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从DCENT数据集中,自1850年以来地球表面温度的动态一致集合
Duo Chan1, Geoffrey Gebbie2, Peter Huybers3
1School of Ocean and Earth Science, University of Southampton, Southampton, UK. Duo.Chan@soton.ac.uk.
Scientific data
|August 30, 2024
概括
本研究介绍了动态一致的温度集 (DCENT),这是一个用于历史气候研究的新数据集. DCENT为1850-1900年提供了一个较冷的基线,表明历史变暖比以前估计的要大.
科学领域:
- 气候科学 气候科学
- 地球系统科学 地球系统科学
- 古气候学 古气候学
背景情况:
- 准确的历史地表温度记录对于气候研究和政策至关重要.
- 现有的仪器温度估计显示在全球和区域范围内存在不一致.
- 解决这些不一致性对于可靠的气候变化评估至关重要.
研究的目的:
- 开发一个新的,动态一致的历史表面温度异常组合.
- 提高全球和区域温度重建的准确性和一致性.
- 为评估历史气候变暖提供更强大的基线.
主要方法:
- 开发了动态一致的温度ENsemble (DCENT),一个200个成员,5°×5°分辨率的数据集从1850年.
- 在陆地表面空气温度数据中采用了优化的双向均质化算法.
- 利用基于物理学的相互比较方法进行海面温度偏差调整.
- 整合了一种合的能量平衡模型,用于统一大陆和海洋记录.
主要成果:
- DCENT提供了与1982-2014年气候学相对的每月表面温度异常.
- 整体利用最新的数据同质化和偏差调整技术.
- 一个关键的发现是,与现有估计相比,1850-1900年的基线较冷.
结论:
- DCENT数据集提供了更一致,更准确的历史地表温度重建.
- 较冷的基线意味着历史变暖的幅度更大.
- 这种改进的数据集将加强气候研究,并为政策制定提供信息.
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