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Evaluation of atmospheric aerosol and tropospheric ozone effects on global terrestrial ecosystem carbon dynamics.

机译:评估大气气溶胶和对流层臭氧对全球陆地生态系统碳动态的影响。

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摘要

The increasing human activities have produced large amounts of air pollutants ejected into the atmosphere, in which atmospheric aerosols and tropospheric ozone are considered to be especially important because of their negative impacts on human health and their impacts on global climate through either their direct radiative effect or indirect effect on land-atmosphere CO2 exchange. This dissertation dedicates to quantifying and evaluating the aerosol and tropospheric ozone effects on global terrestrial ecosystem dynamics using a modeling approach.;An ecosystem model, the integrated Terrestrial Ecosystem Model (iTem), is developed to simulate biophysical and biogeochemical processes in terrestrial ecosystems. A two-broad-band atmospheric radiative transfer model together with the Moderate-Resolution Imaging Spectroradiometer (MODIS) measured atmospheric parameters are used to well estimate global downward solar radiation and the direct and diffuse components in comparison with observations. The atmospheric radiative transfer modeling framework were used to quantify the aerosol direct radiative effect, showing that aerosol loadings cause 18.7 and 12.8 W m -2 decrease of direct-beam Photosynthetic Active Radiation (PAR) and Near Infrared Radiation (NIR) respectively, and 5.2 and 4.4 W m -2 increase of diffuse PAR and NIR, respectively, leading to a total 21.9 W m-2 decrease of total downward solar radiation over the global land surface during the period of 2003-2010. The results also suggested that the aerosol effect may be overwhelmed by clouds because of the stronger extinction and scattering ability of clouds.;Applications of the iTem with solar radiation data and with or without considering the aerosol loadings shows that aerosol loading enhances the terrestrial productions [Gross Primary Production (GPP), Net Primary Production (NPP) and Net Ecosystem Production (NEP)] and carbon emissions through plant respiration (RA) in global terrestrial ecosystems over the period of 2003-2010. Ecosystem heterotrophic respiration (RH) was negatively affected by the aerosol loading. These results support previous conclusions of the advantage of aerosol light scattering effect on plant productions in other studies but suggest there is strong spatial variation. This study finds indirect aerosol effects on terrestrial ecosystem carbon dynamics through affecting plant phenology, thermal and hydrological environments. All these evidences suggested that the aerosol direct radiative effect on global terrestrial ecosystem carbon dynamics should be considered to better understand the global carbon cycle and climate change.;An ozone sub-model is developed in this dissertation and fully coupled with iTem. The coupled model, named iTemO3 considers the processes of ozone stomatal deposition, plant defense to ozone influx, ozone damage and plant repairing mechanism. By using a global atmospheric chemical transport model (GACTM) estimated ground-level ozone concentration data, the model estimated global annual stomatal ozone deposition is 234.0 Tg O3 yr-1 and indicates which regions have high ozone damage risk. Different plant functional types, sunlit and shaded leaves are shown to have different responses to ozone. The model predictions suggest that ozone has caused considerable change on global terrestrial ecosystem carbon storage and carbon exchanges over the study period 2004-2008. The study suggests that uncertainty of the key parameters in iTemO3 could result in large errors in model predictions. Thus more experimental data for better model parameterization is highly needed.
机译:人类活动的增加导致大量空气污染物排放到大气中,大气中的气溶胶和对流层臭氧被认为特别重要,因为它们对人类健康产生负面影响,并通过直接辐射效应或对全球气候的影响对陆地-大气CO2交换的间接影响。本论文致力于通过一种建模方法来量化和评估气溶胶和对流层臭氧对全球陆地生态系统动力学的影响。建立了生态系统模型,即综合陆地生态系统模型(iTem),以模拟陆地生态系统中的生物物理和生物地球化学过程。与观测值相比,使用了两个宽带大气辐射传输模型以及中分辨率成像光谱仪(MODIS)测得的大气参数,可以很好地估算全球向下的太阳辐射以及直接分量和扩散分量。大气辐射传递模型框架用于量化气溶胶的直接辐射效应,表明气溶胶负荷分别导致直接束光合有效辐射(PAR)和近红外辐射(NIR)分别降低了18.7和12.8 W m -2,以及5.2散射PAR和NIR分别增加了4.4 W m -2和2003 W--2,导致2003-2010年全球陆地表面向下总太阳辐射总共减少了21.9 W m-2。结果还表明,由于云具有更强的消光和散射能力,因此气溶胶作用可能会被云所淹没。; iTem在具有太阳辐射数据且有或没有考虑气溶胶负荷的情况下的应用表明,气溶胶负荷可增强陆地生产[ 2003-2010年期间,全球陆地生态系统中的初级生产总值(GPP),净初级生产(NPP)和生态系统净产量(NEP)以及通过植物呼吸作用产生的碳排放量。生态系统异养呼吸(RH)受到气溶胶负荷的负面影响。这些结果支持了其他研究中关于气溶胶光散射效应对植物生产优势的先前结论,但表明存在很大的空间变化。这项研究通过影响植物物候,热力和水文环境,发现了气溶胶对陆地生态系统碳动态的间接影响。所有这些证据表明,应考虑气溶胶对全球陆地生态系统碳动力学的直接辐射作用,以更好地了解全球碳循环和气候变化。;本文开发了一个臭氧子模型,并与iTem充分耦合。名为iTemO3的耦合模型考虑了臭氧气孔沉积,植物对臭氧入侵的防御,臭氧破坏和植物修复机制的过程。通过使用全球大气化学迁移模型(GACTM)估算的地面臭氧浓度数据,该模型估算的全球年度气孔臭氧沉积量为234.0 Tg O3 yr-1,并表明哪些区域具有较高的臭氧破坏风险。不同的植物功能类型,阳光照射和阴影遮盖的叶子对臭氧的反应也不同。该模型预测表明,在2004-2008年的研究期内,臭氧对全球陆地生态系统的碳存储和碳交换造成了重大变化。该研究表明,iTemO3中关键参数的不确定性可能导致模型预测中的较大误差。因此,迫切需要更多的实验数据来更好地进行模型参数化。

著录项

  • 作者

    Chen, Min.;

  • 作者单位

    Purdue University.;

  • 授予单位 Purdue University.;
  • 学科 Geophysics.;Atmospheric Sciences.
  • 学位 Ph.D.
  • 年度 2013
  • 页码 223 p.
  • 总页数 223
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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