过度的湿度抑制了亚马逊森林的碳沉降,在季节性水余下
Shulin Ren1,2,3, Xiyan Xu1, Gensuo Jia1,2
1State Key Laboratory of Earth System Numerical Modeling and Application, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China.
Global change biology
|August 9, 2025
概括
由于降雨模式的改变,亚马逊森林的碳吸收量正在下降. 增加的湿度限制了光合作用,影响了碳预算,特别是在受干扰地区之外.
科学领域:
- * 生态学 * 生态学
- * 气候科学 气候科学
- * 森林碳循环过程
背景情况:
- *亚马逊盆地的水文循环正在转向更潮湿的季节和更干燥的干旱季节.
- * 这种水文转变对亚马逊森林碳预算的影响尚不清楚.
- *以前的研究还没有充分探讨干旱压力之外的季节性变化的作用.
研究的目的:
- * 调查不断变化的水文模式如何影响亚马逊森林的碳预算.
- * 量化过去二十年森林碳汇的变化.
- * 确定导致碳吸收变化的特定气候因素.
主要方法:
- *对多个基于观察的碳流数据集的分析.
- *利用了气候数据集,包括降水和蒸汽压力赤字 (VPD).
- *从碳流量数据推断总初级产量 (GPP) 来评估光合作用吸收.
主要成果:
- * 亚马逊森林的碳汇在过去20年里有所减少.
- *60.3%的减少发生在没有人类直接干扰的地区.
- * 52.6%的下降发生在雨季,主要是由于有限的光合作用活性辐射 (PAR) 和过度潮湿,而不仅仅是干旱.
结论:
- *水文模式的转变对亚马逊森林的碳汇产生了负面影响.
- * 雨季期间的过度潮湿,加上低的PAR,大大降低了碳吸收.
- *这些发现强调了在评估森林碳预算时考虑雨季条件和过度湿度的重要性,而不仅仅是干旱.
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