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首页> 外文期刊>Journal of Advances in Modeling Earth Systems >Seeing the Canopy for the Branches: Improved Within Canopy Scaling of Leaf Nitrogen
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Seeing the Canopy for the Branches: Improved Within Canopy Scaling of Leaf Nitrogen

机译:看到分支机构的天篷:叶片氮的冠层缩放内改善

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摘要

Transitioning across biological scales is a central challenge in land surface models. Processes that operate at the scale of individual leaves must be scaled to canopies, and this is done using dedicated submodels. Here, we focus on a submodel that prescribes how light and nitrogen are distributed through plant canopies. We found a mathematical inconsistency in a submodel implemented in the Community and Energy Land Models (CLM and ELM), which incorporates twigs, branches, stems, and dead leaves in nitrogen scaling from leaf to canopy. The inconsistency leads to unrealistic (physically impossible) values of the nitrogen scaling coefficient. The mathematical inconsistency is a general mistake, that is, would occur in any model adopting this particular submodel. We resolve the inconsistency by allowing distinct profiles of stems and branches versus living leaves. We implemented the updated scheme in the ELM and find that the correction reduces global mean gross primary production (GPP) by 3.9?Pg C (3%). Further, when stems and branches are removed from the canopy in the updated model (akin to models that ignore shading from stems), global GPP increases by 4.1?Pg C (3.2%), because of reduced shading. Hence, models that entirely ignore stem shading also introduce errors in the global spatial distribution of GPP estimates, with a strong signal in the tropics, increasing GPP there by over 200?g?C?m?2?yr?1. Appropriately incorporating stems and other nonphotosynthesizing material into the light and nitrogen scaling routines of global land models, will improve their biological realism and accuracy. Plain Language Summary Land surface models that estimate the flow of chemical elements, water, and energy into and out of terrestrial vegetation rely on many submodels. We found a mathematical inconsistency in a widely used submodel that controls how light and nitrogen are distributed through the plant canopy. The inconsistency is centered around how twigs, branches, stems, and dead leaves influence the distribution of nitrogen, and thus photosynthesis, throughout the canopy. When we corrected the inconsistency, we found that the modeled global carbon uptake of terrestrial vegetation decreased by 3%. We further show that completely ignoring twigs, branches, stems, and dead leaves in canopy upscaling inappropriately increases estimated global gross primary production, by failing to account for the shade they cast, with the greatest increases in the tropics.
机译:在生物尺度过渡是陆地表面模型中的中心挑战。必须将以单独的叶子的规模运行的进程扩展到檐篷,这是使用专用子模型完成的。在这里,我们专注于规定光线和氮气如何通过植物檐篷分配的子模型。我们在社区和能源土地模型(CLM和ELM)中实施了一个亚模型中的数学不一致,其将枝条,分支,茎和死叶纳入从叶子到树冠中的氮气缩放。不一致导致氮缩放系数的不切实际(物理上不可能)值。数学不一致是一个常规错误,即在采用这个特定子模型的任何模型中都会发生。我们通过允许不同的茎和分支与生物叶子的不同曲线来解决不一致。我们在ELM中实施了更新的方案,并发现校正将全局平均初级生产(GPP)减少3.9?PG C(3%)。此外,当从更新的模型中从冠层中除去茎和分支时(类似于忽略茎的遮蔽的模型),由于阴影降低,全局GPP增加了4.1?PG C(3.2%)。因此,完全忽略阀杆着色的模型也引入了GPP估计的全局空间分布中的错误,热带中具有强烈的信号,增加了200多个?G?C?2?2?YR?1。适当地将茎和其他非空白的非空白化物质化为全球土地模型的光线和氮素缩放常规,将提高其生物学现实主义和准确性。普通语言摘要土地表面模型估算化学元素,水和能量流入和脱离陆地植被的流动依赖于许多子模型。我们在广泛使用的子模型中发现了一种数学不一致,控制光线和氮气如何通过植物冠层分布。不一致的是围绕着树枝,分支,茎和死叶来影响氮气的分布,从而占整个冠层的分布。当我们纠正不一致时,我们发现,陆地植被的模型碳吸收下降了3%。我们进一步表明,通过未能考虑他们所铸造的阴影,可以完全忽视树冠上的俯视,分支,茎和死亡叶,增加了估计的全球初级生产,最大的增加,热带地区最大。

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