 1999, the global atmospheric CH4 abundance has been nearly stable; globally averaged CH4 in 1999 was only 3 ppb less than the 2006 global average of 1775 ppb. The authors concede the exact causes of the plateau in methane levels “remain unknown, making predictions of future methane levels difficult.”
The authors concede that very little is know about the location, extent, or vulnerability of both terrestrial and marine methane hydrate deposits - current estimates may be low by a factor of 10. They caution that the level of concern about catastrophic release of methane to the atmosphere is directly linked to the size of these reservoirs. The authors dryly note that past abrupt changes “provide further motivation for considering the potential for future abrupt changes in methane.”
The report doesn’t find “catastrophic methane releases” in either the models or Earth’s history, but notes the uncertainty:
[M]odeling and detailed studies of ice core methane so far do not support catastrophic methane releases to the atmosphere in the last 650,000 years or in the near future. A very large release of methane may have occurred at the Paleocene-Eocene boundary (about 55 million years ago), but other explanations for the evidence have been offered.
The authors see the PETM as significant to the present day because it is an analog to the potential fossil fuel carbon release if we burn all the coal reserves. The ~5,000 GtC released by burning coal would increase global average temperatures by about 5°C (assuming the IPCC’s estimates of climate sensitivity are correct). Atmospheric CO2 was probably at least 560 ppm at the initiation of the PETM event.
The authors note the 5°C global temperature increase of the PETM event cannot be explained by the ~2,000 GtC increase in atmospheric carbon based on paleoclimate records. One possible explanation is that IPCC estimates for the climate sensitivity are too low by a factor of 2 or more - but a decreased climate sensitivity would be expected for the ice-free world that existed at the time of the PETM event, compared to the ice-age climate of today with its ice albedo feedback.
A brochure summarizing the report - Abrupt Climate Change: Summary and Findings - is also available, and a press release is available here