
The Big Chill
Interactive Video
•
Science, Geography, Biology, Physics
•
6th - 12th Grade
•
Hard
Wayground Content
FREE Resource
The video discusses how some regions may warm while others cool due to the Great Ocean Conveyor Belt, a network of ocean currents that distribute heat globally. It explains how salty water sinks in the Arctic, creating a current that travels to the equator and rises as it warms. Freshwater from melting glaciers can disrupt this system, potentially leading to a shutdown with severe climate consequences. The video highlights the possibility of this occurring within the next century, affecting global weather patterns and causing droughts or severe winters in different regions.
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OPEN ENDED QUESTION
3 mins • 1 pt
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