在温暖的气候下,气候变化的加速
Licheng Guo1, Shangfa Xiong1,2, Benjamin J W Mills3
1Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China.
Science advances
|July 10, 2024
概括
全球变暖加速了土壤中 (P) 的释放,这是一个关键的营养素. 这一发现影响了对地球气候调节和气候变化下的生态系统的理解.
科学领域:
- 地质化学 地质化学
- 生物地质化学生物地质化学
- 气候科学 气候科学
背景情况:
- (P) 气候变化是全球元素循环和生物圈大小的关键.
- 全球气候对P气候变化的影响在理论上是显著的,但缺乏经验性的全球数据.
- 了解P释放机制对于预测生态系统对气候变化的反应至关重要.
研究的目的:
- 实证地研究全球表面温度与释放率之间的关系.
- 评估全球变暖引起的营养供应在地球气候调节中的作用.
- 评估加速的P损失对生态系统和海洋环境的影响.
主要方法:
- 全球表面土壤温度数据的汇编 (0-30厘米深度).
- 全球表面土壤中含量的分析.
- 温度和P释放指标之间的统计相关性.
主要成果:
- 在较高的年均表面温度下显著增强了P释放.
- 识别了增强的营养供应与变暖作为地球自然恒温器的组成部分.
- 他将这种关系与过去的变暖事件中扩大海洋无氧气的关系联系起来.
结论:
- 全球表面温度直接影响气候变化的速度.
- 由于人为气候变化,土壤中的加速流失对农业和生态系统构成风险.
- 温暖驱动的P释放可能会改变海洋的氧化还原条件并扩大无氧.
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