Iceland review - 2015, Page 32

Iceland review - 2015, Page 32
30 ICELAND REVIEW Volcanologist Haraldur Sigurðsson was off by five days when pre- dicting the end of the eruption in Holuhraun. Starting on August 31, it lasted almost six months, or 181 days, concluding on February 27. Using a simple mathemat- ical formula with the help of his grand- son, Gabríel Sölvi Wendels, an engineering student at Reykjavík University, Haraldur calculated in October that, judging by the decreasing subsidence of the Bárðarbunga caldera—the volcano which lies under Vatnajökull fed the eruption north of the glacier by an underground channel—and hence reduced pressure of magma, the eruption would end on March 4. SCIENTIFIC BREAKTHROUGH “It’s the first time in history that the end of a volcanic eruption has been predicted,” Haraldur maintains. “There are three steps to a scientific theory. First, data is collect- ed, in this case about the subsidence of the Bárðarbunga caldera. Next, a theory or model based on the data is made—which isn’t necessarily correct and must be tested. Finally, a forecast is made and if it proves correct it supports the theory on which further forecasts can be based.” Geophysicist Freysteinn Sigmundsson agrees. “It tells us that the system is … basi- cally rather simple and the question is now what will happen with the magma cham- ber below Bárðarbunga in the future,” he told national broadcaster RÚV. Freysteinn reasons that Haraldur’s theory can be used to evaluate further developments in the volcano. “In 1978, my colleague Steve Sparks and I put forth a theory about lateral magma flow in volcanoes like Bárðarbunga, Askja, Grímsvötn and Krafla, but we didn’t have the opportunity to test it,” Haraldur says of the origins of his theory. “When the magma intrusion began in Bárðarbunga on August 16, with magma reaching the surface on August 29, there was a question whether the theory could be put to the test,” Haraldur explains. “We had data about the subsidence and it followed a certain process with unbelievable accuracy. It wasn’t linear but a curve, which with time became flatter. And so a formula could be made: once the curve would become horizontal, the erup- tion would stop, as the curve indicates the outflow of magma. “Gabríel Sölvi calculated when the curve would become horizontal and came up with the first week of March. And we stood by it. The curve proved remarkably even, there were almost no daily fluctuations, it was almost perfect,” Haraldur excites. “It was simple in this case because the magma chamber is probably very large so that outside disturbances have no effect on the model. It can no doubt be used on other eruptions in the future.” However, the significance of Haraldur’s prediction is dis- puted. “Some scientists claim it was mere coincidence,” he says. WAYS OF A VOLCANO The eruption in Holuhraun was preceded by a series of earthquakes which began in Bárðarbunga on August 16. “We had observed increased activity since May and we had been in contact with the Department of Civil Protection. Then, on August 16 an immensely powerful earthquake series suddenly began and it immediately became clear that this was a case of magma on the move,” says Kristín As the eruption in Holuhraun has come to an end, scientists evaluate its effect and discuss what Bárðarbunga volcano may be up to next. BY EYGLÓ SVALA ARNARSDÓTTIR. PHOTOS BY PÁLL STEFÁNSSON. FIRE OUT
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