for 
- example - cascading tipping points via AMOC
example - cascading tipping points via AMOC
- As Arctic system melts faster, it releases more freshwater into the North Atlantic
- This is happening on the southern tip of Greenland, for example and the lower density of water slows down the AMOC current
- Warm saline water flows from the Southern Ocean up into the North Atlantic
- When it reaches the southern tip of Greenland,  the heat is radiated into the atmosphere and heats up Europe
- When the freshwater meltwater from Greenland mixes with this AMOC current, the AMOC water is less heavy and sinks slower
- This pushes monsoons further south, which can explain why there are more droughts and fires in the Amazon rainforest
- The slowdown of the AMOC leaves more saline water stuck in Antarctica, potentially contributing to the faster melting of Antarctica glaciers