Department of Geography and Planning, University of Toronto, Toronto, ON, Canada.
Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California.
Glob Chang Biol. 2019 Jul;25(7):2499-2514. doi: 10.1111/gcb.14624. Epub 2019 Apr 10.
The terrestrial biosphere plays a critical role in mitigating climate change by absorbing anthropogenic CO emissions through photosynthesis. The rate of photosynthesis is determined jointly by environmental variables and the intrinsic photosynthetic capacity of plants (i.e. maximum carboxylation rate; ). A lack of an effective means to derive spatially and temporally explicit has long hampered efforts towards estimating global photosynthesis accurately. Recent work suggests that leaf chlorophyll content (Chl ) is strongly related to , since Chl and are both correlated with photosynthetic nitrogen content. We used medium resolution satellite images to derive spatially and temporally explicit Chl , which we then used to parameterize within a terrestrial biosphere model. Modelled photosynthesis estimates were evaluated against measured photosynthesis at 124 eddy covariance sites. The inclusion of Chl in a terrestrial biosphere model improved the spatial and temporal variability of photosynthesis estimates, reducing biases at eddy covariance sites by 8% on average, with the largest improvements occurring for croplands (21% bias reduction) and deciduous forests (15% bias reduction). At the global scale, the inclusion of Chl reduced terrestrial photosynthesis estimates by 9 PgC/year and improved the correlations with a reconstructed solar-induced fluorescence product and a gridded photosynthesis product upscaled from tower measurements. We found positive impacts of Chl on modelled photosynthesis for deciduous forests, croplands, grasslands, savannas and wetlands, but mixed impacts for shrublands and evergreen broadleaf forests and negative impacts for evergreen needleleaf forests and mixed forests. Our results highlight the potential of Chl to reduce the uncertainty of global photosynthesis but identify challenges for incorporating Chl in future terrestrial biosphere models.
陆地生物圈通过光合作用吸收人为 CO 排放,在缓解气候变化方面发挥着关键作用。光合作用的速度是由环境变量和植物内在光合作用能力(即最大羧化率;)共同决定的。长期以来,由于缺乏一种有效的方法来明确地推导出 ,因此,准确估计全球光合作用的努力受到了阻碍。最近的研究表明,叶片叶绿素含量(Chl)与 密切相关,因为 Chl 和 都与光合作用氮含量相关。我们使用中等分辨率的卫星图像推导出明确的时空 Chl,然后将其用于陆地生物圈模型中的参数化。模型化的光合作用估算值与 124 个涡度协方差站点的实测光合作用进行了评估。在陆地生物圈模型中包含 Chl 提高了光合作用估算值的时空变异性,平均减少了涡度协方差站点的偏差 8%,其中农田(21%的偏差减少)和落叶林(15%的偏差减少)的改进最大。在全球范围内,包含 Chl 减少了陆地光合作用的估算值 9 PgC/年,并提高了与重建的太阳诱导荧光产物和从塔测量扩展的网格化光合作用产物的相关性。我们发现 Chl 对落叶林、农田、草原、热带稀树草原和湿地的模型化光合作用有积极的影响,但对灌木林和常绿阔叶林有混合影响,对常绿针叶林和混交林有负面影响。我们的结果强调了 Chl 减少全球光合作用不确定性的潜力,但也为未来陆地生物圈模型中纳入 Chl 提出了挑战。