大气测量显示了亚马逊碳平衡对干旱的敏感性
L V Gatti1, M Gloor2, J B Miller3
11] Instituto de Pesquisas Energéticas e Nucleares (IPEN)-Comissao Nacional de Energia Nuclear (CNEN)-Atmospheric Chemistry Laboratory, 2242 Avenida Professor Lineu Prestes, Cidade Universitaria, Sao Paulo CEP 05508-000, Brazil [2].
Nature
|February 7, 2014
概括
亚马逊盆地在2010年干旱期间损失了大量的碳,但在潮湿的一年是碳中和的. 降水极端程度的增加可能会使亚马逊因火灾和干旱而变成碳源.
科学领域:
- 气候科学是气候科学.
- 生态生态学 生态生态学
- 生物地质化学生物地质化学
背景情况:
- 土地碳池和气候反导致全球气候预测的不确定性.
- 亚马逊盆地是一个主要的碳储备区,面临着气温上升和极端天气.
- 了解热带碳预算和反机制至关重要.
研究的目的:
- 报告亚马逊盆地的季节性和年度碳平衡.
- 确定控制陆地碳预算对气候异常敏感性的机制.
- 评估干旱和雨季对亚马逊碳流的影响.
主要方法:
- 使用了2010年 (干旱年) 和2011年 (潮年) 的二氧化碳和一氧化碳测量结果.
- 计算了盆地范围内的碳平衡和净生物群交换 (NBE).
- 嵌入的碳损失估计从使用二氧化碳测量的火灾.
主要成果:
- 亚马逊盆地在干旱年减少了0.48 ± 0.18 Pg C yr{-1},在潮湿年几乎是碳中和 (0.06 ± 0.1 Pg C yr{-1)).
- 在干旱的一年里,植被是碳中和的;在潮湿的一年里,它是碳汇 (0.25 ± 0.14 Pg C yr(-1)).
- 干旱抑制了光合作用,在2010年中和了碳汇.
结论:
- 湿度的可用性显著影响了亚马逊的碳平衡.
- 持续的极端降水可能会将亚马逊从碳汇转变为碳源.
- 这种转变将是由于火灾排放量增加和干旱引起的净生物群交换抑制造成的.
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