Photograph by Paul Nicklen, National Geographic
Published March 29, 2013
It's a global warming paradox.
As air and sea temperatures rise, Arctic sea ice is rapidly and uniformly dwindling. In 2012, Arctic sea ice declined so much that the loss "utterly" obliterated the previous record, set in 2007, according to the U.S. National Snow and Ice Data Center.
As of 2012, the area of Arctic sea ice around the North Pole had shrunk to 1.58 million square miles (4.1 million square kilometers)—the smallest measurement since 1979, when satellite observations began.
But in Antarctica, where sea ice is more scattered and driven by wind and waves, there's another story—ice is increasing in places.
In September of last year, satellite data indicated that Antarctica was surrounded by the greatest area of sea ice ever recorded in the region: 7.51 million square miles (19.44 million square kilometers), according to the center. (Related: "Antarctic Sea Ice Hits Record ... High?")
Previous studies pointed to snow: Global warming has warmed Antarctic air, and warmer air holds more moisture, which in turn creates more precipitation. That means more snow is falling on Antarctica, and more of the white stuff makes the top layers of the ocean less salty and thus less dense. These layers became more stable, preventing warm currents in the deep ocean from rising and melting sea ice.
Now, a new study has pinpointed another culprit: melting ice shelves. As ice shelves that ring the southernmost continent disintegrate in warming temperatures, the fresh water that flows from them accumulates in a cool
and fresh surface layer on top of the ocean. This cool layer then shields the surface ocean from the warmer, deeper waters that are melting the ice shelves.
The study "shows that global warming can cause regional cooling, and that's quite counterintuitive," said study leader Richard Bintanja, of the Royal Netherlands Meteorological Institute. (See a map of the impact of global warming worldwide.)
"Most people think if you warm the whole system, it will warm everywhere," he said.
Also counterintuitively, a colder Antarctica may contribute to a rise in sea levels. Colder temperatures mean less snow on the ice sheets, which makes more water stay in the ocean, he pointed out.
Overall, loss of polar ice has contributed about 11.1 millimeters (0.03 feet) to global sea levels since 1992, research shows. Sea levels are rising at a rate of 3.2 millimeters a year. (See pictures of sea level rise.)
Ice Shelves to Blame?
In researching the Antarctic conundrum, Bintanja and colleagues noted routine observations showing that the deepest parts of the ocean off Antarctica are warming.
The team also found research showing that some ice shelves in Antarctica extend up to 0.62 mile (one kilometer) deep into the ocean. The deep warm water can easily come into contact with a shelf and melt it from below.
These observations led the scientists to suggest that the resulting meltwater rises to the surface-fresh water is lighter than saltwater-and forms a cold shallow layer that prevents the warm water from below to mix upward, thus cooling the surface layer and allowing more sea ice to form. (Test your ocean IQ.)
A climate model behaved in the same way, reinforcing the theory, said Bintanja, whose study appears March 31 in the journal Nature Geoscience.
What's more, the team said their new theory can account for most of the sea ice expansion. For instance, a statistical model suggested that other factors, such as precipitation and winds, are responsible for only about 25 percent of sea ice growth.
"A Complicated Place"
Walt Meier, of the U.S. National Snow and Ice Data Center in Boulder, Colorado, said the new study is "pretty interesting—it's something that I haven't seen before."
But he's more cautious about the study's claim that melting ice shelves account for the overall trend, he said. (Read "The Big Thaw" in National Geographic magazine.)
Sea ice can be found far from the edges of the continent, especially in winter when the ice is at its maximum cover, he noted.
"When ice is way far from the coast, the shelf water seems unlikely to have a major effect" on making more sea ice, he said—rather, melting ice shelves may give sea ice formation "a head start."
Noted study leader Bintanja: "We tested this with our climate model, and the effect of meltwater does extend all the way to the sea ice front."
Overall, Meier said, all of the dynamics in Antarctica—from wind to temperature to weather—makes it difficult to ferret out the facts.
"It's a complicated place."
Perhaps we are postponing the ice age that the elitists predicted back in the 70s. An ice age would be much more devastating than global warming.
hmmm. . . .By this logic, Antarctica would have no ice
during glacial periods (Ice ages) due to the lack of moisture in the cold air.
I had a great history prof who stated well this situation: "When you put your ear to the ground and hear the beating of hooves, think horses, not zebras.”
Stay calm and worry not of CO2.
Changes in oceanic pH over the last 25 million years :http://metaworks.pangaea.de/download.php?fileid=252
..::"Ocean Acidification is now irreversible... at least on timescales of at least... TENS of THOUSANDS of years...
Even with stabilisation of atmospheric CO2 at 450 ppm, Ocean Acidification will have profound impacts (death and extinction) on many marine systems.
LARGE and rapid reductions of global CO2 emissions are needed globally by at LEAST 50% by 2050.
Analysis of past events in Earth's geologic history suggests that chemical recovery (normal pH for LIFE in the Ocean) will take TENS of THOUSANDS of years - while the recovery of ecosystem function and biological diversity (LIFE AS WE KNOW IT) can take much longer. (MILLIONS OF YEARS)
..:: "Every day, 70 MILLION TONS of CO2 are released into Earth's atmosphere. ( remaining in the atmosphere for thousands of years )
..:: "Every day, 20 MILLION TONS of that CO2 are absorbed into the OCEANS, thereby increasing the overall ACIDITY of the OCEANS.
By 2100, Ocean acidity will increase another 150 to 200 hundred percent.
This is a dramatic change in the acidity of the oceans. And it has a serious impact on our ocean ecosystems; in particular, it has an impact on any species of calcifying organism that produces a calcium carbonate SHELL.
..:: "These are changes that are occurring far too fast for the oceans to correct naturally, said Dr Richard Feely with the US National Oceanic and Atmospheric Administration (NOAA)
..:: "Fifty-five million years ago when we had an event like this (and that took over 10,000 years to occur), it took the oceans over 125,000 years to recover, just to get the chemistry back to normal," he told BBC News.
..:: "It took two to 10 million years for the organisms to re-evolve, to get back into a normal situation.
..:: "So what we do over the next 100 years will have implications for ocean ecosystems from tens of thousands to millions of years. That's the implication of what we're doing to the oceans right now."
@Larry Lawhorn The CO2 emissions are not as bad as you may think. also, the ocean accounts for the majority of CO2 in our atmosphere. The real culprits are gases like methane. those attribute more to our "greenhouse gases" than CO2. Plus with the warming of the sun, our CO2 emissions are going to go up just as they have been since before the industrial revolution.
@Larry Lawhorn Thanks Larry .. and thanks for the links you shared with us
Methane is a
trace compound (1.8 PPM) and "lives" for only about 10 years in the
atmosphere before it oxidizes.
Even at 25X warming capabilities it would act like 45 PPM CO2 or about 12% of the total CO2 absorption capabilities.
Stay calm and worry not of CH4.
The Yellowstone River's oil spill was the first in U.S. frozen water in two-plus decades.
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