土壤呼吸驱动的CO2脉冲主导着澳大利亚的流量变化
Eva-Marie Metz1, Sanam N Vardag1,2, Sourish Basu3,4
1Institute of Environmental Physics, Heidelberg University, 69120 Heidelberg, Germany.
概括
降雨后澳大利亚的二氧化碳 (CO2) 脉冲导致全球沉降变化. 这些通过卫星检测的干旱季末二氧化碳排放对澳大利亚的碳平衡和气候模型产生重大影响.
科学领域:
- 地球系统科学
- 大气化学
- 生态学
背景情况:
- 澳大利亚的陆地生态系统显著影响全球二氧化碳 (CO2) 沉降的变化.
- 来自偏远地区的有限现场数据阻碍了对二氧化碳流动因素的理解.
研究的目的:
- 通过卫星观测,研究澳大利亚二氧化碳流动变化的驱动因素.
- 量化观察到的二氧化碳脉冲对澳大利亚年度碳平衡的影响.
主要方法:
- 2009年至2018年间卫星测量大气二氧化碳的分析.
- 卫星衍生的二氧化碳流与以前的反转和自下而上的估计进行比较.
主要成果:
- 在干旱季结束时,在澳大利亚发现了反复出现的二氧化碳脉冲.
- 这些脉冲发生在降雨开始后,
- 发现的脉冲造成的季节性二氧化碳变化比之前估计的多两倍.
结论:
- 干旱季末的二氧化碳排放是控制澳大利亚年度碳平衡变化的重要因素.
- 土壤复湿是影响大陆范围二氧化碳流量的关键过程.
- 这些发现对全球气候碳循环反建模具有重要意义.
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