相关实验视频
Updated: Mar 28, 2026

Using Generative Art to Convey Past and Future Climate Transitions
Published on: March 31, 2023
对"大西洋和太平洋多十年振荡和北半球温度"的评论的回应
B A Steinman1, L M Frankcombe2, M E Mann3
1Large Lakes Observatory and Department of Earth and Environmental Sciences, University of Minnesota Duluth, Duluth, MN, USA. bsteinma@d.umn.edu.
克拉夫托夫和其他人 通过使用不充分的气候模型和低估不确定性,错误地评估了内部气候变化. 他们的分析是有缺陷的,因为模型组合有限,强制信号的表现不足.
科学领域:
- 气候科学
- 大气科学
- 地球系统科学
背景情况:
- 准确评估内部气候变化对于了解气候变化至关重要.
- 之前的研究依赖于模型模拟来估计内部变异性.
- 对于稳定的气候预测,量化观察到的内部变异性的不确定性至关重要.
研究的目的:
- 批判性地评估Kravtsov等人使用的方法. 在评估模拟内部气候变化的统计独立性时.
- 解决在观察到的内部变化计算中低估不确定性的说法.
- 在Kravtsov等人提出的分析中发现根本的缺陷.
主要方法:
- 对气候模型组合的分析,重点是实现的数量.
- 评估单一气候模型代表强制气候信号的能力.
- 模拟内部气候变化的统计评估.
主要成果:
- 克拉夫索夫等人进行的分析. 根本上是有缺陷的
- 他们的方法是使用模型组合, 实现太少.
- 没有一个单一的气候模型能够充分反映强制性的气候信号,
结论:
- 克拉夫索夫等人提出的要求. 关于统计独立性评估和内部气候变化的不确定性是没有根据的.
- 这项研究强调了对更大,更多样化的气候模型集团的迫切需要.
- 需要改进的方法来准确地表示气候模拟中的强制信号.
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