林冠层内垂直气温分布对光合和蒸腾作用的影响

H. Komatsu, T. Kumagai, N. Hotta, 小松 光, 熊谷 朝臣, 堀田 紀文
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引用次数: 3

摘要

本研究探讨了利用多层冠层模型准确模拟森林冠层内垂直气温分布是否对预测垂直光合作用和蒸腾作用分布至关重要。通过对早期森林冠层内垂直水分分布的观测研究,我们发现森林冠层内常见的垂直水分差异小于3.0°C。我们用叶片尺度的蒸腾-光合作用模型证明了3。当AT高于约15℃时,0℃AT差异对叶片尺度光合作用和蒸腾速率的影响小于林冠层内光合有效辐射(PAR)强度的常见垂直差异。而当AT低于10℃时,叶片光合速率和蒸腾速率的差异大于PAR差异。然而,当AT变化3.0°C时,速率的变化范围与叶片尺度蒸腾-光合作用模型的可预测性相当。因此,我们得出结论,在这个阶段,精确模拟AT分布对于使用多层冠层模型计算垂直光合作用和蒸腾分布是不必要的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effects of vertical air temperature distribution within forest canopies on photosynthesis and transpiration
This study examined whether accurately simulating vertical air temperature (AT) distribution within forest canopies is essential for predicting vertical photosynthesis and transpiration distribution using multilayer canopy models. Inspecting earlier observational studies that reported vertical AT distribution within forest canopies, we showed that the common vertical AT difference within forest canopies was lower than 3.0 °C. We showed, using a leaf-scale transpiration-photosynthesis model, that a 3. 0 °C AT difference caused smaller differences in leaf-scale photosynthesis and transpiration rates than a common vertical difference in photosynthetic active radiation (PAR) intensity within forest canopies when AT was higher than ca. 15 °C. While, the AT difference caused larger differences in leaf-scale photosynthetic and transpiration rates than the PAR difference when AT was lower than ca. 10 °C . However, the ranges in the rates with changing AT by 3.0 °C were comparable with predictability of a leaf-scale transpiration-photosynthesis model. Thus, we conclude that accurately simulating AT distribution is not essential at this stage for calculating vertical photosynthesis and transpiration distribution using multilayer canopy models.
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