Terrestrial Ecosystem Model in R (TEMIR) version 1.0: simulating ecophysiological responses of vegetation to atmospheric chemical and meteorological changes

A. Tai, David H. Y. Yung, T. Lam
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引用次数: 2

Abstract

Abstract. The newly developed offline land ecosystem model Terrestrial Ecosystem Model in R (TEMIR) version 1.0 is described here. This version of the model simulates plant ecophysiological (e.g., photosynthetic and stomatal) responses to varying meteorological conditions and concentrations of CO2 and ground-level ozone (O3) based on prescribed meteorological and atmospheric chemical inputs from various sources. Driven by the same meteorological data used in the GEOS-Chem chemical transport model, this allows asynchronously coupled experiments with GEOS-Chem simulations with unique coherency for investigating biosphere–atmosphere chemical interactions. TEMIR agrees well with FLUXNET site-level gross primary productivity (GPP) in terms of both the diurnal and monthly cycles (correlation coefficients R2>0.85 and R2>0.8, respectively) for most plant functional types (PFTs). Grass and shrub PFTs have larger biases due to generic model representations. The model performs best when driven by local site-level meteorology rather than reanalyzed gridded meteorology. Simulation using gridded meteorology agrees well for annual GPP in seasonality and spatial distribution with a global average of 134 Pg C yr−1. Application of Monin–Obukhov similarity theory to infer canopy conditions from gridded meteorology does not improve model performance, predicting an increase of +7 % in global GPP. Present-day O3 concentrations simulated by GEOS-Chem and an O3 damage scheme at high sensitivity show a 2 % reduction in global GPP with prominent reductions of up to 15 % in eastern China and the eastern USA. Regional correlations are generally unchanged when O3 is present and biases are reduced, especially for regions with high O3 damage. An increase in atmospheric CO2 concentration of 20 ppmv from the level in 2000 to the level in 2010 modestly decreases O3 damage due to reduced stomatal uptake, consistent with ecophysiological understanding. Our work showcases the utility of this version of TEMIR for evaluating biogeophysical responses of vegetation to changes in atmospheric composition and meteorological conditions.
R 语言陆地生态系统模型(TEMIR)1.0 版:模拟植被对大气化学和气象变化的生态生理反应
摘要本文介绍了新开发的离线陆地生态系统模型 Terrestrial Ecosystem Model in R (TEMIR) 1.0 版。该版本的模型模拟了植物生态生理(如光合作用和气孔)对不同气象条件以及二氧化碳和地面臭氧(O3)浓度的响应,这些响应基于规定的气象条件和来自不同来源的大气化学输入。在 GEOS-Chem 化学传输模型中使用的相同气象数据的驱动下,可与 GEOS-Chem 模拟进行异步耦合实验,在研究生物圈-大气化学相互作用方面具有独特的一致性。TEMIR 与 FLUXNET 站点级总初级生产力(GPP)在大多数植物功能类型(PFTs)的昼夜周期和月度周期方面(相关系数 R2>0.85 和 R2>0.8)都非常吻合。禾本科和灌木植物功能类型由于通用模型的表述而存在较大偏差。当模型由当地站点级气象而非重新分析的网格气象驱动时,模型表现最佳。使用网格气象学模拟的年 GPP 在季节性和空间分布上与全球平均值 134 Pg C yr-1 非常吻合。应用莫宁-奥布霍夫相似性理论从网格气象学推断冠层条件并没有改善模型性能,预测全球 GPP 增加了 +7%。用 GEOS-Chem 和高灵敏度 O3 破坏方案模拟的当今 O3 浓度显示,全球 GPP 下降了 2%,中国东部和美国东部的显著下降高达 15%。当存在 O3 时,区域相关性一般不会改变,偏差也会减小,尤其是在 O3 破坏程度较高的区域。大气中的二氧化碳浓度从 2000 年的水平增加 20 ppmv 到 2010 年的水平,由于气孔吸收量减少,O3 损害会适度降低,这与生态生理学的理解是一致的。我们的工作展示了这一版本的 TEMIR 在评估植被对大气成分和气象条件变化的生物地球物理响应方面的实用性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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