Web Date: February 1, 2006
The risks of global disasters because of climate change may be much greater than previously believed, says a report issued by the U.K. Meteorological Office. It expresses concern that the world may be nearing temperature-change thresholds that could trigger irreversible effects. The study summarizes government-sponsored research presented at a conference last February.
The document, "Avoiding Dangerous Climate Change," presents evidence that the Greenland ice cap may already be melting and that a local increase of 2.7 °C over today's average temperature in Greenland "may be a threshold that triggers" irreversible melting of the ice cap. If the ice cap melts completely, sea level would rise 7 meters, inundating most of the world's coastal cities. Such a temperature increase is well within the range of climate-change projections for the century. According to the "Third Assessment Report" of the UN Intergovernmental Panel on Climate Change, the average global temperature is expected to rise between 1.4 and 5.8 °C by 2100.
A global increase of 1 °C is likely to lead to extensive coral bleaching, vastly disrupting marine ecosystems, the report says. It noted recent studies showing that the ocean is already more acidic because of its absorption of excess carbon dioxide from the atmosphere. "This is likely to reduce the ocean's capacity to absorb carbon dioxide from the atmosphere and affect the entire marine food chain," the study says.
The document notes that an increase of 3 °C could reverse the land carbon sink—that is, release carbon from forests and permafrost—and destabilize the Antarctic ice sheets.
The study reports that technological options—such as energy efficiency, nuclear energy, and renewable transport fuels—for making large reductions in emissions over the long term already exist. “There are no magic bullets,” the report says, noting that excluding any option will increase costs of cutting emissions.
The report can be found at www.metoffice.gov.uk
- Chemical & Engineering News
- ISSN 0009-2347
- Copyright © American Chemical Society