A brand new paper released in Nature suggests that the polar ice sheets are more vulnerable to global warming than previously feared. 2 degrees Celsius of global warming could commit us to 6-9 meters (20-30 feet) of long-term sea level rise. The study is based an extensive database of geological indicators for the last interglacial period, roughly 125,000 years ago, when polar temperatures were about 3-5 degrees Celsius warmer than today, as is expected if global warming hits 2-3 degrees Celsius above pre-industrial levels. The findings reinforce that the developed world needs to be prepared to fund significant adaptation support, particularly for low-lying countries such as Bangladesh.
Friday, September 16, 2011
The Energy Collective | NATURE: Sea level rise may exceed worst expectations
A brand new paper released in Nature suggests that the polar ice sheets are more vulnerable to global warming than previously feared. 2 degrees Celsius of global warming could commit us to 6-9 meters (20-30 feet) of long-term sea level rise. The study is based an extensive database of geological indicators for the last interglacial period, roughly 125,000 years ago, when polar temperatures were about 3-5 degrees Celsius warmer than today, as is expected if global warming hits 2-3 degrees Celsius above pre-industrial levels. The findings reinforce that the developed world needs to be prepared to fund significant adaptation support, particularly for low-lying countries such as Bangladesh.
Sunday, April 8, 2007
Acidic oceans
The acidity of the ocean has increased by 30% since pre-industrial times and is predicted to double by 2100 because of increased uptake of CO2 according to expatriate Australian Australia’s leading oceanographer, Dr Tony Haymet, former Chief of Marine and Atmospheric Science at CSIRO, now director of the prestigious Scripps Institution of Oceanography and Vice Chancellor of Marine Sciences at the University of California.
Increasing the amount of CO2 in the oceans causes an increase in hydrogen carbonate ions, HCO3-, but a decrease in carbonate CO22- which organisms need to make calcium carbonate shells and other structures.
The predicted acidity increase will have unknown consequences for marine life and ecosystems such as coral reefs, tiny marine organisms called pteropods, and fish larvae to name but three.