TAG | Sea to rise nearly 1 meter by 2100 |
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| by Stan Beer | |
| Friday, 02 February 2007 | |
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The team found that carbon dioxide concentration followed the modelled scenarios almost exactly, that global-mean surface temperatures were in the upper part of the range projected by the IPCC, and that observed sea level has been rising faster than the models had projected and closely followed the IPCC Third Assessment Report upper limit of an 88cm rise between 1990 and 2100. Sea levels have risen largely due to warming of the ocean and the consequent thermal expansion and melting of non-polar glaciers and ice caps and the ice sheets of Antarctica and Greenland, according to the report. The climate system, and in particular sea level, may be responding more quickly to rising carbon emissions than climate scientists have estimated with climate models. The team of climate scientists has cautioned against suggestions that the Intergovernmental Panel on Climate Change (IPCC) has previously overestimated the rate of climate change. The scientists noted that because the review period (1990-2006) was short, it would be premature to conclude that sea levels will continue to increase at the same rate in the future. However, they also said their findings show that previous projections have not exaggerated the rate of change but may in some respects have underestimated it. Measurements of carbon dioxide through facilities such as the Australian Bureau of Meteorology's Cape Grim observatory in Tasmania support the paper's conclusions. The global average temperature estimates are collated separately by NASA's Goddard Institute for Space Studies in the USA and the Hadley Centre and Climatic Research Unit in the UK. The sea level observations come from both coastal and island tide gauges and data provided by satellites. One of the authors of the review, Dr John Church of the Antarctic Climate & Ecosystems CRC and CSIRO, noted that any (or all) of the modelled contributions could be underestimated but that there is most uncertainty about the contribution made by ice-sheet melts. "Models of the potential contribution of the Greenland and Antarctic ice sheets need to be improved to include the potential of a relatively dynamic response," Dr Church said. This work is a component of the Wealth from Oceans Flagship, an initiative of CSIRO to more broadly understand the impact of marine climate change. Lead author of the review was Dr Stefan Ramstorf, of the Potsdam Institute for Climate Impact Research, Potsdam, Germany; with contributing authors: Dr Anny Cazenave, Toulouse France; Dr John Church, Antarctic Climate and Ecosystem CRC and CSIRO; Dr James Hansen at NASA Goddard Institute for Space Studies, USA; Drs Ralph E. Keeling and Richard C.J. Somerville, Scripps Institution of Oceanography, UCSD, USA; and, Dr David E. Parker, Hadley Centre, Met Office, UK.{moscomment}
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