在古世后期-古世早期的干燥水气候中,世界温室气温
Victor A Piedrahita1,2,3,4, Andrew P Roberts4, Eelco J Rohling5,6
1Key Laboratory of Deep Petroleum Intelligent Exploration and Development, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China.
Nature communications
|August 15, 2024
概括
极端的全球变暖导致了亚热带地区的显著干旱在晚期古世 - 早期欧世 (LPEE) 期间. 这些与碳循环变化相关的干旱条件持续了数千年,为当前的气候变化提供了洞察力.
科学领域:
- 古气候学 古气候学
- 气候科学 气候科学
- 地球系统科学 地球系统科学
背景情况:
- 对于亚热带地区来说,了解极端变暖事件期间的水气候变化对于亚热带地区至关重要.
- 晚期古世 - 早期古世 (LPEE) 为研究过去的大规模碳循环扰乱及其气候影响提供了有价值的模拟物.
研究的目的:
- 在LPEE期间重建西底斯的原地中海区域的水气候条件.
- 调查碳循环扰乱对水气候变化和干旱的影响.
主要方法:
- 使用地质代理的古气候重建 (在摘要中未指明的细节).
- 分析长期和短暂的碳循环变化及其与水气候数据的相关性.
主要成果:
- 在LPEE期间,碳循环扰动控制了轨道强迫的水气候变化.
- 长期的碳变化导致降水逐渐减少,而短暂的干扰导致了快速变暖和极端干旱.
- 大型变暖事件后的水气候恢复大约需要24-27 kyr.
结论:
- 大规模的碳循环扰乱对LPEE水气候产生了重大影响,导致了干旱.
- 这些发现表明,人为变暖可能导致长期干旱,并造成长期后果.
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