Mineral Dust Aerosols: Ecological and radiative impacts

矿物粉尘气溶胶：生态和辐射影响

• 批准号: RGPIN-2016-05417
• 负责人: King, James
• 金额: $ 1.82万
• 依托单位: Université de Montréal
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2016
• 资助国家: 加拿大
• 起止时间: 2016-01-01 至 2017-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=615680
• 关键词: Mineral; Dust; Aerosols; Ecological; radiative

Mineral dust aerosols affect climate directly through the scattering and absorbing of shortwave and thermal radiation and currently account for the largest uncertainty in the radiative forcing within current global climate models. Terrestrial and marine ecosystems in arid regions rely on the atmospheric deposition of mineral aerosols as a result of wind erosion to provide essential soluble nutrients. Currently, mineral dust emission schemes used within global climate models are based on theoretical models parameterized and corrected with highly idealized laboratory results. This simplification leads to simulated emissions that poorly represent actual transported size distributions and therefore mineral dust production and deposition rates. Although mass conservation is maintained in the models, biased rates of flux occur for minerals and nutrients from the source material, resulting in poor estimates of the biological impact of wind erosion. The proposed research program seeks to provide a new approach to the dynamic wind erosion process for measuring and quantifying mineral dust emissions. The program consists of two complementary methodological approaches to establish the role and impact of mineral dust size and chemical distributions throughout the transport process. First, it will evaluate the change in particle size distribution and associated mineralogy of particles as a result from the transport process through a series of laboratory wind tunnel investigations with natural and fabricated soils. These proposed investigations will seek to quantify the enrichment of nutrients in the transportation process to estimate the differences in the radiative and biological properties of mineral aerosols from their parent soils. Secondly, a novel methodology to measure dust emission fluxes is proposed using eddy covariance to provide more reliable estimates over traditional time-averaged methods. A series of comparative field studies in Namibia will utilize these different approaches over a range of surfaces to provide the first such set of this data. The chosen field sites are situated in regions that are directly impacted by the fertilizing component of mineral dust they receive. These results will be tested against current dust emission flux models to improve the performance of existing models and redefine standard procedures for measuring mineral dust emissions. This proposed research program will increase the ability for forecasting dust storms and their impacts on society and the natural environment. This new research will also improve the ability to predict the timing and severity of visibility and associated transport hazard systems within Canadian prairies and other arid zones.

矿物尘埃气溶胶通过短波和热辐射的散射和吸收直接影响气候，目前是目前全球气候模型中辐射强迫的最大不确定性因素。干旱地区的陆地和海洋生态系统依靠风蚀造成的大气矿物气溶胶沉积来提供必要的可溶营养物质。目前，全球气候模型中使用的矿物粉尘排放计划是以理论模型为基础的，这些模型已被参数化，并用高度理想化的实验室结果进行了修正。这种简化导致模拟的排放不能很好地反映实际输送的粒度分布，从而导致矿物粉尘的产生和沉积速率。尽管在模型中保持了质量守恒，但来源材料中的矿物质和营养物质的通量出现了偏差，导致对风蚀的生物影响的估计不准确。拟议的研究计划旨在为测量和量化矿物粉尘排放的动态风蚀过程提供一种新的方法。该方案由两种互补的方法组成，以确定矿物粉尘的大小和化学分布在整个运输过程中的作用和影响。首先，它将通过对天然和人造土壤进行一系列实验室风洞调查，评估运输过程中颗粒粒度分布和相关矿物学的变化。这些拟议的调查将力求量化运输过程中营养物质的丰富程度，以估计矿物气溶胶与其母质土壤之间的辐射和生物特性的差异。其次，提出了一种利用涡动协方差来测量粉尘排放通量的新方法，以提供比传统的时间平均方法更可靠的估计。纳米比亚的一系列比较实地研究将在一系列表面上使用这些不同的方法，以提供第一组这样的数据。选定的田间地块所在的区域直接受到它们所接收的矿物粉尘的肥料成分的影响。这些结果将与目前的粉尘排放通量模型进行测试，以改进现有模型的性能，并重新定义测量矿物粉尘排放的标准程序。这项拟议的研究计划将提高预测沙尘暴及其对社会和自然环境影响的能力。这项新的研究还将提高预测加拿大草原和其他干旱地区内能见度和相关运输危险系统的时间和严重程度的能力。