Posts Tagged ‘antarctica’

Episode 16 – Antarctica: Unprecedented Western Ice Melt and CO2-Saturated Southern Ocean

Play

Episode 16 - Antarctica: Unprecedented Western Ice Melt and CO2-Saturated Southern OceanA sobering satellite study shows it was warm enough for a week or two in January 2005 for Western Antarctica ice to melt over an area as big as California. Such a huge ice melt in western Antarctica is unprecedented and could mean that global warming is even getting to the thick ice of the South Pole.

Until now, the very cold Antarctic Southern Ocean absorbed into its waters 15% of the worldwide carbon dioxide “sinking” into the Earth’s seas. U.K. scientists have discovered the Southern Ocean is saturated with CO2 absorbed from the atmosphere. That data implies many other regions of the Earth’s oceans must also be saturated with CO2. Does that mean that even more CO2 is getting into the greenhouse gas “blanket” that is warming up our planet?

episode 16

 

Episode 6 – New U.N. Global Climate Change Report: Earth Could Warm Up 3.2 to 11.52 Degrees Fahrenheit by 2100

Play

Episode 6 - New U.N. Global Climate Change Report: Earth Could Warm Up 3.2 to 11.52 Degrees Fahrenheit by 2100The United Nation’s Intergovernmental Panel On Climate Change, known as the IPCC, has been working on another report since its last one in 2001. This is supposed to be a consensus of scientists and computer labs around the world about where global climate change is headed. This report says it is “very likely” that increasing carbon dioxide is caused by human activity.

How high will sea levels rise? For reasons that are not clear, the rapidly increasing ice melts of Antarctica and Greenland were left out of the initial draft of the IPCC’s 2007 report – allegedly because computer models don’t have current data to accurately access the impact. So, the report might project only a 5 to 23-inch rise in sea level. But one prominent glaciologist thinks the worst case for sea level rise could be five times higher than the IPCC’s estimate.