在异常温暖的一年后,长期抑制生态系统的二氧化碳吸收
John A Arnone1, Paul S J Verburg, Dale W Johnson
1Desert Research Institute, Reno, Nevada 89512, USA. jarnone@dri.edu
Nature
|September 19, 2008
概括
异常温暖的年份通过诱导干旱和刺激土壤呼吸来减少陆地生态系统的碳封存. 二氧化碳吸收的恢复需要两年,这表明频繁的变暖可能会降低地球的碳沉积能力.
科学领域:
- 生态生态学 生态生态学
- 生物地质化学生物地质化学
- 气候科学 气候科学
背景情况:
- 地球上的生态系统通过光合作用和呼吸来调节大气中的二氧化碳.
- 气候变化显著影响生态系统碳交换 (NEE).
- 量化单一气候变量的影响,如温度异常,在NEE在跨年规模是具有挑战性的,因为混因素.
研究的目的:
- 通过实验量化温度异常对生态系统净二氧化碳交换 (NEE) 和碳封存的影响.
- 为了确定经历了变暖后生态系统碳平衡的恢复时间.
主要方法:
- 使用了四个大型封闭式溶解仪,每个含有六个复制的12,000公斤高草草原单体.
- 在四年研究的第二年,将一半的单立体暴露在异常温暖的一年中.
- 在整个研究过程中,持续监测生态系统过程,包括NEE.
主要成果:
- 气候变暖引起的干旱在温暖的一年中抑制了净初级生产率.
- 在异常发生后的一年内,变暖刺激了土壤异质性呼吸.
- 生态系统需要两年时间才能使NEE恢复到控制水平,这导致在研究期间净碳捕获量减少了三倍.
结论:
- 不常见的异常温暖的年份可以显著减少生态系统的碳捕获.
- 更频繁的变暖事件,可能由人为二氧化碳驱动,可能导致陆地碳汇持续下降.
- 了解这些影响对于预测未来气候变化动态至关重要.
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