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Numerical modeling of ozone damage to plants and its effects on atmospheric CO_2 in China

机译:中国臭氧对植物的危害及其对大气CO_2影响的数值模拟

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Tropospheric ozone (O-3) is known to damage plant cells and suppress leaf photosynthesis, which can further reduce terrestrial carbon uptake and leave more carbon dioxide (CO2) in the atmosphere. While recent studies have assessed the effects of O-3 on terrestrial carbon fluxes, the potential impacts on atmospheric CO2 concentrations have not been quantified. Here, we use a regional climate model (RegCM-CHEM4) coupled with the Yale Interactive terrestrial Biosphere model YD3s to estimate the effects of O-3 exposure on atmospheric CO2 over China. Compared to simulations without O-3 effects, sensitivity experiments with O-3 damage show a significant reduction (12.1 +/- 4.4%) in the gross primary productivity (GPP), up to 35% in summer. Meanwhile, terrestrial carbon sink is suppressed by 112.2 +/- 22.5 Tg C for 2013 at the national level. Strong inhibitions of O-3 on carbon fluxes are found in North, Northeast and South Central China, where O-3 levels are high. Consequently, we find a significant increase in atmospheric CO2 concentrations due to O-3 -induced terrestrial carbon sink reduction. The increases of CO2 are more evident in the growing season. The maximum CO2 enhancement reaches as high as 6 ppm in Yunnan and Guizhou provinces. Our assessments indicate that tropospheric O-3 has a detrimental impact on plant carbon uptake and leads to more CO2 accumulating in the atmosphere. Such impacts of O-3 should be taken into account in global carbon cycle and future climate change.
机译:对流层臭氧(O-3)已知会破坏植物细胞并抑制叶片的光合作用,从而进一步减少陆地碳的吸收并在大气中留下更多的二氧化碳(CO2)。尽管最近的研究评估了O-3对陆地碳通量的影响,但尚未量化对大气CO2浓度的潜在影响。在这里,我们使用区域气候模型(RegCM-CHEM4)以及耶鲁互动地球生物圈模型YD3s来估算O-3暴露对中国大气CO2的影响。与没有O-3效应的模拟相比,具有O-3损害的敏感性实验表明,总初级生产力(GPP)显着降低(12.1 +/- 4.4%),夏季最高降低35%。同时,在国家层面,2013年地面碳汇被抑制了112.2 +/- 22.5 TgC。在华北,东北和华中南部,O-3含量高,发现了O-3对碳通量的强烈抑制作用。因此,我们发现由于O-3引起的陆地碳汇减少而导致大气CO2浓度显着增加。在生长季节,二氧化碳的增加更为明显。在云南和贵州省,最大的二氧化碳增加量高达6 ppm。我们的评估表明,对流层O-3对植物的碳吸收具有有害影响,并导致更多的CO2累积在大气中。在全球碳循环和未来气候变化中应考虑到O-3的这种影响。

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