Characterization of the Effects of a Severe Drought on Dust Lifting
Characterization of the Effects of a Severe Drought on Dust Lifting
批准号:
1526444
负责人:
Nilton Renno
金额:
$67.2万
依托单位国家:
美国
项目类别:
Continuing Grant
财政年份:
2015
资助国家:
美国
项目状态:
已结题
起止时间:
2015-08-15 至 2019-07-31
中文摘要
众所周知,大气中的尘埃颗粒通过吸收和散射辐射以及通过其影响云过程的能力来影响天气和气候。 为了更好地了解大气中粉尘含量的变化,重要的是研究粉尘气溶胶是如何从地面传输到大气中的,这一过程被称为跳跃。 该奖项将为加州欧文斯湖干盐湖的观测和数据分析提供资金,欧文斯湖干盐湖是一个干燥的湖床,被认为是灰尘污染的重要来源。 这项研究将设法确定土壤颗粒大小分布、结皮土壤、含水量和粉尘带电在跳跃中的作用。 该项目的长期社会效益是通过更好地代表天气和气候系统中的灰尘,从而改善预报。 在短期内,研究人员将与欧文斯谷空气质量官员合作,提供与健康影响的直接联系,该项目还将有助于学生的教育和培训。该研究项目将调查土壤成分,颗粒大小分布和土壤含水量对跃变层深度,跃变强度,跃变产生的电场,以及PM2.5气溶胶浓度在各种天气现象和气候条件下作为风切变应力的函数。 该活动主要是观察性的,仪器位于加州的欧文斯湖盐沼。 这项工作的三个主要目标是:1)跃移和尘埃上升-继续和改进的测量将用于检验关于垂直尘埃通量和近地表湿度之间相关性的相互竞争的假设,2)电场对尘埃上升的影响-电场数据将用于检验电力吸引跃移粒子朝向地表的假设,3)沙尘天气现象-研究人员将研究从小规模沙尘羽流和涡旋到大规模沙尘暴等天气现象中的跃移层和沙尘抬升的强度和深度,以准确地量化每种天气现象对沙尘循环的贡献。 还将检验由对流事件扬起的尘埃更富含细颗粒的假设。
英文摘要
Dust particles in the atmosphere are known to affect weather and climate through the absorption and scattering of radiation and through their ability to affect cloud processes. In order to better understand the variability of dust loading in the atmosphere it is important to study how dust aerosols are transported from the surface to the atmosphere, a process known as saltation. This award will provide funding for observations and analysis of data from the Owens Lake playa in California, a dry lake bed that is known as a significant source of dust pollution. The research will seek to determine the roles of soil particle size distribution, crusted soil, water content, and dust electrification in saltation. The long-term societal benefits of the project are through better representation of dust in the weather and climate system, thereby improving forecasts. In the shorter-term the researchers will work with the Owens Valley air quality officer, offering a direct link to health effects, and the project will also contribute to the education and training of students.This research project will investigate the effects of soil composition, particle size distribution, and soil water content on the depth of the saltation layer, the intensity of saltation, the electric fields generated by saltation, and the PM2.5 aerosol concentration as a function of wind shear stress in a variety of weather phenomena and climate conditions. The campaign is primarily observational, with instrumentation residing in the Owens Lake salty playa in California. The three main objectives of the work are in the following areas: 1) Saltation and dust lifting - Continued and improved measurements will be used to test competing hypotheses about the correlation between vertical dust flux and near surface humidity, 2) Effects of electric fields on dust lifting - Electric field data would be used to test the hypothesis that electric forces attract saltating particles toward the surface, inhibiting increases in the depth of the saltation layer with increases in wind shear stress at the surface, and 3) Dusty weather phenomena - The researcher will study the intensity and depth of the saltation layer and dust lifting in weather phenomena ranging from small-scale dusty plumes and vortices to larger-scale dust storms to accurately quantify the contributions from each to the dust cycle. The hypothesis that dust lifted by convective events is much richer in fine particles will also be tested.
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