Methane emergency in the Arctic? August 20, 2013 12:32 AM | 7 Comments Thanks to Bob Baker for this. It really isn’t that hard to know what is true and what isn’t. From kindergarten to junior high to high school to college to graduate school, I cannot recall a lot of confusion or controversy. Within the education departments across the planet a fact is a fact. Two plus two is four. E=Mc2. Redding is really hot in the summer. It is only when politicians and media companies and Anthony Watts get involved that the science becomes distorted and confused. When money and power need the truth to be something it isn’t. And people are easy to fool. If their television tells them, they believe. And yet trustworthy sources exist. Like Skeptical Science, where “there is an ongoing effort to combat disinformation from those who maintain that climate change is a non-issue or non-reality.” And where sometimes, they must call out those who “overhype the impacts of climate change beyond the realm of plausibility. Some of this is well-intentioned but misguided. For those who advocate climate literacy or for scientists who engage with the public, it is necessary to call out this stuff in the same manner as one would call out a scientist who doesn’t think that the modern CO2 rise is due to human activities.” While I was in Colorado in June at AGU’s Communicating Climate Science Conference, I asked a question of one of the presenters who was an expert on the Arctic who worked with the National Snow & Ice Data Center. I asked about the Arctic Methane Emergency Group (AMEG) and whether current science had evidence that there is indeed an emergency in the Arctic and whether the global climate is at risk of an imminent release of a massive methane burst. The scientist was perplexed — she had never heard of AMEG — and seemed quite certain, that at least in the short run, we were not in danger of a methane catastrophe. Now I was confused until I spoke directly with another scientist with whom I was quite familiar and deeply trusted. And he stated with adamant certainty that AMEG could not be trusted with any of their doomsday scenarios. He said he had repeatedly confronted their bad math and science and appealed to AMEG directly to no avail. They ignored him and refused to correct their flawed calculations. According to Skeptical Science, “Many overblown scenarios or catastrophes seem to involve methane in the Arctic in some way. There are even groups out there declaring a planet-wide emergency because of catastrophic, runaway feedbacks, involving the interplay between high latitude methane sources and sea ice. “In this article, I will argue that there is no compelling evidence for any looming methane spike. Other scientists have spoken out against this scenario as well, and I will encompass some of their arguments into this piece. In summary, the reason a huge feedback is unlikely is because of the long timescale required for global warming to reach some of the largest methane hydrate reservoirs (defined later), and because no evidence exists for such an extreme methane concentration sensitivity to climate in the past record. Permafrost feedbacks are of concern, but there is no basis for assuming a dramatic ‘tipping point’ in the atmospheric methane concentration.” Read the whole article if you are interested. But here is the conclusion: “The observed methane venting from the East Siberian shelf sea-floor to the atmosphere is probably not a new component of the Arctic methane budget. Furthermore, warming of the Arctic waters and sea ice decline will likely impact subsea permafrost on longer timescales, rather than the short term. “Methane feedbacks in the Arctic are going to be important for future climate change, just like the direct emissions from humans. This includes substantial regions of shallow permafrost in the Arctic, which is already going appreciable change. Much larger changes involving hydrate may be important longer-term. “Nonetheless, these feedbacks need to be kept in context and should be thought of as one of the many other carbon cycle feedbacks, and dynamic responses, that supplement the increasing anthropogenic CO2 burden to the atmosphere. There is no evidence that methane will run out of control and initiate any sudden, catastrophic effects. There’s certainly no runaway greenhouse. Instead, chronic methane releases will supplement the primary role of CO2. Eventually some of this methane oxidizes into CO2, so if the injection is large enough, it can add extra CO2 forcing onto the very long term evolution of global climate, over hundreds to thousands of years.” And if you want to wade more deeply into the weeds on this issue, here is Joe Romm’s take from last year. – See more at: http://blogs.redding.com/dcraig/archives/2013/08/methane-emergen.html#sthash.U179SPt8.dpuf
Aug. 19, 2013 — Reservoirs of silica-rich magma — the kind that causes the most explosive volcanic eruptions — can persist in Earth’s upper crust for hundreds of thousands of years without triggering an eruption, according to new University of Washington modeling research.
That means an area known to have experienced a massive volcanic eruption in the past, such as Yellowstone National Park, could have a large pool of magma festering beneath it and still not be close to going off as it did 600,000 years ago.
“You might expect to see a stewing magma chamber for a long period of time and it doesn’t necessarily mean an eruption is imminent,” said Sarah Gelman, a UW doctoral student in Earth and space sciences.
Recent research models have suggested that reservoirs of silica-rich magma, or molten rock, form on and survive for geologically short time scales — in the tens of thousands of years — in the Earth’s cold upper crust before they solidify. They also suggested that the magma had to be injected into the Earth’s crust at a high rate to reach a large enough volume and pressure to cause an eruption.
But Gelman and her collaborators took the models further, incorporating changes in the crystallization behavior of silica-rich magma in the upper crust and temperature-dependent heat conductivity. They found that the magma could accumulate more slowly and remain molten for a much longer period than the models previously suggested.
Gelman is the lead author of a paper explaining the research published in the July edition of Geology. Co-authors are Francisco Gutiérrez, a former UW doctoral student now with Universidad de Chile in Santiago, and Olivier Bachmann, a former UW faculty member now with the Swiss Federal Institute of Technology in Zurich.
There are two different kinds of magma and their relationship to one another is unclear. Plutonic magma freezes in the Earth’s crust and never erupts, but rather becomes a craggy granite formation like those commonly seen in Yosemite National Park. Volcanic magma is associated with eruptions, whether continuous “oozing” types of eruption such as Hawaii’s Kilauea Volcano or more explosive eruptions such as Mount Pinatubo in the Philippines or Mount St. Helens in Washington state.
Some scientists have suggested that plutonic formations are what remain in the crust after major eruptions eject volcanic material. Gelman believes it is possible that magma chambers in the Earth’s crust could consist of a core of partially molten material feeding volcanoes surrounded by more crystalline regions that ultimately turn into plutonic rock. It is also possible the two rock types develop independently, but those questions remain to be answered, she said.
The new work suggests that molten magma reservoirs in the crust can persist for far longer than some scientists believe. Silica content is a way of judging how the magma has been affected by being in the crust, Gelman said. As the magma is forced up a column from lower in the Earth to the crust, it begins to crystallize. Crystals start to drop out as the magma moves higher, leaving the remaining molten rock with higher silica content.
“These time scales are in the hundreds of thousands, even up to a million, years and these chambers can sit there for that long,” she said.
Even if the molten magma begins to solidify before it erupts, that is a long process, she added. As the magma cools, more crystals form giving the rock a kind of mushy consistency. It is still molten and capable of erupting, but it will behave differently than magma that is much hotter and has fewer crystals.
The implications are significant for volcanic “arcs,” found near subduction zones where one of Earth’s tectonic plates is diving beneath another. Arcs are found in various parts of the world, including the Andes Mountains of South America and the Cascades Range of the Pacific Northwest.
Scientists have developed techniques to detect magma pools beneath these arcs, but they cannot determine how long the reservoirs have been there. Because volcanic magma becomes more silica-rich with time, its explosive potential increases.
“If you see melt in an area, it’s important to know how long that melt has been around to determine whether there is eruptive potential or not,” Gelman said. “If you image it today, does that mean it could not have been there 300,000 years ago? Previous models have said it couldn’t have been. Our model says it could. That doesn’t mean it was there, but it could have been there.”
The work was funded by the National Science Foundation and the National Scientific and Technological Research Commission of Chile.
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(AP Photo/Fosphotos, Elina Liberta) Weather woes: A flash of lighting is seen in Piraeus, near Athens during a rainstorm in February. Hours of heavy rainfall in Athens caused extensive flooding. Across Europe severe weather and flooding have caused economic losses estimated at more than $22 billion so far this year.
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