由CO2肥驱动的丰富的北极地区的绿化
Sandeep Thayamkottu1, T Luke Smallman2,3, Jaan Pärn1
1Institute of Ecology and Earth Sciences, University of Tartu, Vanemuise Street. 46, 51003 Tartu, Estonia.
概括
温暖的北极泥炭地显示,由于二氧化碳施肥,二氧化碳的吸收增加,导致更多的碳分配给树叶. 这项研究阐明了这些重要生态系统中的碳循环动态.
科学领域:
- 生态生态学 生态生态学
- 气候科学 气候科学
- 生物地质化学生物地质化学
背景情况:
- 玻里亚泥炭地是重要的碳汇,储存大量有机碳.
- 北极地区正在以加速的速度变暖,影响了泥炭地碳循环.
- 在气候变化下,了解影响泥炭地二氧化碳 (CO2) 流动的因素至关重要.
研究的目的:
- 为了调查二氧化碳流动在北极丰富的中年间变化的驱动因素.
- 为了确定内部碳分配模式,以应对气候变暖.
主要方法:
- 利用了一种中等复杂度的陆地生态系统模型.
- 采用贝叶斯模型-数据融合框架进行校准.
- 综合的联变量,卫星观测和2014-2020年现场数据.
主要成果:
- 观察到由二氧化碳施肥驱动的绿化趋势,增加了原始生产总值 (GPP).
- 到2020年,GPP与2014年相比增加了大约75千克米-2年-1.
- 异质性呼吸保持不变,叶片的碳分配增加.
结论:
- 二氧化碳施肥是该生态系统中GPP增加的一个关键因素.
- 生态系统将更多的碳分配给树叶,这表明碳储存的转变.
- 这些发现凸显了泥炭地碳动态对气候变化的复杂反应.
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