Monday, September 01, 2014
Warmists invent magic ice
It melts and gets thicker at the same time, apparently. There are lots of findings that antarctic ice is increasing -- e.g. here -- but the galoots below say it has been increasingly melting
Sea levels around Antarctica have been rising a third faster than the global average, a clear sign of high meltwater runoff from the continent's icesheet, scientists said on Sunday.
Satellite data from 1992 to 2011 found the sea surface around Antarctica's coast rose by around eight centimetres (3.2 inches) in total compared to a rise of six cm for the average of the world's oceans, they said.
The local increase is accompanied by a fall in salinity at the sea surface, as detected by research ships.
These dramatic changes can only be explained by an influx of freshwater from melting ice, warned the study. "Freshwater is less dense than salt water, and so in regions where an excess of freshwater has accumulated, we expect a localised rise in sea level," said Craig Rye from Britain's National Oceanography Centre, who led the probe.
The estimate of ice loss and the precise source of it are hard to pin down, though. According to the team's computer model, around 350 billion tonnes a year of freshwater influx, plus or minus 100 billion tonnes, would explain the rise.
This estimate puts together freshwater from the ground-based icesheet and also from the thinning of ice shelves -- floating ice that is attached to the coast and created by glaciers disgorging from the icesheet.
Most of the meltwater is being discharged around the Antarctic peninsula -- the giant finger of land that juts towards South America -- and in the Amundsen Sea.
"Accelerating discharge from the Antarctic icesheet has had a pronounced and widespread impact on the adjacent subpolar seas over the past two decades," said the study.
The stability of the Antarctic ice sheet is one of the big factors in the global warming equation. The biggest single source of freshwater in the world, it would drown many coastal cities if a large part of it were to melt.
Getting an accurate fix on this risk, though, is bedevilled by unknowns, partly because the icesheet is also gaining mass in some places through greater snowfall.
Posted by John J. Ray (M.A.; Ph.D.).