首页> 外文期刊>Journal of Advances in Modeling Earth Systems >Robust Inverse Modeling of Growing Season Net Ecosystem Exchange in a Mountainous Peatland: Influence of Distributional Assumptions on Estimated Parameters and Total Carbon Fluxes
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Robust Inverse Modeling of Growing Season Net Ecosystem Exchange in a Mountainous Peatland: Influence of Distributional Assumptions on Estimated Parameters and Total Carbon Fluxes

机译:山区泥炭地生长季节净生态系统交换的鲁棒逆模型:分布假设对估计参数和总碳通量的影响

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While boreal lowland bogs have been extensively studied using the eddy‐covariance (EC) technique, less knowledge exists on mountainous peatlands. Hence, half‐hourly CO 2 fluxes of an ombrotrophic peat bog in the Harz Mountains, Germany, were measured with the EC technique during a growing season with exceptionally dry weather spells. A common biophysical process model for net ecosystem exchange was used to describe measured CO 2 fluxes and to fill data gaps. Model parameters and uncertainties were estimated by robust inverse modelling in a Bayesian framework using a population‐based Markov Chain Monte Carlo sampler. The focus of this study was on the correct statistical description of error, i.e. the differences between the measured and simulated carbon fluxes, and the influence of distributional assumptions on parameter estimates, cumulative carbon fluxes, and uncertainties. We tested the Gaussian, Laplace, and Student's t distribution as error models. The t‐distribution was identified as best error model by the deviance information criterion. Its use led to markedly different parameter estimates, a reduction of parameter uncertainty by about 40%, and, most importantly, to a 5% higher estimated cumulative CO 2 uptake as compared to the commonly assumed Gaussian error distribution. As open‐path measurement systems have larger measurement error at high humidity, the standard deviation of the error was modeled as a function of measured vapor pressure deficit. Overall, this paper demonstrates the importance of critically assessing the influence of distributional assumptions on estimated model parameters and cumulative carbon fluxes between the land surface and the atmosphere.
机译:虽然北部地区的低地沼泽已使用涡度协方差(EC)技术进行了广泛研究,但对山区泥炭地的了解却很少。因此,在极端干旱的天气条件下,使用EC技术在德国哈茨山的一块全营养泥炭沼泽中半小时的CO 2通量进行了测量。用于净生态系统交换的通用生物物理过程模型用于描述测得的CO 2通量并填补数据缺口。使用基于总体的马尔可夫链蒙特卡洛采样器在贝叶斯框架中通过鲁棒逆建模来估计模型参数和不确定性。这项研究的重点是对误差的正确统计描述,即测量和模拟的碳通量之间的差异,以及分布假设对参数估计值,累积碳通量和不确定性的影响。我们测试了高斯,拉普拉斯和学生的t分布作为误差模型。偏差信息标准将t分布确定为最佳误差模型。与通常假定的高斯误差分布相比,它的使用导致参数估计值明显不同,参数不确定性减少了大约40%,最重要的是,估计的累积CO 2吸收量增加了5%。由于开放路径测量系统在高湿度下具有较大的测量误差,因此将误差的标准偏差建模为所测得的蒸气压不足的函数。总体而言,本文证明了严格评估分布假设对估计的模型参数和地面与大气之间累积的碳通量的影响的重要性。

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