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DOI | 10.1016/j.atmosenv.2019.117186 |
Rapid changes of dust geochemistry in the Saharan Air Layer linked to sources and meteorology | |
Rodríguez S.; Calzolai G.; Chiari M.; Nava S.; García M.I.; López-Solano J.; Marrero C.; López-Darias J.; Cuevas E.; Alonso-Pérez S.; Prats N.; Amato F.; Lucarelli F.; Querol X. | |
发表日期 | 2020 |
ISSN | 1352-2310 |
卷号 | 223 |
英文摘要 | Based at Izaña Observatory (~2400 m a.s.l. in Tenerife), we performed 1-h resolution measurements of elemental composition of dust in the Saharan Air Layer (SAL) and studied the variability of the ratios of these elements to aluminium (elemental ratios). In a period (~1 week) of continuous dust presence (50–200 μg/m3), we observed rapid variations of dust composition; some elemental ratios changed by a factor 2 in a few (5–8) hours. The lowest variability (Normalized Variability Range, %) was found for Si/Al (9%) and Fe/Al (9%), followed by the ratios of K, Ti, Mg, Mn, Ca and Sr to Al (20–80%), and the highest for S/Al, Na/Al and Cl/Al (110–160%) and a number of trace metals (Cr, Cu, Ni, Zn, Zr) and Br (>200%). This variability was induced by the alternating impacts of three of the large North African dust sources: NE Algeria (rich in evaporite minerals bearing Ca, S, Sr, K and Mg and in illite mineral), Western Sahara to Bechar region (containing Na, S and Cl rich Yermosol soils) and SW Sahara – Western Sahel (rich in illite and hematite). We traced the variability in large-scale meteorology using the so-called North African Dipole Intensity (NAFDI: strength of the subtropical Saharan high -Morocco-to the monsoon tropical low -Nigeria-). The mobilization of dust from the different sources was associated with westward propagating Harmattan pulses linked to the change of phase of NAFDI (- to +), the associated westward shifts of the Saharan Heat Low and convective monsoon inflow. We found a correlation between dust composition in the SAL and NAFDI: moderate NAFDI values (0 to +2.5) were associated with Ca, K, Na, Mg and S rich dust linked to dust sources in NE Algeria, whereas higher NAFDI values (+2.5 to +4) were linked to Fe rich dust (Ca, Na and S depleted) linked to dust sources in SW Sahara – Western Sahel. The results of this study also show that some trace elements (Br, Cr, Ni, Zn and Zr) are influenced by industrial emissions into North Africa. © 2019 Elsevier Ltd |
英文关键词 | Dust geochemistry; Harmattan; NAFDI; North Africa; Saharan air layer; Saharan dust sources |
语种 | 英语 |
scopus关键词 | Atmospheric thermodynamics; Geochemistry; Hematite; Industrial emissions; Magnesium; Meteorology; Trace elements; Tropics; Harmattan; NAFDI; North Africa; Saharan air layers; Saharan dust; Dust; aluminum; arsenic; barium ion; calcium ion; chromium; cuprous ion; iron; lead; magnesium; manganese; nickel; potassium; rubidium ion; selenium; silicon; sodium; strontium; titanium; zinc ion; zirconium; atmospheric convection; atmospheric pollution; chemical composition; dust; geochemistry; industrial emission; isotopic ratio; meteorology; mobilization; observatory; pollutant source; subtropical region; trace element; Yermosol; aerosol; Article; dust; geochemistry; geographic and geological parameters; gravimetry; meteorology; North African; optical depth; particulate matter; priority journal; saharan air layer; Western Sahara; Algeria; Bechar; Canary Islands; Morocco; Nigeria; Sahel; Sahel [Sub-Saharan Africa]; Santa Cruz de Tenerife [(PRV) Canary Islands]; Spain; Tenerife; Western Sahara |
来源期刊 | Atmospheric Environment |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/129616 |
作者单位 | Izaña Atmospheric Research Centre, AEMET, Tenerife, Spain; Estación Experimental de Zonas Aridas EEZA CSIC, Almería, Spain; Instituto de Productos Naturales y Agrobiología, IPNA CSIC, Tenerife, Spain; Istituto Nazionale di Fisica Nucleare, Firenze, Italy; Department of Chemistry, University of La Laguna, Spain; Universidad Europea de Canarias, Tenerife, Spain; Institute of Environmental Assessment and Water Research, IDAEA-CSIC, Barcelona, Spain; Physics and Astronomy Department, University of Florence, Italy |
推荐引用方式 GB/T 7714 | Rodríguez S.,Calzolai G.,Chiari M.,et al. Rapid changes of dust geochemistry in the Saharan Air Layer linked to sources and meteorology[J],2020,223. |
APA | Rodríguez S..,Calzolai G..,Chiari M..,Nava S..,García M.I..,...&Querol X..(2020).Rapid changes of dust geochemistry in the Saharan Air Layer linked to sources and meteorology.Atmospheric Environment,223. |
MLA | Rodríguez S.,et al."Rapid changes of dust geochemistry in the Saharan Air Layer linked to sources and meteorology".Atmospheric Environment 223(2020). |
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