2013年中东地区气溶胶光学特性研究。

Desert Pub Date : 2019-12-01 DOI:10.22059/JDESERT.2019.76360
M. Gharibzadeh, Khan Alam
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引用次数: 2

摘要

气溶胶通过直接、半直接和间接的机制影响地球大气的辐射通量。气溶胶也是气候模式不确定性的主要来源之一。在中东,除了气候影响外,气溶胶还造成能见度降低、人类健康危害和空气污染等各种问题。在局部和全球尺度上研究气溶胶的光学和物理性质有助于减少气候强迫的不确定性。本研究分析了气溶胶光学特性,包括气溶胶光学深度(AOD)、埃指数(AE)、不对称参数(ASY)、单散射反照率(SSA)和相函数。这些特性在2013年期间使用气溶胶机器人网络(AERONET)数据在中东的五个站点进行了调查。结果显示AOD与AE在各位点呈反比关系。春季和夏季各观测点AOD值较高,AE值较低,为粗态沙尘。随着波长的增加,由于吸收型气溶胶在可见光谱中占主导地位,ASY开始下降。随后,由于粗模粒子的优势,ASY随红外区波长的增加而增加。在大多数站点,特别是在春夏季,由于沙尘的优势,SSA随着波长的增加而增加。春、夏季各站点相函数均较高。粗模粒子产生了高相函数和小散射角。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study of aerosol optical properties in the Middle East during 2013.
Aerosols affect the earth's atmospheric radiative fluxes via direct, semi-direct, and indirect mechanisms. Aerosols also are one of the main sources of uncertainty in climate models. In the Middle East, in addition to climate effects, various problems such as reduced visibility, human health hazards, and air pollution are caused by aerosols. Studying the optical and physical properties of aerosols on local and global scales helps reduce the uncertainties in climate forcing. In this study, aerosol optical properties, including Aerosol Optical Depth (AOD), Angstrom Exponent (AE), ASYmmetry parameter (ASY), Single Scattering Albedo (SSA), and phase function were analyzed. These properties were investigated over five sites in the Middle East during 2013 using the Aerosol Robotic NETwork (AERONET) data. The results revealed an inverse relationship between AOD and AE in all sites. A high AOD value and a low AE value were detected in spring and summer in all studied sites, suggestive of coarse mode dust particles. ASY initially decreased due to the dominance of absorbing type aerosols in the visible spectrum with the increase in wavelength. Afterwards, ASY increased with the increase in wavelength in the infrared region due to the dominance of the coarse mode particles. In most sites, SSA increased, particularly in spring and summer, with the increase in the wavelength because of the dominance of desert dust. In spring and summer, the phase function was high over all sites. High phase functions associated with small scattering angles were caused by the coarse mode particles.
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