Armand Thibault looked out over the Pacific's rumbling winter waves from his balcony in Neskowin, Ore. "The predicted high tide today is a 10.1 [feet]," he relayed via YouTube on Friday, January 29. "I'm very glad we don't have a storm surge behind this one. Tomorrow is supposed to be a 10.2, so it should be interesting." [More]

Armand Thibault looked out over the Pacific's rumbling winter waves from his balcony in Neskowin, Ore. "The predicted high tide today is a 10.1 [feet]," he relayed via YouTube on Friday, January 29. "I'm very glad we don't have a storm surge behind this one. Tomorrow is supposed to be a 10.2, so it should be interesting." [More]

The village of Brep in Pakistan doesn't exist in the same place anymore. That's because a torrential flood forced the community to move after a lake formed by glacial meltwater burst its bounds and leveled the town.  

Glacial lake outbursts have become a yearly occurrence across the high mountain region stretching from Afghanistan to Bhutan sometimes called the Roof of the World. 

Every second, a vast quantity of cold, dense seawater equal to six times the combined flow of every land river on Earth streams over an ocean-floor ridge that stretches between Greenland and Scotland. This deep southbound current, flowing from the Norwegian, Iceland and Greenland seas into the North Atlantic, is the lower limb of the Gulf Stream and its northerly extension, a great conveyor belt of ocean heat and salt that transports warm tropical water north from the equator. Most climate change models predict global warming will slow these flows, in part by altering a key component of the Atlantic's circulation, called deep-water formation. If that happens, northern Europe will cool--or warm less severely--as the rest of the globe swelters. [More]