结合局部模式定标与紧急约束方法降低热带土地碳循环反馈的不确定性

N. Raoult, T. Jupp, B. Booth, P. Cox
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引用次数: 0

摘要

摘要陆地碳循环在气候变化中的作用仍然非常不确定。预测传播的一个关键来源与光合作用对变暖的假定反应有关,尤其是在热带地区。光合作用的最佳温度决定了变暖对光合作用的影响是积极的还是消极的,从而在二氧化碳引发的全球变暖下放大或抑制光合作用的二氧化碳施肥。陆地碳循环模型已经根据当地涡通量测量进行了广泛的校准,但这之前并没有被明确转化为热带陆地碳汇如何应对变暖的不确定性降低。使用之前使用哈德利中心耦合气候-碳循环模型(HadCM3C)第3版进行的参数扰动集合,我们确定了光合作用的最佳温度与本世纪末大气CO2的预计量之间的紧急关系,这在热带森林中尤为重要。我们将其与光合作用最佳温度的约束相结合,该约束来自使用联合英国陆地环境模拟器(JULES)陆地表面模型的伴随进行的涡度协方差测量。总之,耦合模型的涌现关系和对光合作用最佳温度的约束定义了在共同排放情景(A1B)下,在HadCM3C耦合气候-碳循环中对未来大气CO2的涌现约束。紧急约束提高了模拟CO2变化的概率密度(2100–1900),并将其峰值移动到497的较低值 ± 91,而607 ± 128 ppmv(百万分之一体积)。尽管这一结果可能与模型和场景有关,但它证明了将大规模紧急约束方法与使用详细局部测量的参数估计相结合的潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Combining local model calibration with the emergent constraint approach to reduce uncertainty in the tropical land carbon cycle feedback
Abstract. The role of the land carbon cycle in climate change remains highly uncertain. A key source of the projection spread is related to the assumed response of photosynthesis to warming, especially in the tropics. The optimum temperature for photosynthesis determines whether warming positively or negatively impacts photosynthesis, thereby amplifying or suppressing CO2 fertilisation of photosynthesis under CO2-induced global warming. Land carbon cycle models have been extensively calibrated against local eddy flux measurements, but this has not previously been clearly translated into a reduced uncertainty in terms of how the tropical land carbon sink will respond to warming. Using a previous parameter perturbation ensemble carried out with version 3 of the Hadley Centre coupled climate–carbon cycle model (HadCM3C), we identify an emergent relationship between the optimal temperature for photosynthesis, which is especially relevant in tropical forests, and the projected amount of atmospheric CO2 at the end of the century. We combine this with a constraint on the optimum temperature for photosynthesis, derived from eddy covariance measurements using the adjoint of the Joint UK Land Environment Simulator (JULES) land surface model. Taken together, the emergent relationship from the coupled model and the constraint on the optimum temperature for photosynthesis define an emergent constraint on future atmospheric CO2 in the HadCM3C coupled climate–carbon cycle under a common emissions scenario (A1B). The emergent constraint sharpens the probability density of simulated CO2 change (2100–1900) and moves its peak to a lower value of 497 ± 91 compared to 607 ± 128 ppmv (parts per million by volume) when using the equal-weight prior. Although this result is likely to be model and scenario dependent, it demonstrates the potential of combining the large-scale emergent constraint approach with a parameter estimation using detailed local measurements.
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