Raman Aishwarya, Arellano Avelino F, Sorooshian Armin
Department of Hydrology and Atmospheric Sciences, Tucson, AZ 85721, USA.
Department of Chemical and Environmental Engineering, Tucson, AZ 85721, USA.
Atmosphere (Basel). 2016 Feb;7(2). doi: 10.3390/atmos7020024. Epub 2016 Feb 5.
We examine the spatio-temporal variability of aerosol loading in the recent decade (2005-2014) over the North American Monsoon (NAM) region. Emerging patterns are characterized using aerosol optical depth (AOD) retrievals from the NASA Terra/Moderate Resolution Imaging Spectroradiometer (MODIS) instrument along with a suite of satellite retrievals of atmospheric and land-surface properties. We selected 20 aerosol hotspots and classified them into fire, anthropogenic, dust, and NAM alley clusters based on the dominant driver influencing aerosol variability. We then analyzed multivariate statistics of associated anomalies during pre-, monsoon, and post-monsoon periods. Our results show a decrease in aerosol loading for the entire NAM region, confirming previous reports of a declining AOD trend over the continental United States. This is evident during pre-monsoon and monsoon for fire and anthropogenic clusters, which are associated with a decrease in the lower and upper quartile of fire counts and carbon monoxide, respectively. The overall pattern is obfuscated in the NAM alley, especially during monsoon and post-monsoon seasons. While the NAM alley is mostly affected by monsoon precipitation, the frequent occurrence of dust storms in the area modulates this trend. We find that aerosol loading in the dust cluster is associated with observed vegetation index and has only slightly decreased in the recent decade.
我们研究了近十年(2005 - 2014年)北美季风(NAM)区域气溶胶负荷的时空变化。利用美国国家航空航天局(NASA)泰拉卫星/中等分辨率成像光谱仪(MODIS)仪器反演的气溶胶光学厚度(AOD)以及一系列大气和陆地表面特性的卫星反演数据,对出现的模式进行了特征描述。我们选取了20个气溶胶热点区域,并根据影响气溶胶变化的主要驱动因素将它们分为火灾、人为、沙尘和北美季风通道簇。然后,我们分析了季风前、季风期和季风后相关异常的多元统计数据。我们的结果表明,整个北美季风区域的气溶胶负荷有所下降,这证实了此前关于美国大陆AOD呈下降趋势的报道。这在季风前和季风期的火灾和人为簇中很明显,分别与火灾次数和一氧化碳的下四分位数和上四分位数的减少有关。在北美季风通道中,整体模式较为模糊,尤其是在季风期和季风后季节。虽然北美季风通道主要受季风雨的影响,但该地区频繁发生的沙尘暴调节了这一趋势。我们发现,沙尘簇中的气溶胶负荷与观测到的植被指数有关,并且在最近十年中仅略有下降。