通过植被气候反来调和东亚的全新世纪中期温度差异
Jie Chen1, Qiong Zhang2, Zhengyao Lu3
1Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China.
Science bulletin
|May 1, 2024
概括
调查了Holocene温度难题,气候模型和代理数据之间的不匹配. 发现植被气候反导致东亚地区的变暖,改善了模型数据的一致性.
科学领域:
- 古气候学 古气候学
- 地球系统科学 地球系统科学
- 气候建模气候模型
背景情况:
- 全新纪温度难题凸显了代理气候重建和模型模拟之间的差异.
- 重建表明冷却后的Holocene热最大值,而模型显示由于冰盖的退缩和温室气体的变暖.
研究的目的:
- 为了研究植被气候反对东亚中 Holocene 温度异常的影响.
- 用地球系统模型将植被变化对区域温度模式的影响隔离出来.
主要方法:
- 使用完全合的地球系统模型EC-Earth.
- 进行了模拟,并没有结合的动态植被,用于Holocene中期 (∼6 ka).
主要成果:
- 植被气候反导致东亚大部分地区的变暖.
- 观察到空间上多样化的温度变化,显著改善了模型数据的一致性.
结论:
- 植被气候反在解决全新世纪温度难题方面发挥着至关重要的作用.
- 准确模拟气候场景需要包括植被气候反.
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