دورية أكاديمية

Vertical characterization of fine and coarse dust particles during an intense Saharan dust outbreak over the Iberian Peninsula in springtime 2021

التفاصيل البيبلوغرافية
العنوان: Vertical characterization of fine and coarse dust particles during an intense Saharan dust outbreak over the Iberian Peninsula in springtime 2021
المؤلفون: López-Cayuela, María Ángeles, Córdoba-Jabonero, Carmen, Bermejo-Pantaleón, Diego, Sicard, Michaël, Salgueiro, Vanda, Molero, Francisco, Carvajal-Pérez, Clara Violeta, Granados-Muñoz, María José, Comerón, Adolfo, Couto, Flavio, Barragán, Rubén, Zorzano, María-Paz, Bravo-Aranda, Juan Antonio, Muñoz-Porcar, Constantino, Costa, María João, Artíñano, Begoña, Rodríguez-Gómez, Alejandro, Bortoli, Daniele, Pujadas, Manuel, Abril-Gago, Jesús, Alados-Arboledas, Lucas, Guerrero-Rascado, Juan Luis
المساهمون: Instituto Nacional de Técnica Aeroespacial (INTA), Instituto Interuniversitario de Investigacion del Sistema Tierra en Andalucia (IISTA-CEAMA), Universidad de Granada = University of Granada (UGR), Laboratoire de l'Atmosphère et des Cyclones (LACy), Institut national des sciences de l'Univers (INSU - CNRS)-Université de La Réunion (UR)-Centre National de la Recherche Scientifique (CNRS)-Météo-France, Universitat Politècnica de Catalunya Barcelona (UPC), Earth Remote Sensing Laboratory (EaRSLab), University of Évora Portugal, Centro de Investigaciones Energéticas, Medioambientales y Tecnológicas (CIEMAT), Earth Remote Sensing Laboratory (EaRSLab) (EaRSLab), Centro de Astrobiología LAEX (CSIC-INTA), This research has been supported by the Spanish Ministry of Science and Innovation (grant no. PID2019-104205GB-C21/AEI/10.13039/501100011033)., The authors are grateful for support from the Spanish Ministry of Science and Innovation (MICIN, grant nos. PID2020-117825GB-C21, PID2020-120015RB-I00, PID2019-104205GB-C21/AEI/10.13039/501100011033, PID2019-103886RB-I00/AEI/10.13039/501100011033, EQC2018-004686-P, CGL2017-90884-REDT, and CGL2017-85344-R), the Madrid Regional Government (grant no. Y2018/EMT-5177), the Andalusian Regional Government (grant nos. P20_00136 and P18-RT-3820), the University of Granada (grant no. A-RNM-430-UGR20, Singular Laboratory programme LS2022-1, Scientific Units of Excellence Program grant no. UCE-PP2017-02), and the EU H2020 programme (grant nos. 654109, 778349, 871115, 101008004, and 101086690). The EVO team is co-funded by Portuguese funds through the Fundação para a Ciência e a Tecnologia (FCT) within the framework of the ICT (grant nos. UIDB/04683/2020 and UIDP/04683/2020) and TOMAQAPA (grant no. PTDC/CTAMET/29678/2017) projects. The ARN team thanks the technical staff of the El Arenosillo site for maintenance support. The BCN team particularly thanks Ellsworth J. Welton for providing the MPL unit in place at the Barcelona site. The authors thankfully acknowledge the FEDER programme for the instrumentation used in this work, which is part of the Laboratorio Singular de Tecnologías Avanzadas Observatorio Global de la Atmósfera (ÁGORA), supported by the University of Granada. Ellsworth J. Welton and Sebastian A. Stewart are warmly acknowledged for their continuous help in keeping the MPL systems up to date. María Ángeles López-Cayuela and Clara Violeta Carvajal-Pérez are supported by the INTA predoctoral contract programme. The authors thank the NOAA/ESRL Physical Science Laboratory for providing synoptic maps. The authors acknowledge the use of imagery from the NASA Worldview application (https://worldview.earthdata.nasa.govTest/, last access: 20 June 2021), part of the NASA Earth Observing System Data and Information System (EOSDIS)., European Project: 101086690,REALISTIC, European Project: 654109,H2020,H2020-INFRAIA-2014-2015,ACTRIS-2(2015), European Project: 778349,H2020,H2020-MSCA-RISE-2017,GRASP-ACE(2018), European Project: 871115,H2020,H2020-INFRADEV-2018-2020,ACTRIS IMP(2020), European Project: 101008004,ATMO-ACCESS
المصدر: ISSN: 1680-7316.
بيانات النشر: HAL CCSD
European Geosciences Union
سنة النشر: 2023
المجموعة: Institut national des sciences de l'Univers: HAL-INSU
مصطلحات موضوعية: Atmospheric, Atmospheric Aerosols, aerosol, aerosols, dust, mineral, lidar, extreme events, Particles, Algorithm, meteorological, [SDE]Environmental Sciences
الوصف: International audience ; Abstract. An intense and long-lasting Saharan dust outbreak crossed the Iberian Peninsula (IP) from the southwest (SW) to the northeast (NE) from 25 March until 7 April 2021. This work aims to assess the optical and mass contribution of both fine and coarse dust particles along their transport. Five Iberian lidar stations were monitoring the transport and evolution of the Saharan dust particles, i.e. El Arenosillo/Huelva, Granada, Torrejón/Madrid and Barcelona in Spain, and Évora in Portugal. The particular meteorological conditions determined the aerosol scenario along the overall dust event, differing in the first part of the event (25–31 March), in which the strongest dust incidence occurred on 29–31 March at the south and central stations and 1 April at Barcelona, from the second one (1–7 April). The use of the two-step POLIPHON algorithm showed the relevance of using polarized lidar measurements for separating the aerosol properties of dust fine and coarse particles as an added value. Both the fine dust (Df) and coarse dust (Dc) components of the total particle backscatter coefficient (total dust, DD = Dc + Df) were separately derived. The dust plume was well-mixed with height and no significant differences were found in the vertical structure of both the Dc and Df particle backscatter coefficients. From the beginning of the dust outbreak until 1 April, the vertical Df / DD mass ratio was nearly constant in time at each station and also in altitude with values of ∼ 10 %. Moreover, the mean dust optical depth at 532 nm was decreasing along that dust pathway, reporting values from SW to NE stations of 0.34 at El Arenosillo/Huelva, 0.28 at Granada, 0.20 at Évora, 0.28 at Torrejón/Madrid, and 0.14 at Barcelona, although its Df / DD ratio remained almost constant (28 %–30 %). A similar pattern was found for the total dust mass loading and its Df / DD ratio, i.e. mostly decreasing mean mass values were reported, being constant in its Df / DD ratio (∼ 10 %) along the SW–NE dust pathway. In ...
نوع الوثيقة: article in journal/newspaper
اللغة: English
العلاقة: info:eu-repo/grantAgreement//101086690/EU/centRe of Excellence in AerosoL remote sensIng technology and Science in The Indian oCean/REALISTIC; info:eu-repo/grantAgreement//654109/EU/Aerosols, Clouds, and Trace gases Research InfraStructure/ACTRIS-2; info:eu-repo/grantAgreement//778349/EU/Development of GRASP radiative transfer code for the retrieval of aerosol microphysics vertical-profiles from space measurements and its impact in ACE mission/GRASP-ACE; info:eu-repo/grantAgreement//871115/EU/Aerosol, Clouds and Trace Gases Research Infrastructure Implementation Project/ACTRIS IMP; info:eu-repo/grantAgreement//101008004/EU/Solutions for Sustainable Access to Atmospheric Research Facilities/ATMO-ACCESS; hal-04458801; https://hal.science/hal-04458801Test; https://hal.science/hal-04458801/documentTest; https://hal.science/hal-04458801/file/acp-23-143-2023.pdfTest
DOI: 10.5194/acp-23-143-2023
الإتاحة: https://doi.org/10.5194/acp-23-143-2023Test
https://hal.science/hal-04458801Test
https://hal.science/hal-04458801/documentTest
https://hal.science/hal-04458801/file/acp-23-143-2023.pdfTest
حقوق: info:eu-repo/semantics/OpenAccess
رقم الانضمام: edsbas.E88AD599
قاعدة البيانات: BASE