Forest Hydrology Laboratory, Division of Forest and Biomaterials Science, Graduate School of Agriculture, Kyoto University, Kyoto 606-8502, Japan.
Key Laboratory of Tropical Forest Ecology, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Menglun 666303, China.
Tree Physiol. 2024 May 5;44(5). doi: 10.1093/treephys/tpae041.
This study aimed to reveal the mechanism and significance of wet canopy photosynthesis during and after rainfall in temperate coniferous ecosystems by evaluating the influence of abaxial leaf interception on wet canopy photosynthesis. We used the eddy covariance method in conjunction with an enclosed-path gas analyser to conduct continuous ecosystem CO2 flux observations in a Japanese cypress forest within the temperate Asian monsoon area over 3 years. The observation shows that wet-canopy CO2 uptake predominantly occurred during the post-rainfall canopy-wet period rather than the during-rainfall period. Then, the measured canopy-wet net ecosystem exchange was compared with the soil-vegetation-atmosphere transfer multilayer model simulations under different parameter settings of the abaxial (lower) leaf surface wet area ratio. The multilayer model predicted net ecosystem exchange most accurately when it assumed the wet area ratio of the abaxial surface was 50% both during and after rainfall. For the wet canopy both during and after rainfall, the model overestimated CO2 uptake when it assumed no abaxial interception in the simulation, but underestimated CO2 uptake when it assumed that the entire abaxial leaf surface was wet. These results suggest that the abaxial surface of the Japanese cypress leaf is only partly wet to maintain stomatal openness and a low level of photosynthesis. These results allow for an evaluation of the effect of rainfall on forest carbon circulation under a changing climate, facilitating an improvement of ecosystem carbon exchange models.
本研究旨在通过评估背叶面截留对湿树冠光合作用的影响,揭示温带针叶林生态系统降雨期间和之后湿树冠光合作用的机制和意义。我们使用涡度协方差法结合封闭路径气体分析仪,在温带亚洲季风区的 3 年内对日本柏木林进行了连续的生态系统 CO2 通量观测。观测结果表明,湿树冠 CO2 吸收主要发生在雨后树冠湿润期,而不是降雨期间。然后,将测量的树冠湿润净生态系统交换与土壤-植被-大气转移多层模型模拟进行比较,在不同的背叶面(下)湿润面积比参数设置下。当假设背叶面湿润面积比在降雨期间和之后均为 50%时,多层模型对净生态系统交换的预测最为准确。对于降雨期间和之后的湿树冠,当模拟中假设没有背叶面截留时,模型高估了 CO2 吸收,但当假设整个背叶面湿润时,模型低估了 CO2 吸收。这些结果表明,日本柏木叶的背叶面只有部分湿润,以保持气孔开放和较低的光合作用水平。这些结果可以评估气候变化下降雨对森林碳循环的影响,有助于改进生态系统碳交换模型。