一种改进的沙尘暴干沉积模式

Abbasi A, M. Mr, Setodeh P
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引用次数: 0

摘要

特别是近年来,沙尘暴对世界各地的有害影响已成为人们非常关注的问题。在这种现象中,细颗粒的运动可分为干沉积和湿沉积两类。通过各种阻力网络来模拟粉尘沉积是一种常见的做法,因为它有助于表征每种机制对干沉积总体速率的影响。在本研究中,与以前的模型相比,考虑的假设较少。提出的模型涵盖了更广泛的条件,也包括热泳的影响。此外,利用风速等气象数据,将复杂的大气稳定度和风摩擦速度计算方法简化。将修正后的沉积模型与已有的现场资料进行了定性和定量比较,证实了该模型的可靠性。引用本文:Abbasi A, Malayeri MR, Setodeh P(2018)一种改进的沙尘暴干沉积模型。[J] .地球科学进展(英文版);doi: 10.4172 / 2157 - 7617.1000486
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Revamped Model of Dust Storm Dry Deposition
In recent years in particular, the detrimental impacts of dust storms around the world has become a matter of much concern. In this phenomenon, the movement of fine particles may fall into two categories of dry and wet depositions. It is a common practice to model dust deposition by a network of various resistances as it facilitates to characterize the impact of each mechanism on the overall rate of dry deposition. In this study, fewer assumptions are considered in comparison to previous models. The proposed model covers a wider range of conditions and also includes the impact of thermophoresis. Moreover, the complicated calculations of atmospheric stability and wind friction velocity are replaced with a simpler algorithm by using the meteorological data such as wind speed. The reliability of the modified deposition model is confirmed when compared with the available field data from the literature with good agreement both qualitatively and quantitatively. Citation: Abbasi A, Malayeri MR, Setodeh P (2018) A Revamped Model of Dust Storm Dry Deposition. J Earth Sci Clim Change 9: 486. doi: 10.4172/2157-7617.1000486
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