Geological analysis suggest the current-day continents we know and love will drift together, forming a new supercontinent like ones that existed many millions of years ago. What’s not certain is where that supercontinent will be. The authors of a new Nature study suggest that the next supercontinent, dubbed Amasia, will join together up in the Arctic. Antarctica, though, would stay by its lonesome in the south.

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Joshua trees in the Mojave Desert

Solar energy has been enjoying its day in the sun with massive federal subsidies, but the energy taken from sunlight also has a dark side. Building these plants in the American West destroys large swathes of the desert ecosystem. Cacti must be mowed down and local wildlife displaced to make room for the giant mirrors that will essentially carpet the desert. The LA Times has a great feature on the Ivanpah project in the Mojave that began construction in October 2010.

Far from an empty stretch of sand, the Mojave supports diverse wildlife. No one knows exactly how the new solar power plant will affect the tortoises, eagles, and Joshua trees that currently inhabit the area. Is it okay to sacrifice the desert in the fight against larger climate change? The situation has put environmental groups in a bind, as Times reporter Julie Cart explains:

The national office of the Sierra Club has had to quash local chapters’ opposition to some solar projects, sending out a 42-page directive making it clear that the club’s national policy goals superseded the objections of a local group. Animosity bubbled over after a local Southern California chapter was told to refrain from opposing solar projects.

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The outline of Lake Vostok beneath the ice, as seen from space.

Last week, as Russian scientists neared the end of two decades of drilling to reach Lake Vostok, an ancient Antarctic lake buried beneath miles of ice that hasn’t seen light in 20 million years, people around the world waited with bated breath for news. Yesterday the Russian state-run news agency announced that on Sunday, the drill had reached water, apparently the lake surface. Today, the project leader clarified that they need to verify that the water the drill struck was actually Lake Vostok. New Scientist has a tidy explanation of why it’s not necessarily obvious if you’ve hit a massive underground lake:

[Hitting water] suggests the lake has been breached, but the team are now checking the level of water in the borehole and readings from pressure sensors to confirm that the water did come from the lake and not a pocket of water in the ice above the lake. Ice temperatures rise as you go deeper into the ice sheet, and approach melting point just above the lake, so the fact that the team hit liquid water doesn’t necessarily mean they’ve reached the lake.

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For years, solar energy researchers have tried to imitate the success of photosynthesis by building devices like an artificial leaf and a solar cell that hijacks chemistry of photosynthetic bacteria. Now researchers at MIT have come up with an innovative technique that also happens to be very cheap: all you need is some “stabilizing powder” and plant waste. Mowed your lawn lately?

The stabilizing powder is a mix of safe, easily attainable chemicals that preserves photosystem I, a protein complex that captures light energy in plant cells. (In contrast, the newest photovoltaic cells in solar panels require metals that are rare or toxic.) The powder is mixed with plant matter such as grass clippings and crushed, and the resulting green goo is spread onto glass or metal substrate. Hook up wires to capture the electric current and that’s your solar panel.

The efficiency of these solar panels is only 0.1%, compared to the 15 to 18% efficiency of solar panels out in the market right now. Lead researcher Andrew Mershin says the technology still needs to improve 10-fold to become practical. After all, being able to power only one lightbulb with a whole house covered in solar panels isn’t much help. But the great advantage of all this is that it’s easy and dirt grass cheap. Because the barrier to entry is so low, anyone would be able to order a bag of chemicals and make their own solar panel. Mershin hopes home tinkerers experiment with the cells and find new ways to make improvements.

Correction, February 6: We eliminated a reference to mulch in the headline: mulch is low in chlorophyll, so it wouldn’t actually work for these plant-powered solar cells.

The outline of Lake Vostok beneath the ice, as seen from space.

After two decades of drilling through miles of Antarctic ice, Russian scientists are about to breach an underground lake that has not been exposed to the surface in more than 20 million years. Lake Vostok, as the body of water is called, is part of a chain of more than 200 lakes hidden beneath the ice, some of which were formed when Australia and Antarctica were still connected. Vostok will be the first one of all to be opened when the drill hits water next week.

Scientists believe that there may be life in the lake, as ice removed from the Vostok borehole has been found to contain bacteria. And since the subterranean lakes, kept liquid by heat from the Earth’s core, are similar to those found on moons Enceladus and Europa, scientists are excited to see what such inhabitants might be like. But the Russian team’s somewhat sloppy drilling methods have got a number of people worried about preserving the pristine lake from contamination, as Marc Kaufman reports in a great feature for the Washington Post.

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In this graphic from the restoration authority, the land that will
be lost to erosion if the plan isn’t undertaken is shown in red.

Six years after Hurricane Katrina devastated New Orleans and the Louisiana coast, the state’s Coastal Protection and Restoration Authority has finally released a draft of a plan to try to keep it from happening again. How? By restoring the wetlands along the Mississippi River Delta, which we have more or less systematically destroyed but used to act as buffers between storm surge waves and inland cities.

Previous plans had relied on mainly on building levees and seawalls, so it’s striking that this plan, which would unroll over the course of 50 years at a cost of $50 billion, focuses on wetland restoration, writes Mark Fischetti, who has been covering this issue for Scientific American for years. Here’s how it would work:

Along the outer edge of the torn-up coast, furthest from New Orleans, former barrier islands that have been worn to thin wisps of land would be broadened with sandy sediment, mostly dredged from the ocean bottom and conveyed through pipelines. Natural ridges of land along the coast would be strengthened in similar fashion. Together, the islands and ridges would form a dotted line around southeastern Louisiana that can cut down storm surges. They would not all connect, so wind-driven water could still find its way through, but the many segments would break up the incoming wavefront into chaotic eddies flowing in conflicting directions that would at least partially cancel out one another.

The plan is already drawing ire from fishermen, who say that current restoration projects haven’t had much effect, and that all this shuttling of sand and water will interfere with their livelihoods.

Read more at Scientific American.

Images courtesy of the Coastal Protection and Restoration Authority

With their majestic peaks, imposing canyons, and lofty designation, America’s national parks seem inviolate, places of natural grandeur far from the vagaries of money or politics. But over the years, 26 sites have lost their national park status. In a slideshow at National Geographic, Brian Handwerk explores why.

A few parks were less-than-ideal candidates to begin with (the National Park Service running the Kennedy Center? huh?). But more often than not, the decision to jettison a park from the list came down to economics: Several parks, like Montana’s Lewis and Clark Caverns, above, were too remote to attract enough visitors; the caverns are now part of the state’s park system. Other ex-parks, however, are no longer open to the public: a Palm Beach retreat that proved too expensive for the government to maintain was bought by Donald Trump—and made into a swanky, exclusive club.

Read the rest at National Geographic.

Image courtesy of Montana State Parks

Spring! Not.

Across the US, this winter has been unusually balmy, with precious little snow, or even rain, and with trees taking the warmth as a cue to send out new leaves in January. Temperature data support those impressions: in the first week of the year, temperatures were 40 degrees F higher than average in some parts of the Midwest, Discovery News reports, and snow cover is at 19 percent across the country, compared to an average of 50 percent at this time of year. In notoriously chilly Fargo, North Dakota, the January 4 high temperature of 55 broke the record for the warmest January day on record, and the country has seen close to no rain or snow in this first week of 2012, writes Wunderground meteorologist Jeff Masters. “It has been remarkable to look at the radar display day after day and see virtually no echoes,” he writes, referring to the radar echoes reflected back by storms. “It is very likely that this has been the driest first week of January in U.S. recorded history.”

Why this freaky weather? The answer is, basically, an extremely unusual jet stream over the last few months, Masters explains. The jet stream that defines weather in North America is controlled by the North Atlantic Oscillation and the Arctic Oscillation, climate patterns that reflect differences in sea-level pressure across certain stretches of the globe. And the pressure differences this year have been tremendous—for the North Atlantic Oscillation (NAO), this year saw the most extreme difference ever recorded in December, and the second most extreme for the Arctic Oscillation (AO).

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If you could watch a movie of the planet over the last several million years, you’d see the ice caps advance and retreat: The planet’s climate moves in cycles, with ice ages and interglacial periods alternating. But looking at previous interglacials similar to our own, geophysicists now think that the current mostly ice-less period may be longer than it would have been had a certain species not invented the combustion engine. Specifically, it looks like with amount of greenhouse gases we’ve already spewed into the atmosphere, the next ice age will be delayed. And before you decide that’s a good thing, at the rate we’re currently going, we’re not just pushing off the glaciers for a few geologically insignificant years: the team says that the atmospheric concentration of CO2 would to be at most 240 parts per million (ppm) before glaciation would kick in. Right now, it’s 390 ppm, with no signs of dropping and many signs of continuing to rise. When (and how) the planet’s self-regulation system will kick in isn’t clear, but the long, increasingly hot trip probably isn’t going to be pretty.

Read more at the BBC.

Image courtesy of NASA / Wikipedia

A tower for removing gas at the Marcellus Shale Formation in Pennsylvania.

When it was revealed in November that several small earthquakes in northwestern England had been caused by fracking, the controversial process of extracting shale gas from bedrock by cracking the rock with pressurized water, the gas company responsible stated that it was an extremely unlikely occurrence. True as that may be, residents of Youngstown, Ohio, can now testify that something similar has happened again. This time, it wasn’t the removal of shale gas that triggered the earthquakes, but apparently the subsequent cracking of sandstone in order to store the wastewater produced by fracking.

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Flooding in Piazza San Marco, Venice

Venice is sinking, and the nearby Adriatic sea—like the global sea level—is rising. The city could, some estimates suggest, be underwater by the end of the century. Much of the trouble is due to Venice’s precarious, low-lying position in the middle of a lagoon, but human activity in the area has played a role in the city’s subsidence, as well. As Scott K. Johnson explains at Ars Technica:

The pumping of shallow groundwater in the mid-1900s also contributed to the problem. Water in the pores between grains of sediment provides pressure that bears some of the load. When pore pressure decreases, or water is removed completely, grains can be packed together more tightly by collapsing the pore spaces. As sediment is compacted, the land surface drops. While the effect was small (less than 15cm), Venice doesn’t have much wiggle room.

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The peripatetic magnetic south pole.

A hundred years after Robert Scott‘s disastrous mission to the South Pole, a pair of Kiwi scientists are traveling to his observation hut today to continue the work he began there: tracking the Earth’s magnetic field. Since 1957, New Zealand has measured the field at Scott’s base every five years, accruing data that, along with measurements from other, more comfortable sites around the world, helps maintain the model used by NATO and nations’ defense departments for navigation.

The planet’s magnetic field needs tracking because it is shifting: the magnetic south pole has been traveling northwestward at a rate of 6 to 9 miles a year for the past century. (The geographic South Pole is somewhere altogether different.) This shift occurs because the mass of molten metal that makes up the Earth’s outer core is in a constant state of turmoil, and the  the poles could veer off in another direction at any time. Intriguing, the magnetic field has also been getting weaker since the 1800s. But whether that means the poles will flip at some point in the future—it’s happened before!—or whether it will start getting stronger again very soon is a mystery.

[via Nature News]

Image courtesy of NOAA

The holidays are hard on Christmas lights. Exposed to the vagaries of small nephews and exuberant pets, most strings will experience a few casualties, and while a missing bulb no longer means the entire set stops working, Americans still throw out millions of pounds of lights a year. Adam Minter, who’s writing a book on the globalization of recycling, describes exactly what happens to your old lights when they’re shipped over to a concern in China, which, ironically, makes better use of minced-up lights than any US company could.

Workers untangle the lights and toss them into small shredders, where they are chopped into millimeter-sized fragments and mixed with water into a sticky mud-like substance. Next, they’re shoveled onto a large, downward-angled, vibrating table, covered in a thin sheen of flowing water.

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If you live in the Northeast, chances are you’ve had a disappointingly balmy December so far (the snow seems to have taken a wrong turn somewhere and wound up over Texas instead). But when the air gets that snap and you  reach for the wool socks, Emily Eggleston at Scientific American has a few factoids that promise to fascinate. Here’s why wool keeps you warm:

Wool keeps out the cold because it is an excellent insulator. Crimped and crisscrossed woolen fibers create tons of little air pockets. The tiny air masses within my socks have difficulty moving in and out of the fabric. Without convective heat transfer and contact with air of other temperatures, the spaces between wool fibers maintains a steady temperature.

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In the form of brood parasites, the bird world has enough irresponsible moms to start a reality TV show: cowbirds, for instance, lay their eggs in other species’ nests, stab most of the hosts’ eggs to death, and then leave their offspring to be raised by the host parents. The standing explanation for this involves most host birds being not that sharp on the uptake (watch a tiny warbler fussing over a cuckoo chick ten times its size (above) and you’d think that too). But maybe, a new study suggests, it’s sometimes to the host’s benefit to let imposter eggs stay in their nests.

The researchers chose mockingbirds as their hosts and cowbirds as their parasites, because mockingbirds usually fight like crazy to keep cowbirds of their nests but get strangely quiescent once the invaders have laid their eggs, a behavior that piqued the researchers’ interest. Once all the birds in the sample population had laid, the researchers went around adding and removing eggs from nests to see whether having a certain number of cowbird eggs affected mockingbird survival. They found that mockingbird eggs that shared their digs with cowbird eggs and suffered repeated cowbird invasions were more likely to survive, apparently because when each cowbird arrived, it would stab a certain proportion of the eggs in the nest regardless of whether they were host eggs or the eggs of the previous cowbird. Letting the parasite’s eggs stay, then, means that more of the host eggs avoid getting stabbed. The researchers conclude that when there are a lot of cowbirds around and hence a high probability of multiple nest hijackings, it makes sense for mockingbird parents not to shove out the invaders’ eggs.

Nice. And with all this dubious parenting and wanton violence, it’s straight from an episode of Teen Mom meets Cops, no?