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Sounds like we're talking about a feedback loop here, where a warming planet leads to a planet that warms even more quickly. SHAPIRO: Just - you're describing the disappearance of sea ice leading oceans to retain more heat. And we see those influences, for example, with some extreme marine trash events in the Bering Strait of Alaska and also differences in the marine soundscape and what animals that live in the ocean are hearing and how they can communicate with each other. And as we're losing sea ice in the Arctic, that's also opening up opportunities for additional shipping and industry. And those warm ocean temperatures can linger into fall and winter, causing disruptions for future sea ice.īut also, we see animals behaving differently in different seasons, difficulties with food access. But if we remove that sea ice, we uncover a very dark ocean surface, and that's good at absorbing heat. And that's what's helping to reflect the additional energy back to space and reduce melt.
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MOON: If we look at the planet from space, we can imagine looking down on sea ice, and it's very bright. So what happens when there is less of that sea ice in the Arctic? To start with, sea ice reflects sunlight.
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SHAPIRO: A melting Arctic leads to a series of dominoes falling, so let's talk about some of the different knock-on effects. And as a result, we're seeing rapid and really dramatic changes. The Arctic is actually warming faster than most of the globe. MOON: Unfortunately, that's another good indicator of patterns that we're seeing across the Arctic. SHAPIRO: What does that record high in Siberia tell you? Climate scientist Twila Moon is one of the report's authors, and she joins us now. This comes on the same day the National Oceanic and Atmospheric Administration released its annual Arctic Report Card. Today, the U.N.'s World Meteorological Organization officially verified that a town in Siberia called Verkhoyansk hit 100 degrees Fahrenheit last year. In the Arctic, it was literally unheard of until now.
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