CHILE – In less than 24 hours Lake Cachet II in Chile’s southern Patagonia vanished, leaving behind just some large puddles and chunks of ice in the vast lake bed. The lake’s water comes from ice melting from the Colonia Glacier, located in the Northern Patagonian ice field, some 2,000 kilometers (1,250 miles) south of the capital, Santiago. The glacier normally acts as a dam containing the water, but rising temperatures have weakened its wall. Twice this year, on January 27 and March 31, water from the lake bore a tunnel between the rocks and the glacier wall. The result: Lake Cachet II’s 200 million cubic liters of water gushed out into the Baker river, tripling its volume in a matter of hours, and emptying the five square kilometer (two square miles) lake bed. Cachet II has drained 11 times since 2008 — and with global temperatures climbing, experts believe this will increase in frequency. “Climate models predict that as temperatures rise, this phenomenon, known as GLOFs (Glacial Lake Outburst Floods), will become more frequent,” said glaciologist Gino Casassa from the Center for Scientific Studies (CES). Casassa, a member of the 2007 Nobel Peace Prize-winning Intergovernmental Panel on Climate Change, told AFP there have been 53 similar cases of lakes draining in Chile between 1896 and January 2010, with increased frequency in the later years. CES research assistant Daniela Carrion was camped out with a small research team taking measurements of the Colonia Glacier when the lake drained in March. “When we woke up, we saw a change in the valley,” Carrion told AFP. “The paths that we walked on had flooded, and the whole area was filled with large chunks of ice.” The lake dropped 31 meters (90 feet) when the water drained out, according to a report from the General Water Directorate, which monitors lake levels in Chile using satellite data. When the lake starts draining an alarm system is triggered, giving residents in the sparsely-populated area up to eight hours to move animals and flee to higher ground.