Discussion Overview
The discussion revolves around the availability and reliability of simulation codes for modeling Earth's historical temperature records over the past 2000 years. Participants explore the complexities of climate modeling, the factors influencing temperature, and the challenges of verifying simulation accuracy.
Discussion Character
- Exploratory
- Technical explanation
- Debate/contested
Main Points Raised
- Some participants inquire about publicly available simulation codes that can model Earth's temperature history with a yearly resolution.
- One participant mentions the Keeling curve as a potential source of historical temperature data, suggesting it has been calculated backward from its inception in 1958.
- There is a discussion about the difficulty of verifying the accuracy of climate models and the trustworthiness of "what if" scenarios generated by simulations.
- Some participants argue that climate models require significant computing power and involve numerous assumptions, making it challenging to achieve certainty in predictions.
- Concerns are raised about the potential collapse of major ocean currents, such as the Gulf Stream, and the implications this could have on climate data reliability.
- Participants note that while many models point in the same direction, none have been calculated in a browser environment, raising questions about their accessibility and usability.
- There is a suggestion to look at the financial data from reinsurance companies as a potentially reliable indicator of climate trends, despite the reluctance to engage with political aspects of climate change.
Areas of Agreement / Disagreement
Participants express a range of views on the reliability and accessibility of climate simulation models, with no consensus reached on the best approach or the validity of various models discussed.
Contextual Notes
Participants highlight the limitations of current models, including the need for extensive computing resources and the challenges of incorporating numerous feedback loops and chaotic elements in climate systems.