由于大气CO2季节性循环的变化而受到限制的土地光合作用
Sabrina Wenzel1, Peter M Cox2, Veronika Eyring1
1Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany.
Nature
|September 30, 2016
概括
增加二氧化碳的水平会促进植物生长, 但确切的数量是不确定的. 这项研究使用季节性CO2循环变化来限制二氧化碳受精对全球植物生产力的影响.
科学领域:
- 气候科学
- 生态学
- 生物地质化学
背景情况:
- 由于未知植被对大气二氧化碳增加的反应,对未来气候变化的预测存在很大的不确定性.
- 气候碳循环模型一致认为,二氧化碳的增加提高了陆地总初级生产率 (GPP),但这种施肥效应的幅度有很大差异 (二氧化碳的增加增加增加了60%).
研究的目的:
- 通过观察大气二氧化碳季节性循环幅度的变化,证明大规模二氧化碳施肥的新兴限制.
- 在气候碳循环模型中将大气二氧化碳测量与陆地GPP趋势联系起来.
主要方法:
- 大气二氧化碳测量的比较 (阿拉斯加巴罗点;夏威夷库穆卡希角) 与气候碳循环模型的历史模拟.
- 分析 CO2 季节周期的幅度与 GPP 的 CO2 施肥幅度之间的关系.
主要成果:
- 在这两个地点观察到的季节性CO2周期幅度的增加与年平均GPP的增加一致.
- 碳二氧化肥的差异解释了模型趋势的扩散.
- 跨模型的季节性CO2幅度和GPPCO2受精量之间存在几乎线性关系.
结论:
- GPP二氧化碳受精的新出现的限制源于观察到的季节性二氧化碳幅度趋势.
- 在二氧化碳度翻倍的情况下,高度的 GPP 增加为 37±9%,而热带以外的生态系统则为 32±9%.
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