The long-term spatial and temporal distribution of aerosol optical depth and its associated atmospheric circulation over Southeast Africa

被引:4
|
作者
Nyasulu, Matthews [1 ,2 ,3 ]
Haque, Md. Mozammel [1 ,4 ]
Musonda, Bathsheba [2 ,5 ]
Fang, Cao [1 ,4 ]
机构
[1] Nanjing Univ Informat Sci & Technol, Int Joint Lab Climate & Environm Change ILCEC, Yale NUIST Ctr Atmospher Environm, Nanjing 210044, Peoples R China
[2] Nanjing Univ Informat Sci & Technol, Sch Appl Meteorol, Nanjing 210044, Peoples R China
[3] Dept Climate Change & Meteorol Serv DCCMS Malawi, POB 1808, Blantyre, Malawi
[4] Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Key Lab Meteorol Disaster Minist Educ KLME, Nanjing 210044, Peoples R China
[5] Zambia Meteorol Dept, Lusaka 30200, Zambia
基金
中国国家自然科学基金;
关键词
Aerosol optical depth (AOD); Biomass burning; Atmospheric circulation; Southeast Africa; BOUNDARY-LAYER HEIGHT; RAINFALL VARIABILITY; AERONET SITES; AIR-POLLUTION; MODIS; SATELLITE; URBAN; TRENDS; CLIMATOLOGY; PARAMETERS;
D O I
10.1007/s11356-021-18446-7
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Recent studies have revealed significant impact of anthropogenic aerosols to both climate and human health. Even though significant efforts have been made across the globe, studies related to aerosols over Southeast Africa remain scanty, hence causing high uncertainty in predicting and understanding the impacts of these aerosols. The present study therefore analyzed long-term spatial and temporal distribution of aerosol optical depth at 550 nanometer wavelength (AOD(550)) over the entire Southeast Africa. Relatively low AOD(550) has been detected over the region in comparison to highly polluted regions across the globe. The highest annual average (>0.2) was observed over Lake Malawi, Zambezi valley, and the coastal areas of Central Mozambique while low annual values were recorded over northeast of Mozambique, and the eastern areas of Zimbabwe. In terms of seasonality, AOD(550) was observed to be high (>0.3) during the dry months of September-October-November (SON) while being low (<0.1) during March-April-May (MAM) and June-July-August (JJA) in most areas. The seasonality of AOD(550) was observed to be highly influenced by changes in seasonal biomass burning and seasonal atmospheric circulation. Statistical analyses revealed an insignificant change of AOD(550) between 2002 and 2020 in most areas of the study domain. Regional open burning of biomass like bush fires and burning of crop residues during the dry months are the main sources of aerosol concentration. Therefore, the present study advocates the regulation and institutionalization of proactive and strategic mechanisms that curtail open burning activities within the region.
引用
收藏
页码:30073 / 30089
页数:17
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