全球五个 AERONET 站的气溶胶光学深度与可降水量的相关研究

Santosh Sapkota, Sabina Gautam, Aayush Gautam, Bhairab Ale
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引用次数: 0

摘要

2016年1月至12月,在加德满都博德、北京、甘地学院(位于南亚区,高污染区)、堪培拉和联合国大学盖坦分校(位于东南区,低污染区)等不同地点进行了地基测量。作为气溶胶机器人网络(AERONET)的一部分,该研究利用 CIMEL 太阳光度计获得了季节性和年际性 AOD。数据显示,加德满都(0.45±0.01)、甘地学院(0.45±0.02)和北京(0.85±0.03)的 AOD 值高于其他站点,加德满都属于高海拔地区。分析发现,加德满都(0.45±0.01)、甘地学院(0.45±0.02)、UNC 盖坦(0.28±0.001)和堪培拉(0.06±0.002)的季风前 AOD 值较高。另一方面,北京的季风 AOD 较高(0.85±0.03)。研究发现了导致特定地区 AOD 值较高的各种因素。位于亚洲季风区的北京、甘地学院和加德满都,由于经济活动、车辆、城市化、植被火灾、农作物种植的土地开垦,以及冬季生物质燃烧、供暖需求和砖窑、工厂和车辆污染,气溶胶负荷较高。堪培拉和 UNC Gaitan 的 AOD 值较高,主要原因是生物质燃烧和灰尘。波长越短,AOD 值越高,反之亦然。我们对不同波长的 AOD 和可感知水进行了相关分析,观察到一一对应的关系。在堪培拉,柱状水蒸气(CWV)与 1640 纳米波长的 AOD 有很高的相关性(判定系数,R2 = 0.61),但与甘地学院 1640 纳米波长的 AOD 没有关系(判定系数,R2 = 0)。加德满都和盖坦联合国军司令部上空的 AOD 与可接受水之间存在微弱的负相关,但堪培拉、北京和甘地学院上空的 AOD 与可接受水之间存在正相关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Correlative study of Aerosol Optical Depth with Precipitable water over five AERONET station across the world
Ground-based measurements were taken at various locations, including Kathmandu Bode, Beijing, Gandhi College (located in South Asian zone, highly polluted area), Canberra, and UNC Gaitan (located in South Eastern zone, low polluted area), from January to December 2016. The study investigated the seasonal and inter-annual AOD that were obtained using CIMEL Sunphotometer, as a part of the Aerosol Robotic Network (AERONET). The data showed that Kathmandu (0.45±0.01), Gandhi College (0.45±0.02 and Beijing (0.85±0.03) had higher AOD values compared to other stations, with Kathmandu being a high-altitude site. The analysis found that pre-monsoon AOD were higher over Kathmandu (0.45±0.01), Gandhi College (0.45±0.02), UNC Gaitan (0.28±0.001), and Canberra (0.06±0.002). On the other hand, the monsoon AOD was higher over Beijing (0.85±0.03). The study identified various factors contributing to the higher AOD values in specific regions. Beijing, Gandhi College, and Kathmandu, located in Asian monsoon regions, experienced high aerosol loading due to economic activities, vehicles, urbanization, vegetation fire, land clearing for crop cultivation, as well as winter biomass burning, heating needs, and pollution from bricks kilns, factories, and vehicles. Canberra and UNC Gaitan had higher AOD values primarily due to biomass burning and dust. AOD values are higher for shorter wavelength and vice-versa. We conducted a correlation analysis between AOD and perceptible water at different wavelengths and observed one to one correspondence. The columnar water vapor (CWV) exhibited a high correlation with AOD in Canberra (Coefficient of determination, R2 = 0.61) at 1640 nm but had no relationship with AOD in Gandhi College (Coefficient of determination, R2 = 0) at 1640nm. There is weak negative correlation between AOD and preceptable water over Kathmandu and UNC Gaitan, but have positive correlation in Canberra, Beijing and Gandhi College
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