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Phoenix666 writes:

It's big. It's cold. And it's melting into the world's oceans.

It's Zachariae Isstrom, the latest in a string of Greenland glaciers to undergo rapid change in our warming world. A new NASA-funded study published today in the journal Science finds that Zachariae Isstrom broke loose from a glaciologically stable position in 2012 and entered a phase of accelerated retreat. The consequences will be felt for decades to come.

The reason? Zachariae Isstrom is big. It drains ice from an area of 35,440 square miles (91,780 square kilometers). That's about 5 percent of the Greenland Ice Sheet. All by itself, it holds enough water to raise global sea level by more than 18 inches (46 centimeters) if it were to melt completely. And now it's on a crash diet, losing 5 billion tons of mass every year. All that ice is crumbling into the North Atlantic Ocean.

"North Greenland glaciers are changing rapidly," said lead author Jeremie Mouginot, an assistant researcher in the Department of Earth System Science at the University of California, Irvine. "The shape and dynamics of Zachariae Isstrom have changed dramatically over the last few years. The glacier is now breaking up and calving high volumes of icebergs into the ocean, which will result in rising sea levels for decades to come."

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Phoenix666 writes:

Using data from a 3053-meter-long core of ice and bedrock collected from the center of the island in 1993, Schaefer's team has found valuable clues to what the period held. In particular, the 1.55 meters of bedrock at the core's base revealed much about the island's history of glaciation, Schaefer says, in atoms that chronicle exposure to the elements. Earth's surface is constantly bombarded by cosmic rays, high energy particles streaming into Earth from space. They collide with atoms in Earth's atmosphere as well as in the uppermost centimeters of its rocks, producing new particles. Some of those particles have a particularly useful set of properties: They don't naturally occur in the rocks, and they are radioactive. Thus, they can act as a sort of clock, marking time since the rocks were last ice free and exposed to the atmosphere.

Schaefer and his colleagues measured the abundance of two cosmogenic isotopes, aluminum-26 and beryllium-10, in grains of the mineral quartz that they found within the bedrock. Each isotope is produced at a different rate by cosmic rays and has a different half-life. Once the rocks are no longer exposed to the atmosphere—for example, buried by ice—the ratio of 26Al to 10Be in the rocks changes because of their differing half-lives. Schaefer and his team found that the ratio in the bedrock was simply too low for the site to have remained buried continuously over the last 1.25 million years—suggesting that it had been exposed and ice free at least once during that time.

Schaefer says he is certain the findings show that Greenland was ice free at one point

Original Submission

Phoenix666 writes:

A genetic variation has evolved in populations that have eaten a plant-based diet over hundreds of generations, such as in India, Africa, and parts of East Asia.

A different version of the allele adapted to a marine diet was discovered among the Inuit people in Greenland, who mainly consume seafood.

The adaptation allows these people to efficiently process omega-3 and omega-6 fatty acids and convert them into compounds essential for early brain development and controlling inflammation.

In Inuit populations of Greenland, a previously identified adaptation is opposite to the one found in the long-standing vegetarian populations: While the vegetarian allele has an insertion of 22 bases (a base is a building block of DNA) within the gene, this insertion was found to be deleted in the seafood allele.
[Paleo diet works if you have Inuit genes]

"The opposite allele is likely driving adaptation in Inuit," says Kaixiong Ye, a postdoctoral researcher working in the lab of Alon Keinan, associate professor of biological statistics and computational biology at Cornell University.

Original Submission

"exec" writes:

Unusually Early Greenland Melt:

Based on observation-initialized weather model runs by DMI, almost 12% of the Greenland ice sheet had more than 1mm of melt on Monday 11th April, following an early start to melting the previous day. Scientists at DMI were at first incredulous due to the early date. "We had to check that our models were still working properly" said Peter Langen, a climate scientist at DMI. "Fortunately we could see from the PROMICE.dk stations on the ice sheet that it had been well above melting, even above 10 °C. This helped to explain the results". The former top 3 earliest dates for a melt area larger than 10% were previously all in May (5th May 2010, 8th May 1990, 8th May 2006).

Even weather stations quite high up on the ice sheet observed very high temperatures on Monday", said Robert Fausto, a scientist at GEUS who maintains PROMICE.dk melt data. "At KAN_U for example, a site at 1840 m above sea level, we observed a maximum temperature of 3.1°C. This would be a warm day in July, never mind April". Other PROMICE stations in the network at lower levels had daily average temperatures between 5 and 10 °C.

Also at phys.org.

-- submitted from IRC

Original Submission