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Thank you, Dr. Lee, for that excellent presentation on your new hypothesis regarding climate feedback loops. It's certainly a thought-provoking perspective.

You're welcome, Professor Chen. I appreciate the opportunity to share our preliminary findings.

I do have a question, or rather, a point of clarification regarding the weighting you applied to the oceanic carbon sink in your model. While I understand the rationale, it seems to perhaps overemphasize its long-term stability.

Could you elaborate on your concerns, Professor? We based that weighting on recent paleoclimate data, suggesting a more consistent uptake capacity than previously thought.

Certainly. My main reservation stems from the potential for ocean acidification to compromise that very stability in warmer oceans. While paleoclimate data is invaluable, it doesn't fully account for the rapid rate of current CO2 absorption. Wouldn't a more dynamic or even decreasing weighting be a more prudent approach to reflect this potential vulnerability?

That's a very valid point, Professor. We did consider the acidification factor, but perhaps we were too optimistic in assuming the resilience of the buffering capacity. Your insight certainly highlights a potential area for refinement in our future modeling efforts.