Multiple Choice

Two planetary climate models, System A and System B, both currently exhibit a stable, high-ice equilibrium. When subjected to an identical, temporary warming event:

  • System A experiences a minor loss of ice and returns to its original state within a few cycles.
  • System B experiences a more significant loss of ice and takes much longer to return to its original state.

What does this comparison suggest about the feedback mechanisms governing these two systems?

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Updated 2025-08-10

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