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By Jeremy Deaton

You might know the feeling—after months of encouraging news from your bathroom scale, you discover the device is broken. The outlook on your weight-loss goal is worse than you realized.

Scientists just went through something similar, except instead of a scale, it was a system of satellites, and instead of your winter weight, it was the Greenland ice sheet.

Zachariae Isbrae, in northeast Greenland.Anders A Bjork/The Ohio State University

Researchers have been tracking Greenland's ice sheet melt by measuring the shrinking mass of the island via satellite. It now seems there was an error in measurement. A new study published in the journal Science Advances finds the ice is melting 7 percent faster than previously thought.

Scientists use satellites to map Earth's gravity field, gathering information about the distribution of mass around the globe. Earth doesn't exert gravity equally in all directions. Where there is more mass, satellites detect a stronger gravitational pull.

Using satellite data, scientists can measure various geophysical phenomena, including the melt of the Greenland ice sheet. As ice dissolves, the island loses mass and exerts a weaker gravitational pull—at least that's the idea.

An artist's rendering of NASA's Gravity Recovery and Climate Experiment satellites measuring Earth's gravity field.NASA/JPL-Caltech

In practice, it's a little more complicated. Satellites can only detect a change in mass. They can't determine how much of that mass is ice, how much is land and how much is mantle ebbing and flowing beneath the Earths' crust.

"[The system] cannot tell the difference between ice mass and rock mass," said study co-author Michael Bevis, professor of Earth sciences at Ohio State. "So, inferring the ice mass change from the total mass change requires a model of all the mass flows within the Earth."

Here's where this gets interesting.

A cross-section of Earth. The Earth's crust rests on a thick layer of mantle. Below that lies the Earth's solid core.NASA/JPL, Université Paris Diderot and the Institut de Physique du Globe de Paris

Tectonic plates are always moving. The plate under North America—including Greenland—has been traveling northwest for millions of years. Around 40 million years ago, Greenland slid over an extra hot column of partially molten rock. This hot spot softened up the crust below the island's east coast. (The hot spot now rests beneath Iceland, where it is driving all manner of volcanic activity—warming hot springs and fueling the country's geothermal power plants.)

The softening of Earth's crust beneath Greenland had consequences during the last ice age, when Greenland's ice sheet was significantly thicker. The weight of all that ice caused the island to sink into the supple crust below. When the ice age passed and the ice began to melt, the island rebounded. Mantle flowed in beneath Greenland, causing the land to rise again. It's still rising today.

You can imagine how this would interfere with satellite readings. The loss of ice is weakening Greenland's gravitational pull. At the same time, the accumulation of mantle is strengthening its gravitational pull.

One of dozens of GPS units researchers used to measure the rise of land.Dana J. Caccamise II/The Ohio State University

Scientists previously accounted for the flow of mantle, but they underestimated its effect. The study's authors used GPS technology to measure the rise of land at various points along Greenland's east coast. They discovered that mantle is gathering beneath Greenland more quickly than they had realized.

What this means is that scientists have been underestimating ice loss by 20 billion metric tons per year. More of the melting is occurring along Greenland's east coast than previously thought.

Water overflow from a lake formed from melted ice carved this 60-foot canyon into the Greenland ice sheet.Ian Joughin, University of Washington

"By refining the spatial pattern of mass loss in the world's second largest—and most unstable—ice sheet, and learning how that pattern has evolved, we are steadily increasing our understanding of ice-loss processes, which will lead to better-informed projections of sea-level rise," said Bevis.

The study has implications for Antarctica—the 800-pound gorilla of global sea-level rise. Scientist will need to deploy more GPS measurement stations at Earth's southern pole to accurately measure the flow of mantle beneath the continent and get a better reading of Antarctic ice melt.

Better data will allow scientists to predict future sea-level rise more accurately. That could prove crucial for coastal cities preparing for the impacts of climate change.

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When we read about algae blooms, they are often associated with a lake or the ocean, not glaciers. A team of scientists, though, are looking at just that: how algae blooms affect glacier melt.

The Black and Bloom project aims to understand how dark particles and microorganisms living in the melt water on the surface of Greenland's ice sheet are amplifying its melt. These dark spots lower the albedo of the ice sheet and absorb more sun rays than pure ice does. With increased heat comes increased melt; with more melt comes more microorganisms, which then start the circle all over again.

"We want to get a handle on just how much of the darkness is due to microbes and how much to other physical factors," Martyn Tranter, a biogeochemist at the University of Bristol and the project's principal investigator, told Scientific American.

The team of scientists will spend the next six weeks observing the ice sheet. There will be several other expeditions over the next four years to measure and manipulate the ice surface, according to the project's website. Using the data collected during their expeditions, scientists will be able to predict how the ice sheet will change in the future with on-going climate change.

Tranter said the work could also influence water supply predictions in areas such as the Himalayas where algae bloom-infected glaciers are common, Scientific American reported.

Ice melt in Greenland—which is losing an estimated 287 billion tons of ice every year—has already broken records this year, beginning almost two months early. The Danish Meteorological Institute reported 12 percent of the ice sheet was melting as of April 11. Greenland's melt season typically runs from June to September.

Early melting doesn't come as a surprise with the National Aeronautics and Space Administration (NASA) reporting May's average temperatures were 0.93 C above the 1951-1980 average for the month and June was the warmest on record since 1895 in the U.S., with a monthly average temperature of 71.8 F in Lower 48 states, 3.3 F above normal.

The Black and Bloom project will tweet about its progress on Twitter.

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