Across the Arctic, winter can seal entire lakes beneath thick ice and snow. From above, everything appears silent and motionless.
But beneath some of those frozen surfaces, bubbles continue rising from the mud. They contain methane created as microorganisms consume organic material released from thawing permafrost.
In this episode of Beyond the Frozen Horizon, we descend beneath a thermokarst lake to discover how frozen ground collapses into water, how carbon stored for thousands of years can become active again, and why an Arctic lake can continue breathing long after winter appears to have shut it down.