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Toward more realistic projections of soil carbon dynamics by Earth system models

机译:通过地球系统模型对土壤碳动力学进行更现实的预测

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Soil carbon (C) is a critical component of Earth system models (ESMs), and its diverse representations are a major source of the large spread across models in the terrestrial C sink from the third to fifth assessment reports of the Intergovernmental Panel on Climate Change (IPCC). Improving soil C projections is of a high priority for Earth system modeling in the future IPCC and other assessments. To achieve this goal, we suggest that (1) model structures should reflect real-world processes, (2) parameters should be calibrated to match model outputs with observations, and (3) external forcing variables should accurately prescribe the environmental conditions that soils experience. First, most soil C cycle models simulate C input from litter production and C release through decomposition. The latter process has traditionally been represented by first-order decay functions, regulated primarily by temperature, moisture, litter quality, and soil texture. While this formulation well captures macroscopic soil organic C (SOC) dynamics, better understanding is needed of their underlying mechanisms as related to microbial processes, depth-dependent environmental controls, and other processes that strongly affect soil C dynamics. Second, incomplete use of observations in model parameterization is a major cause of bias in soil C projections from ESMs. Optimal parameter calibration with both pool-and flux-based data sets through data assimilation is among the highest priorities for near-term research to reduce biases among ESMs. Third, external variables are represented inconsistently among ESMs, leading to differences in modeled soil C dynamics. We recommend the implementation of traceability analyses to identify how external variables and model parameterizations influence SOC dynamics in different ESMs. Overall, projections of the terrestrial C sink can be substantially improved when reliable data sets are available to select the most representative model structure, constrain parameters, and prescribe forcing fields.
机译:土壤碳(C)是地球系统模型(ESM)的关键组成部分,其不同的表示形式是政府间气候变化专门委员会第三至第五次评估报告在陆地C汇模型中大范围分布的主要来源(IPCC)。在未来的IPCC和其他评估中,改善土壤C投影对于地球系统建模具有高度优先性。为了实现此目标,我们建议(1)模型结构应反映现实世界的过程,(2)应校准参数以使模型输出与观测值匹配,并且(3)外部强迫变量应准确地规定土壤所经历的环境条件。首先,大多数土壤碳循环模型模拟了枯枝落叶产生的碳输入和分解产生的碳释放。传统上,后一个过程以一阶衰减函数表示,主要由温度,湿度,垫料质量和土壤质地调节。虽然此配方可以很好地捕获宏观的土壤有机碳(SOC)动力学,但需要更好地了解其与微生物过程,深度相关的环境控制以及其他对土壤碳动力学有重大影响的过程有关的潜在机制。其次,在模型参数化中不完全使用观测值是导致ESM的土壤C预测存在偏差的主要原因。通过数据同化对基于池和基于通量的数据集进行最佳参数校准是近期研究中的首要任务,以减少ESM之间的偏差。第三,外部变量在ESM中不一致地表示,导致模拟的土壤C动力学差异。我们建议实施可追溯性分析,以识别外部变量和模型参数化如何影响不同ESM中的SOC动态。总体而言,当可以使用可靠的数据集来选择最具代表性的模型结构,约束参数并指定强制字段时,可以大大改善地面C汇的投影。

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