首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Improving canopy processes in the Community Land Model version 4 (CLM4) using global flux fields empirically inferred from FLUXNET data
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Improving canopy processes in the Community Land Model version 4 (CLM4) using global flux fields empirically inferred from FLUXNET data

机译:使用根据FLUXNET数据经验推断的全局通量字段来改善社区土地模型第4版(CLM4)中的冠层过程

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The Community Land Model version 4 (CLM4) overestimates gross primary production (GPP) compared with ata‐driven estimates and other process models. We use global, spatially gridded GPP and latent heat flux upscaled from the FLUXNET network of eddy covariance towers to evaluate and improve canopy processes inCLM4. We investigate differences in GPP and latent heat flux arising from model parameterizations (termed model structural error) and from uncertainty in the photosynthetic parameter V_(c max) (termed model parameter uncertainty). Model structural errors entail radiative transfer, leaf photosynthesis and stomatal conductance, and canopy scaling of leaf processes. Model structural revisions reduce global GPP over the period 1982-2004 from 165 Pg C yr~(?1) to 130 Pg C yr~(?1), and global evapotranspiration decreases from 68,000 km~3 yr~(?1) to 65,000 km~3 yr~(?1), within the uncertainty of FLUXNET‐based estimates. Colimitation of photosynthesis is a cause of the improvements, as are revisions to photosynthetic parameters and their temperature dependency. Improvements are seen in all regions and seasonally over the course of the year. Similar improvements occur in latent heat flux. Uncertainty in Vc max produces effects of comparable magnitude as model structural errors, but of offsetting sign. This suggests that model structural errors can be compensated by parameter adjustment, and this may explain the lack of consensus in values for V_(c max) used in terrestrial biosphere models. Our analyses show that despite inherent uncertainties global flux fields empirically inferred from FLUXNET data are a valuable tool to guide terrestrial biosphere model development and evaluation.
机译:与ata驱动的估计和其他过程模型相比,社区土地模型第4版(CLM4)高估了初级生产总值(GPP)。我们使用全局,空间网格化的GPP和涡流协方差塔FLUXNET网络上的潜热通量来评估和改善CLM4中的冠层过程。我们研究了GPP和潜热通量的差异,这些差异是由模型参数化(称为模型结构误差)和光合作用参数V_(c max)的不确定性(称为模型参数不确定性)引起的。模型结构错误包括辐射转移,叶片光合作用和气孔导度以及叶片过程的冠层缩放。模型结构修正使1982-2004年期间的全球GPP从165 Pg C yr〜(?1)降低到130 Pg C yr〜(?1),全球蒸散量从68,000 km〜3 yr〜(?1)降至65,000 km〜3 yr〜(?1),在基于FLUXNET的估计的不确定性范围内。光合作用的限制是改善的原因,光合作用参数及其温度依赖性的修订也是如此。在一年中,所有地区和季节都有改善。潜热通量也有类似的改善。 Vc max的不确定性会产生与模型结构误差相当的幅度的影响,但会产生符号抵消。这表明可以通过参数调整来补偿模型结构误差,这可以解释在陆地生物圈模型中使用的V_(c max)值缺乏共识。我们的分析表明,尽管存在固有不确定性,但从FLUXNET数据凭经验推断出的全球通量场仍是指导陆地生物圈模型开发和评估的有价值的工具。

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