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The general circulation model (GCM), a method for modeling climate change, is predicated on the idea that, in contrast to weather, climate is a boundary value problem making it unpredictable over short timescales, averaging over a large enough sample size causes the weather to converge towards the climate of the model. The climate, also known as control runs, is the state at which specified atmospheric shapes and boundary conditions cause model outputs to converge.

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The Climate Linear and Non-linear Regime

  • 章节

  • 发表日期：

    2025年

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  • Georgy Golitsyn,
  • Costas Varotsos

摘要

The general circulation model (GCM), a method for modeling climate change, is predicated on the idea that, in contrast to weather, climate is a boundary value problem making it unpredictable over short timescales, averaging over a large enough sample size causes the weather to converge towards the climate of the model. The climate, also known as control runs, is the state at which specified atmospheric shapes and boundary conditions cause model outputs to converge.