Primate wrote:Climate always changes, and dramatic climatic fluctuations have occurred in shorter time spans than those occurring at the present time. Specialized agragrian societies depend on relatively constant climate conditions, which is what most people experience during a lifetime. But it is not the reality.
Primate wrote:...agricultural societies are less adaptable to climate fluctuations.
Ayame wrote:Might be better for hunting and gathering?
Zardoz wrote:Primate wrote:Like many have said, it's as if Peak Oil and Global Warming are in a race to determine which one will get us first.
EnergyUnlimited wrote:You are overreacting guys.
It is good, that this ice is melting.
Once the process is complete, we will move all those starving Africans to Greenland.
They will get new land for free...we will teach them some farming...
We will develope Inuit + African multicultural society...we will get more wealthy consumers to support our expanding economy...
We will also get more water to our oceans... and more water equals more fish...
A favorite mantra of the deniers is that Greenland is actually gaining ice because it's supposedly gaining so much around its center. Not so:
NASA: Greenland ice loss far greater than gain
Like I've been saying, we don't need to argue with them. Reality will do our debating for us.
rockdoc123 wrote:A favorite mantra of the deniers is that Greenland is actually gaining ice because it's supposedly gaining so much around its center. Not so:
NASA: Greenland ice loss far greater than gain
Like I've been saying, we don't need to argue with them. Reality will do our debating for us.
well actually one of the main predictions of all of the GCMs if memory serves me correctly is that the interior of the Antarctic ice mass would increase due to heavier snowfalls while the margins would decrease due to slightly warmer ocean temperatures. Up until the 90s this was happening. The new NASA measurements you mention here sort of throws a monkey wrench in the model predictions as snowfall recently has not increased.
Recent observations of the WAIS, a marine ice sheet with a base below sea level, show that vast quantities of ice are melting at a faster rate than previously recorded. Many observers consider this and an increase in calving icebergs along the Antarctic's margins to be evidence of global warming. The team's findings also counter climate-change skeptics who consider a thickening of Antarctica's enormous ice sheets has stemmed the gradual rise in global sea levels.
Satellite radar altimetry measurements indicate that the East Antarctic ice-sheet interior north of 81.6°S increased in mass by 45 ± 7 billion metric tons per year from 1992 to 2003. Comparisons with contemporaneous meteorological model snowfall estimates suggest that the gain in mass was associated with increased precipitation. A gain of this magnitude is enough to slow sea-level rise by 0.12 ± 0.02 millimeters per year
Although the ice mass loss observed in the new study is less than half of what other recent research has reported, the results show that Greenland is now losing 20% more mass than it receives from new snowfall each year. "This is a very large change in a very short time," said Zwally. "In the 1990's, the ice sheet was growing inland and shrinking significantly at the edges, which is what climate models predicted as a result of global warming. Now the processes of mass loss are clearly beginning to dominate the inland growth, and we are only in the early stages of the climate warming predicted for this century."
Alfred Tennyson wrote:We are not now that strength which in old days
Moved earth and heaven, that which we are, we are;
One equal temper of heroic hearts,
Made weak by time and fate, but strong in will
To strive, to seek, to find, and not to yield.
Kangerdlugssuaq Glacier on the east coast of Greenland has been clocked using GPS equipment and satellites to be flowing at a rate of 14km per year. It is also losing mass extremely fast, with its front end retreating 5km back up its fjord this year alone. The glacier "drains" about 4% of the ice sheet, dumping tens of cubic km of fresh water in the North Atlantic.
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