脱冰永久土解的异步性受千年级气候变化控制
Xinwei Yan1,2, Xu Zhang3,4, Bo Liu5
1College of Urban and Environmental Sciences, Peking University, Beijing, 100871, China.
Nature communications
|January 2, 2025
概括
西藏高原永久土的融化,与北极地区不同,通常在脱冰期间开始. 千年级的大西洋南部翻转循环 (AMOC) 的变化影响永久土的碳释放和降冰的二氧化碳增加.
科学领域:
- 古气候学 古气候学
- 永久土科学 永久土科学
- 地质化学 地质化学
背景情况:
- 永久土的融化是脱冰过程中全球碳循环的一个重要因素.
- 了解环北极和低度永久土的动态对于气候建模至关重要.
- 西藏高原 (TP) 永久土地区的脱冰历史在很大程度上仍未被探索.
研究的目的:
- 重建西藏高原永久土在过去50万年的解历史.
- 调查北半球永久土解模式及其与气候强迫的关系.
- 了解大西洋南部翻转循环 (AMOC) 对永久土动态的影响.
主要方法:
- 洞穴的生长阶段分析以确定TP永久土解时间表.
- 时间标准化用于与北半球永久土记录进行比较.
- 气候建模以阐明驱动TP变暖和永久土融化的反机制.
主要成果:
- TP永久土的解通常在脱冰开始时开始,这与薄弱的季风间隔和缓慢的AMOC有关.
- 亚洲季风的减弱会通过局部反机制导致异常的TP变暖.
- 观察到TP和北极永久土之间的异步解,受高度降温的影响.
- 由于异常的AMOC变异性,最近的脱冰显示TP解延迟和近北极解进展.
结论:
- TP永久土解模式与北极周边地区有很大差异.
- 千年规模的AMOC变化在调节永久土碳释放方面发挥着关键作用.
- 永久土释放的碳是一个潜在的重要因素,但往往被忽视,有助于降冰CO2增加.
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